query: with reference to the climate of india the western disturbances originate over

pos: Western Disturbance Western Disturbance A "Western Disturbance" is an extratropical storm originating in the Mediterranean region that brings sudden winter rain to the northwestern parts of the Indian subcontinent. It is a non-monsoonal precipitation pattern driven by the westerlies. The moisture in these storms usually originates over the Mediterranean Sea and the Atlantic Ocean. Extratropical storms are a global phenomena with moisture usually carried in the upper atmosphere, unlike their tropical counterparts where the moisture is carried in the lower atmosphere. In the case of the Indian subcontinent, moisture is sometimes shed as rain when the storm system encounters the Himalayas. Western

pos: Climate of Tamil Nadu in the middle of March. The climate in the cold weather is pleasant. The days are bright and sunny the sun is not too hot. As soon as the sun sets the temperature falls and the heat of the day yields place to cooler weather. The state has three distinct periods of rainfall: advance rainfall ; rainfall from the tropical cyclones emerging in the neighbourhood of the Andaman islands during the Retreat of Monsoons(October–November); and the North East monsoon during the months of October–December, with dominant northeast monsoon winds from the western disturbances emerging over the Mediterranean Sea. The dry

pos: Chandigarh Delhi. Chandigarh has a humid subtropical climate (Köppen: Cwa) characterised by a seasonal rhythm: very hot summers, mild winters, unreliable rainfall and great variation in temperature (−1 °C to 46 °C OR 30.2 °F to 114 °F). The average annual rainfall is 1110.7 mm. The city also receives occasional winter rains from the Western Disturbance originating over the Mediterranean Sea. The western disturbances usually bring rain predominantly from mid-December till end of April which can be heavier sometimes with strong winds and hails if the weather turns colder (during March–April months) which usually proves disastrous to the crops. Cold winds

pos: Dera Bassi and Ambala in Haryana. Chandigarh is situated 119 km southwest of Shimla, 30 km (19 miles) northeast of Ambala, 236 km (148 miles) southeast of Amritsar and 230 km (144 miles) north of Delhi. Derabassi has a humid subtropical climate (Köppen: Cwa) characterised by a seasonal rhythm: very hot summers, mild winters, unreliable rainfall and great variation in temperature (−1 °C to 46 °C OR 30.2 °F to 114 °F). The average annual rainfall is 1110.7 mm. The city also receives occasional winter rains from the Western Disturbance originating over the Mediterranean Sea. The western disturbances usually brings rain predominantly

pos: Naraingarh ft). The city, lying in the northern plains, has vast fertile and flat land. It has portions of Bhabar in the north east and Terai in rest of the area. Naraingarh has a humid subtropical climate (Köppen: Cwa) characterised by a seasonal rhythm: very hot summers, mild winters, unreliable rainfall and great variation in temperature (−1 °C to 46 °C OR 30.2 °F to 114 °F). The city also receives occasional winter rains from the Western Disturbance originating over the Mediterranean Sea. The western disturbances usually brings rain predominantly from mid-December till end of April which can be heavier sometimes

neg: Climate of India temperature hovers around , and the proximity of the sea increases the level of humidity. In southern India, the temperatures are higher on the east coast by a few degrees compared to the west coast. By May, most of the Indian interior experiences mean temperatures over , while maximum temperatures often exceed . In the hot months of April and May, western disturbances, with their cooling influence, may still arrive, but rapidly diminish in frequency as summer progresses. Notably, a higher frequency of such disturbances in April correlates with a delayed monsoon onset (thus extending summer) in northwest India. In

neg: Western Disturbance Disturbances are important for the development of the Rabi crop, which includes the locally important staple wheat. Western disturbances originate in the Mediterranean region. A high-pressure area over Ukraine and neighbourhood consolidates, causing the intrusion of cold air from polar regions towards an area of relatively warmer air with high moisture. This generates favorable conditions for cyclogenesis in the upper atmosphere, which promotes the formation of an eastward-moving extratropical depression. Traveling at speeds up to , the disturbance moves towards the Indian subcontinent until the Himalayas inhibits its development, upon which the depression rapidly weakens. The Western Disturbances are embedded

neg: Western Disturbance Western disturbances are usually associated with cloudy sky, higher night temperatures and unusual rain. Excessive precipitation due to western disturbances can cause crop damage, landslides, floods and avalanches. Over the Indo-Gangetic plains, they occasionally bring cold wave conditions and dense fog. These conditions remain stable until disturbed by another western disturbance. When western disturbances move across northwest India before the onset of monsoon, a temporary advancement of monsoon current appears over the region. The strongest western disturbances usually occur in the northern parts of Pakistan, where flooding is reported number of times during the winter season. Western disturbances start declining

neg: Climate of India India are subject to a humid subtropical climate. Though they experience hot summers, temperatures during the coldest months may fall as low as . Due to ample monsoon rains, India has only one subtype of this climate under the Köppen system: "Cwa". In most of this region, there is very little precipitation during the winter, owing to powerful anticyclonic and katabatic (downward-flowing) winds from Central Asia. Humid subtropical regions are subject to pronounced dry winters. Winter rainfall—and occasionally snowfall—is associated with large storm systems such as "Nor'westers" and "Western disturbances"; the latter are steered by westerlies towards the Himalayas. Most

neg: Aurangabad, Maharashtra on all directions. Climate Classification: Aurangabad features a semiarid climate under the Köppen climate classification. Temperature: Annual mean temperatures in Aurangabad range from 17 to 33 °C, with the most comfortable time to visit in the winter – October to February. The highest maximum temperature ever recorded was 46 °C (114 °F) on 25 May 1905. The lowest recorded temperature was 2 °C (36 °F) on 2 February 1911. In the cold season, the district is sometimes affected by cold waves in association with the eastward passage of western disturbances across north India, when the minimum temperature may drop down

neg: Geography of Uttar Pradesh Geography of Uttar Pradesh Uttar Pradesh is India's fourth largest and most populous [States of India ], located in the north-central part of the country. It spreads over a large area, and the plains of the state are quite distinctly different from the high mountains in the north. The climate of this state can also vary widely - primarily due to it being far from the moderating effect of the sea and the occasional cold air arising due to western disturbances - with temperatures reaching as high as 49 °C in summer, and as low as -1 °C in winter.

neg: Climate of India also reflects these seasons in its arrangement of months. Once the monsoons subside, average temperatures gradually fall across India. As the Sun's vertical rays move south of the equator, most of the country experiences moderately cool weather. December and January are the coldest months, with the lowest temperatures occurring in the Indian Himalayas. Temperatures are higher in the east and south. In northwestern India region, virtually cloudless conditions prevail in October and November, resulting in wide diurnal temperature swings; as in much of the Deccan Plateau, they register at 16–20 °C (61–68 °F). However, from January to February, "western disturbances"

neg: Climate of India indeed believed to play an important role in the formation of Central Asian deserts such as the Taklamakan and Gobi. The mountain ranges prevent western winter disturbances in Iran from travelling further east, resulting in much snow in Kashmir and rainfall for parts of Punjab and northern India. Despite the Himalayas being a barrier to the cold northerly winter winds, the Brahmaputra valley receives part of the frigid winds, thus lowering the temperature in Northeast India and Bangladesh. The Himalayas, which are often called "The Roof of the World", contain the greatest area of glaciers and permafrost outside of the

neg: Western Disturbance in numbers after winter. During the summer months of April and May, they move across north India. The southwest monsoon current generally progresses from east to west in the northern Himalayan region, unlike western disturbances which follow a west to east trend in north India with consequent rise in pressure carrying cold pool of air. This helps in the activation of monsoon in certain parts of northwest India. The interaction of the monsoon trough with western disturbances may occasionally cause dense clouding and heavy precipitation. The 2013 North India floods, which killed more than 5000 people in a span of

neg: Climate of Spain the border with France, with a few exceptions. It also extends inland in Andalusia and Extremadura. It is characterized by hot dry summers and mild winters with infrequent frosts in inland locations with this climate. The summers are hot, the winters are mild and most of precipitation falls in the autumn. Examples of cities with Csa climate are Malaga, Valencia, Palma or Seville. The "Csb" warm-summer mediterranean climate is found in Galicia and the western areas of Castilla y Leon. Coastal Mediterranean region is marked by Leveche winds: hot, dry, easterly or southeasterly air currents that originate over North Africa.

neg: Climate of India bring heavy bursts of rain and snow. These extra-tropical low-pressure systems originate in the eastern Mediterranean Sea. They are carried towards India by the subtropical westerlies, which are the prevailing winds blowing at North India's range of latitude. Once their passage is hindered by the Himalayas, they are unable to proceed further, and they release significant precipitation over the southern Himalayas. There is a huge variation in the climatic conditions of Himachal Pradesh due to variation in altitude (450–6500 metres). The climate varies from hot and subtropical humid (450–900 meters) in the southern low tracts, warm and temperate (900–1800 metres),

neg: Córdoba, Argentina and downstream. The climate of the city of Córdoba, and that of most of the province, is humid subtropical ("Cwa", according to the Köppen climate classification), moderated by the Pampas winds, cold winds that blow from the South-western quadrant, which originate in Antarctica. There are four marked seasons. Summers run from late November till early March, and bring days between and and night between and with frequent thunderstorms. Heat waves are common, and bring days with temperatures over and hot, sticky nights; however, Pampero winds are sure to bring relief with thunderstorms and a day or two of cool, crisp

neg: Civil disturbances in Western Australia Civil disturbances in Western Australia Civil disturbances in Western Australia include race riots, prison riots, and religious conflicts – often Protestant versus Catholic groups. The earliest civil disturbances were actions by the local indigenous population dealing with European settlers. Demonstrations and protests are linked to a range of issues over time. In the convict era, there were collective actions by convicts. Organised labour had to deal with issues on the Goldfields in the 1890s and 1900s with demonstrations and protest actions, while in Perth these occurred in the 1960s and 1970s over war and race issues. There are some incidents

neg: Climate of Lahore Climate of Lahore Lahore features a five-season semi-arid climate (Köppen climate classification "BSh")(from another source: Composite monsoon climate) with five seasons: foggy winter (15 Nov – 15 Feb) with few western disturbances causing rain; pleasant spring (16 Feb – 15 April); summer (15 April – June) with dust, rain storms and heat wave periods; rainy monsoon (July – 16 September); and dry autumn (16 September –14 November). The hottest month is June, where average highs routinely exceed . The wettest month is July, with heavy rainfalls and evening thunderstorms with the possibility of cloudbursts. The coolest month is January with

neg: South India monsoon climate characterised by moderate to high year-round temperatures and seasonal heavy rainfall above per year. The tropical climate is experienced in a strip of south-western lowlands abutting the Malabar Coast, the Western Ghats and the islands of Lakshadweep and Andaman and Nicobar are also subject to this climate. The tropical wet and dry climate, drier than areas with a tropical monsoon climate, prevails over most of the inland peninsular region except for a semi-arid rain shadow east of the Western Ghats. Winter and early summer are long and dry periods with temperatures averaging above , summer is exceedingly hot

neg: Climate of West Bengal the minimum temperature can often drop to the 5 to 7 degree C mark. Occasionally slight rainfall occurs under the influence of low depressions in northwest India. These is known as' "western disturbances'." The Tropic of Cancer passes 6 km north of Nabadwip, so, according to latitude, the northern part of the state falls in the temperate belt and the southern part fall in the tropical belt. But the southern part receives adequate rainfall and because of maritime influence is not severely hot. Barring the mountainous parts of Darjeeling and Jalpaiguri, the entire state experiences a warm wet tropical monsoon

neg: Climate of Uttar Pradesh to map of India above) Based on IMD classification, UP has the following three predominant seasons: Retreating Monsoon season, although existent, has a very negligible effect in Uttar Pradesh and only occasional mild showers are experienced in winter. Some of these showers are not even due to the Monsoon but due to western disturbances. The primary temperature, rainfall and wind features of the three Distinct Seasons of U.P. can be summarized as below: Given significant climatic differences, U.P. has been divided into two meteorological sub-divisions - U.P. East and U.P. West. The state of Uttar Pradesh is in the heart

neg: Western Disturbance in the mid-latitude Subtropical Westerly Jet. Western disturbances, specifically the ones in winter, bring moderate to heavy rain in low-lying areas and heavy snow to mountainous areas of the Indian Subcontinent. They are the cause of most winter and pre-monsoon season rainfall across northwest India. Precipitation during the winter season has great importance in agriculture, particularly for the rabi crops. Wheat among them is one of the most important crops, which helps to meet India’s food security. An average of four to five western disturbances form during the winter season. The rainfall distribution and amount varies with every western disturbance.

neg: Civil disturbances in Western Australia require diligent examination of sources. Some are unlikely to show up in newspaper reports at all. In some cases incidents need checking and more accurate dating. - see also Riots at Fremantle Prison between this date and 1988 Civil disturbances in Western Australia Civil disturbances in Western Australia include race riots, prison riots, and religious conflicts – often Protestant versus Catholic groups. The earliest civil disturbances were actions by the local indigenous population dealing with European settlers. Demonstrations and protests are linked to a range of issues over time. In the convict era, there were collective actions by convicts. Organised

neg: Climate of Gwadar is recorded on 27 November 2003. Winter rain showers occur in this month due to Western disturbances. The highest rainfall of this month is in 1963 while the average is and the 24-hour rain in this month is occurred on 24 November 1963. December is the month in which the cold wave hits the city because Gwadar is close to the sea making December a mild month. Western disturbances cause heavy showers in this month that decreases the temperature. The highest temperature is recorded on 8 December 2005 while the lowest temperature is recorded on 15 December 2003. Heavy downpour

neg: Climate of West Bengal out of the state.It is the season of Family re-union and enjoyment.It is the season for Feeling togetherness. Winter season is experienced in the state from mid-November to February, with January being the coldest month. Winter is cold to mild over the plains with average minimum temperatures of 9 to 16 °C. A cold and dry northern wind blows in the winter, substantially lowering the humidity level. However some rainfall may be received from the Western Disturbances. However, the Darjeeling Himalayan hill region experiences a harsh winter, with occasional snowfall at places.In the northern plain district like Jalpaiguri, Coochbehar, Alipurduar

neg: Climatic regions of India Climatic regions of India India has a large variation in climate from region to region, due to its vast size. India experiences climate from four major climate groups. These can be further subdivided into seven climatic types. For ecological regions, see Ecoregions of India, for Regions see List of regions of India. The regions belonging to this group experience persistent high temperatures which normally do not go below 18 °C in any month. The Western Coastal Plains, and the Western Ghats which include South Gujarat, Konkan region of Western Maharashtra the state of Goa, the Kanara region of Western/Coastal Karnataka,

neg: Climate of India sub-tropical steppe climate. 1) The first, a tropical semi-arid steppe climate, (Hot semi-arid climate) predominates over a long stretch of land south of Tropic of Cancer and east of the Western Ghats and the Cardamom Hills. The region, which includes Karnataka, inland Tamil Nadu, western Andhra Pradesh, and central Maharashtra, gets between annually. It is drought-prone, as it tends to have less reliable rainfall due to sporadic lateness or failure of the southwest monsoon. Karnataka is divided into three zones – coastal, north interior and south interior. Of these, the coastal zone receives the heaviest rainfall with an average rainfall

neg: Disturbance (ecology) Disturbance (ecology) In ecology, a disturbance is a temporary change in environmental conditions that causes a pronounced change in an ecosystem. Disturbances often act quickly and with great effect, to alter the physical structure or arrangement of biotic and abiotic elements. Disturbance can also occur over a long period of time and can impact the biodiversity within an ecosystem. Major ecological disturbances may include fires, flooding, windstorms, insect outbreaks and trampling. Earthquakes, various types of volcanic eruptions, tsunami, firestorms, impact events, climate change, and the devastating effects of human impact on the environment (anthropogenic disturbances) such as clearcutting, forest clearing

neg: North India inhabited regions have ranged from in Dras, Jammu and Kashmir to 50.6 °C (123 °F) in Alwar, Rajasthan. Dras is claimed to be the second-coldest inhabited place on the planet (after Siberia), with a recorded low of -60 °C. The region receives heavy rain in plains and light snow on Himalayas precipitation through two primary weather patterns: the Indian Monsoon and the Western Disturbances. The Monsoon carries moisture northwards from the Indian Ocean, occurs in late summer and is important to the Kharif or autumn harvest. Western Disturbances, on the other hand, are an extratropical weather phenomenon that carry moisture

neg: 2017 North India cold wave where the temperature fell to . Three people died due to fog related accidents in North India. India's capital New Delhi witnessed minimum temperatures of . Several schools of Noida and Delhi were closed, due to the severity of the cold wave. The western disturbances which creates an upper air cyclonic circulation over Jammu and Kashmir caused rainfall in Chandigarh, which was recorded by India Meteorological Department as the heaviest rainfall in Chandigarh in the last 22 years. Five people including an army officer, died in an avalanche in Kashmir. Four members of a family were killed in avalanches in

neg: US Climate Reference Network US Climate Reference Network The US Climate Reference Network (USCRN) is a network of climate stations developed and maintained by the National Oceanic and Atmospheric Administration (NOAA), completed in 2008.. It has the long-term commitment of the Department of Commerce and the NOAA. The USCRN is made up of over 143 stations in the United States. Its purpose is to maintain a sustainable high quality network which will detect, with high confidence, signals of climate change in the US. It provides the United States with a reference network that meets the requirements of the Global Climate Observing System. The primary

neg: Climate of India eastern India, monsoon onset dates have been steadily advancing over the past several decades, resulting in shorter summers there. Altitude affects the temperature to a large extent, with higher parts of the Deccan Plateau and other areas being relatively cooler. Hill stations, such as Ootacamund ("Ooty") in the Western Ghats and Kalimpong in the eastern Himalayas, with average maximum temperatures of around , offer some respite from the heat. At lower elevations, in parts of northern and western India, a strong, hot, and dry wind known as the loo blows in from the west during the daytime; with very high

neg: Climate of Peshawar than . Winter in Peshawar starts from mid November to the end of March. Summer months are May to September. The mean maximum temperature in summer is over and the mean minimum temperature is . The mean minimum temperature during winter is and maximum is . Peshawar is not situated in the monsoon region, unlike the other northern parts of Pakistan. But occasionally monsoon currents make it as far as Peshawar causing downpours. This can be witnessed in the erratic monsoon of 2015 when the monsoon moisture was going well into eastern Afghanistan. The winter rainfall due to western disturbances

neg: Climate of Asia the monsoon moves northwards along the Western Ghats with precipitation on coastal areas, west of the Western Ghats. The eastern areas of the Western Ghats do not receive much rain from this monsoon as the wind does not cross the Western Ghats. The "Bay of Bengal Branch" of Southwest Monsoon flows over the Bay of Bengal heading towards northeast India and Bengal, picking up more moisture from the Bay of Bengal. The winds arrive at the Eastern Himalayas with large amounts of rain. Mawsynram, situated on the southern slopes of the Eastern Himalayas in Shillong, India, is one of the

neg: Bir Tawil borders are and respectively; the length of its eastern and western borders are and respectively. In the north of the area is the mountain Jabal Tawil (), located at , with a height of . In the east is Jebel Hagar ez Zarqa, with a height of . In the south is the Wadi Tawil (), also called "Khawr Abū Bard", located at . There are a few streams in Bir Tawil, which originate in Lake Nasser. Bir Tawil's climate is, according to the Köppen climate classification, a BWh hot, arid desert. During its summer months (which take up to

neg: Climate of Rajasthan drainage occurs. Sometimes floods also occur in western Rajasthan due to impervious base rocks. In some industrial and urban centers pollution has been reported occasionally. Climate of Rajasthan The Climate of Rajasthan in northwestern India is generally arid or semi-arid and features fairly hot temperatures over the year with extreme temperatures in both summer and winter. Under the Köppen climate classification the greater part of Rajasthan falls under Hot Desert(BWh) and remaining portions of the state falls under Hot Semi Arid(BSh); the climate of the state ranges from arid to semi-arid. Rajasthan receives low and variable rainfalls and thereby is

neg: Climate of Rawalpindi power generation has been identified by U.S. Aid to be between marginal to good ( to ) at 50 m height. Western Disturbance, Monsoon and localized convection currents during the summers are responsible for changing weather conditions in Rawalpindi. Following is a list and conditions provided for the change in weather conditions. winds with the intensity of fresh breeze bring along the monsoon clouds and push them against the mighty Himalayas. Most often, significant rainfall in Rawalpindi doesn't occur until these moisture laden air interact with western disturbances, producing powerful supercell thunderstorms accompanied with heavy winds, lightning and heavy to

neg: Round Mountain (Washington) in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific

neg: Governors Ridge Trail. Governors Ridge is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall.During winter months, weather is usually cloudy, but, due to high pressure systems over the

neg: Dewey Peak River. Dewey Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the

neg: Yakima Peak Naches Peak. Yakima Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over

neg: Lundin Peak west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there

neg: Kaleetan Peak west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there

neg: Chikamin Peak climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often

neg: Kendall Peak west flank and an exposed section of the trail called Kendall Katwalk has seen tragic deaths over the years, most recently September 5, 2018. The nearest higher peak is Red Mountain, to the north-northwest. Kendall Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the

neg: Mount Mystery because he admired its regal appearance in foggy weather. Mount Mystery is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks of the Olympic Range, causing them to drop their moisture in the form of rain or snowfall (Orographic lift). As a result, the Olympics experience high precipitation, especially during the winter months in the form of snowfall. During winter months, weather is usually cloudy, but, due to high pressure systems over

neg: Disturbance (ecology) and the introduction of invasive species can be considered major disturbances. Not only invasive species can have a profound effect on an ecosystem, but also naturally occurring species can cause disturbance by their behavior. Disturbance forces can have profound immediate effects on ecosystems and can, accordingly, greatly alter the natural community. Because of these and the impacts on populations, disturbance determines the future shifts in dominance, various species successively becoming dominant as their life history characteristics, and associated life-forms, are exhibited over time. Conditions under which natural disturbances occur are influenced mainly by climate, weather, and location.Natural fire disturbances for

neg: Cattle theft in India theft networks and shared in the profits in western Punjab. These were recognized by the colonial government as "key administrative intermediaries". The crime came to be known as "cattle lifting" (like shop lifting), and it was practiced by thieves, by organized mafia and by armies during conquest. Cattle theft were a source of riots and civil disturbances. Hundreds of riots erupted in colonial India over cow slaughter. The village ""muqaddam"" (chiefs) pursued peace in the village, and British administrators added laws aimed at preventing cattle theft. According to Ramnarayan Rawat, a professor of South Asian History, cattle theft (or "languri")

neg: Western Himalaya Western Himalaya Western Himalaya, refers to the western half of the Himalayan Mountain region, stretching from Badakhshan in northeastern Afghanistan/southern Tajikistan, through India (Jammu and Kashmir, Himachal Pradesh, Uttarakhand) to central Nepal. It is also known as Punjab Himalaya. All five tributary rivers of the Indus in the Punjab region (Jhelum, Chenab, Ravi, Beas, Sutlej) originate from the Western Himalaya. Included within the Western Himalayas are the Zaskar Range, the Pir Panjal Range, and parts of the Siwalik Range and the Great Himalayas. The Jhelum River rises in the Pir Panjal Range in Jammu and Kashmir state, India, and flows

neg: Climate of Gwadar weather of Gwadar as most winter rains are dumped by it. Gwadar being close to the border of Iran gets moderate to above moderate rain in this month as Western disturbances are strong near western borders of Pakistan. The highest rain for this month is recorded in 1970 while the average is . The heaviest rain in 24 hours occurred on 13 January 1970 that is . February is also very chilly in the city with lowest temperature of on 1 February 2001 while the highest temperature is recorded on 27 February 2008. Moderate intensity rains also occur in this

neg: Natural disasters in India in 100 year’s chance will occur in every 10 years by 2100. Extremes in maximum and minimum temperatures and precipitation will increase particularly over western coast and central and north-east India. The dry years are expected to be drier and wet years wetter due to Climate Change. The per capita availability of freshwater in India is expected to drop below 1000 cubic meters by 2025 because of population growth and climate change. River basins of Cauvery, Penna, Mahi, Sabarmati, Tapi, Luni and few others are already water scarce. Krishna and Subarnarekha may become so by 2025. High population density, coastal

neg: Disturbance (ecology) adaptations that help increase plant fitness necessary for survival. Disturbance (ecology) In ecology, a disturbance is a temporary change in environmental conditions that causes a pronounced change in an ecosystem. Disturbances often act quickly and with great effect, to alter the physical structure or arrangement of biotic and abiotic elements. Disturbance can also occur over a long period of time and can impact the biodiversity within an ecosystem. Major ecological disturbances may include fires, flooding, windstorms, insect outbreaks and trampling. Earthquakes, various types of volcanic eruptions, tsunami, firestorms, impact events, climate change, and the devastating effects of human impact on

neg: Climate of Rajasthan has summers as the longest season. In this time tourist activities are very low. The army reduces its patrol time. The cold weather commences early in October and comes to an end in the middle of January.The climate in the cold weather is pleasant to very cold. The state has two distinct periods of rainfall: rainfall due to the South-West Monsoon after summer and rainfall due to Western Disturbances . Rajasthan receives low and variable rainfalls and thereby is prone to droughts.Availability of water is less due to absence of rivers and lakes. Occasional floods in cities due to improper

neg: Ernakulam Muslims, and 412 Jews. The City of Ernakulam is situated in the Ernakulam District of Central Kerala in India. Ernakulam is located at . It has an average elevation of . Under the Köppen climate classification, the City of Ernakulam features a Tropical monsoon climate. Since the region lies in the south western coastal state of Kerala, the climate is tropical, with only minor differences in temperatures between day and night, as well as over the year. Summer lasts from March to May, and is followed by the South-west monsoon from June to September. October and November form the post

neg: Micropsia turn only affects one half of the visual field and is accompanied by other cerebral visual disturbances. The most common cause of seizures which produce perceptual disturbances such as micropsia and macropsia is medial temporal lobe epilepsy in which the seizures originate in the amygdala-hippocampus complex. Micropsia often occurs as an aura signalling a seizure in patients with medial temporal lobe epilepsy. Most auras last for a very short period, ranging from a few seconds to a few minutes. Micropsia can result from the action of mescaline and other hallucinogenic drugs. Although drug-induced changes in perception usually subside as the

neg: Ctenophora with two adjacent comb rows, and in some species runs all the way along the comb rows. This forms a "mechanical" system for transmitting the beat rhythm from the combs to the balancers, via water disturbances created by the cilia. The Lobata have a pair of lobes, which are muscular, cuplike extensions of the body that project beyond the mouth. Their inconspicuous tentacles originate from the corners of the mouth, running in convoluted grooves and spreading out over the inner surface of the lobes (rather than trailing far behind, as in the Cydippida). Between the lobes on either side of

neg: Tropical Ocean Global Atmosphere program Tropical Ocean Global Atmosphere program The Tropical Ocean Global Atmosphere program (TOGA) was a ten-year study (1985-1994) of the World Climate Research Programme (WCRP) aimed specifically at the prediction of climate phenomena on time scales of months to years. TOGA emphasized the tropical oceans and their relationship to the global atmosphere. Underlying TOGA is the premise that the dynamic adjustment of the ocean in the tropics is far more rapid than at higher latitudes. Thus disturbances emanating from the western Pacific Ocean (such as El Niño) may propagate across the basin on time scales of weeks compared to years for

neg: Ruby Mountain (Washington) west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely

neg: Cutthroat Peak coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience

neg: Burroughs Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely

neg: Image Lake coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains, which surround Image Lake. As fronts from approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest

neg: Jumbo Mountain Jumbo Mountain Jumbo Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperate climate and proximity to the Pacific

neg: Devils Thumb (Washington) Devils Thumb (Washington) Devils Thumb is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperate climate and proximity to the

neg: White Chuck Mountain White Chuck Mountain White Chuck Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snowfall onto the Cascades (Orographic lift). As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperate climate and proximity to

neg: Graybeard Peak Diablo Lake via Fisher Creek. Graybeard Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Due to its temperate climate and proximity

neg: Mount Bute entire Coast Mountains range. Like Bute Inlet, the mountain was named in 1792 by Captain George Vancouver to honor John Stuart, 3rd Earl of Bute who was Prime Minister of Great Britain from 1762 to 1763. Stuart's grandson Charles Stuart was a master's mate on George Vancouver's "Discovery". The mountain's name became official in 1963 when approved by the Geographical Names Board of Canada. Based on the Köppen climate classification, Mount Bute is located in a marine west coast climate zone of western North America.. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains

neg: South Asia in the plains down below. For most part, the climate of the region is called the Monsoon climate, which keeps the region humid during summer and dry during winter, and favours the cultivation of jute, tea, rice, and various vegetables in this region. South Asia is largely divided into four broad climate zones: Maximum relative humidity of over 80% has been recorded in Khasi and Jaintia Hills and Sri Lanka, while the area adjustment to Pakistan and western India records lower than 20%–30%. Climate of South Asia is largely characterized by monsoons. South Asia depends critically on monsoon rainfall. Two

neg: Guye Peak the region, Guye Peak has wet-climate hazards such as mossy or otherwise slippery rocks in the summer and avalanches in the winter. At least eight climbers have died in falls on Guye Peak, including the mathematician Oded Schramm in 2008. Guye Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall onto

neg: Vichy France Until 1962, France possessed four small, non-contiguous but politically united colonies across India, the largest being Pondicherry in Southeast India. Immediately after the fall of France, the Governor General of French India, Louis Alexis Étienne Bonvin, declared that the French colonies in India would continue to fight with the British allies. Free French forces from that area (and others) participated in the Western Desert campaign, although news of the death of French-Indian soldiers caused some disturbances in Pondicherry. The French possessions in Oceania joined the Free French side in 1940, or in one case in 1942. They then served as

neg: Kanitkar Kanitkar Kanitkar is a surname used by Konkanastha Chitapavan sub-caste of Brahmins in India. Kanitkars, like most other Konkanastha Chitpavan Brahmins, originate in the Konkan strip on the western seacoast of India - about 300-500 kilometers south of Mumbai. Kanitkars (other names: Satkar) were from original five towns and 23 descendant families, spread to 110 towns by 1988. Kanitkars belong to Kaushik Gotra, and consider Shri Vyadeshwar at Guhaghar, Maharashtra, India as their primary "family god" [Kul Daivat]. A large majority of Kanitkars still live in Pune, Maharashtra, India - with the rest in Mumbai, Vadodara and many other cities.

neg: Wooden idols of India Wooden idols of India Wooden idols have traditionally been made in India, as a tractabe and commonly-available material to artists and craftsmen in architecture and sculpture. Few specimens survive of early works due to the perishable nature of wood, particularly ina hot and humid climate. However, other sources demonstrate the ancient use of woodcarving in Indian art. This includes a tradition of making icons, often also of wood. The Earliest Reference The earliest reference to any wooden idol made in India goes to the legend of Jīvantasvāmī – a sandalwood image of Mahāvīra or Vardhamāna, the last Tīrthaṅkara of Jain

neg: Climate resilience are least responsible for the phenomenon of climate change are also the ones who are going to be most negatively affected by future environmental disturbances. The same is true in urban centers. Those who are most responsible for climate change are going to disproportionately feel the negative effects of climatic disturbances when compared to their poorer, more vulnerable counterparts in society. Just like the wealthier countries have worked to create the most pollution, the wealthier subpopulations of society who can afford carbon-emitting luxuries like cars and homes undoubtedly produce a much more significant carbon footprint. It is also important to

neg: Climate of India climate zone: it receives between of rainfall each year in the western part, and in the eastern part. The coolest month of the year, on average, is January; April and May are the warmest months. Average temperatures in January range from , and average temperatures in April range from . July is on average the coldest and wettest month: over of rain falls on the delta. A tropical arid and semi-arid climate dominates regions where the rate of moisture loss through evapotranspiration exceeds that from precipitation; it is subdivided into three climatic subtypes- tropical semi-arid steppe, arid climate, tropical and

neg: Climate of Agra level of humidity. During summer, the daytime temperature hovers around 46-50 °C. Nights are relatively cooler and temperature lowers to a comfortable 30 °C. Winters are bit chilly but are the best time to visit Agra. The minimum temperature sometimes goes as low as 2 or 3 °C but usually hovers in the range of 6 to 8 °C. The monsoon and the Western Disturbance are the two main factors which alter the weather over Agra; otherwise, Continental air prevails for rest of the year. Like most cities of North western India, the weather and climate of Agra is extreme

neg: Climate resilience these impending climate disasters both before and after the occur, human populations are able to decrease their vulnerability to these disturbances. A major element of building and maintaining human resilience is public health. The institution of public health as a whole is uniquely placed at the community level to foster human resilience to climate-related disturbances. As an institution, public health can play an active part in reducing human vulnerability by promoting “healthy people and healthy homes.”) Healthy people are less likely to suffer from disaster-related mortality and are therefore viewed as more disaster-resilient. Healthy homes are designed and built to

neg: Climate of Uttar Pradesh and floods due to unpredictable rains, the summers are extremely hot, winters cold and rainy season can be either very wet or very dry. Indian Meteorological Department (IMD) breakdowns the climate of India into the following seasons: This classification is primarily Monsoon centric given the vast effect that it casts on the lives and agriculture of India. The climate of Uttar Pradesh is generally defined to be "tropical monsoon type". However based on the Köppen climate classification, it can be classified mostly as "Humid Subtropical with dry winter (CWa) type" with parts of Western U.P. as "Semi-Arid (BS) type" (refer

neg: Climate of India prevails over most of inland peninsular India except for a semi arid rain shadow east of the Western Ghats. Winter and early summer are long and dry periods with temperatures averaging above . Summer is exceedingly hot; temperatures in low-lying areas may exceed during May, leading to heat waves that can each kill hundreds of Indians.The rainy season lasts from June to September; annual rainfall averages between across the region. Once the dry northeast monsoon begins in September, most precipitation in India falls on Tamil Nadu, leaving other states comparatively dry. The Ganges Delta lies mostly in the tropical wet

neg: William Wilberforce Bird (governor) including on occasions when he had to deal with civil disturbances involving local people. He was involved in both financial and judicial work before being appointed to the Supreme Council of India, of which in due course he became president when the then Governor-General of India was absent. He served as Deputy-Governor of Bengal Presidency throughout the period when Lord Ellenborough was Governor, standing in for him while Ellenborough was engaged in the North-Western Provinces. Bird then replaced Ellenborough as Governor-General of India, acting in that capacity until the arrival of Sir Henry Hardinge from England in 1844. Hardinge reappointed

neg: Climate of India and precipitation. Groupings are assigned codes (see chart) according to the Köppen climate classification system. A tropical rainy climate governs regions persistent to warm or high temperatures, which normally do not fall below . India hosts two climatic subtypes- tropical monsoon climate, tropical wet and dry climate that fall under this group. 1) The most humid is the tropical wet climate—also known as a tropical monsoon climate—that covers a strip of southwestern lowlands abutting the Malabar Coast, the Western Ghats, and southern Assam. India's two island territories, Lakshadweep and the Andaman and Nicobar Islands, are also subject to this climate.

neg: Climate of Uttar Pradesh of the Indian Monsoon is the major bearer of rain in most parts of U.P. It is the South-West Monsoon which brings most of the rain here, although rain due to the "western disturbances" and North-East Monsoon also contribute small quantities towards the overall precipitation of the state. The rain in U.P. can vary from an annual average of 170 cm in hilly areas to 84 cm in Western U.P. Given the concentration of most of this rainfall in the 4 months of Monsoon period, excess rain can lead to floods and shortage to droughts. As such these two phenomenons

neg: Perry The majority of perry pear varieties in the UK originate from the counties of Gloucestershire, Herefordshire and Worcestershire in the west of England; perry from these counties made from traditional recipes now forms a European Union Protected Geographical Indication. Of these perry pear varieties, most originate in parishes around May Hill on the Gloucestershire/Herefordshire border. The standard reference work on perry pears was published in 1963 by the Long Ashton Research Station; since then many varieties have become critically endangered or lost. There were over 100 varieties, known by over 200 local names, in Gloucestershire alone. These local pears are

neg: Climate of Rawalpindi except that usually it is a few degrees warmer. Most nights are cool and days are warm with an average low and high of and , respectively. Overcast for several days is not uncommon during this month with the least amount of sunshine experienced during this month. A record high of recorded on 28 February 1985, while the coldest on 8 February 1978 have been recorded. Average rainfall is relatively greater than January totaling to . In 2013, record rainfall of and a thunderstorms breakout was experienced from three western disturbances that caused bizarre conditions of frequent hailstorms and wind

neg: March 2015 North India unseasonal rain 80 farmers attempted suicide in March alone. It is recorded as the wettest March in 48 years. “Usually, from February, western disturbances tend to subside. But this year, not only were the disturbances more active, they extended up to April. Also, there was an induced low pressure, which pulled moisture both from the Bay of Bengal and the Arabian Sea. This led to heavy and frequent showers in March In March, 62.5 millimetres of rainfall were recorded, almost 100 per cent more than normal (32.1 millimetres) and the highest in the past 100 years (in 1915, it was 78 millimetres).The

neg: Preacher Mountain Preacher Mountain Preacher Mountain is a broad summit located in King County of Washington state. It's located at the western edge of the Cascade Range and is within the Alpine Lakes Wilderness on land managed by Mount Baker-Snoqualmie National Forest. The nearest higher peak is Kaleetan Peak, to the southeast. The Pulpit is situated 2.19 miles to the northwest. Precipitation runoff from the mountain drains into tributaries of the Snoqualmie River. Preacher Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade

neg: Inner Constance south side drains into tributaries of the Dosewallips River. Inner Constance is located in the eastern portion of the Olympic Mountains. This location results in less precipitation than Mount Olympus and the western Olympics receive. Inner Constance is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks of the Olympic Range, causing them to drop their moisture in the form of rain or snowfall (Orographic lift). As a result, the Olympics experience

neg: Udhampur sub tropical. Summer temperatures don't cross 40 degrees while in winters mercury generally dips to 2 degrees or even sometimes to zero. Heavy downpour is also experienced. The annual rainfall is 130 cm mainly in monsoons and winters due to Western Disturbances. Ramnagar town nearby experiences heaviest annual rainfall in a year. Udhampur rarely experiences snow fall while there may be snow in upper reaches. However, due to changing climate patterns snowfall has been experienced in some years. In the year 2011 it snowed and there was about 15 cm snow. Heavy hailstorms with piles of hail can be experienced

neg: Basholi enjoy. It receives winter rainfall from western disturbances and summer rainfall from monsoons. Cold winter and pleasant summer are the main attractions of this place. Many Tourist Melas are organized by the Tourist Department of J&K Govt to promote tourism in the area. Tourist Huts are also proposed to be constructed. It is served by bus service available from Basohli (tehsil HQ). A small town on Basohli-Dhar mahanpurIt is situated at a height of 3700 ft. It is a ridge flanked with thick CHIR, DEODAR and SHRUBS. It experiences temperate type of climate . Cold winter and pleasant summer are

neg: Climate of Karachi bring brief, cold spells to the region, dropping the night temperatures to below 10 degrees Celsius. Western Disturbances from the Persian Gulf and Iran affect the city during this time, bringing with them light rainfall. The highest rainfall during this month was , which was recorded in 1995. The highest temperature of was recorded on 16 January 1965. The average high for the month is 25.6 °C while the average low for the month is a mild 12 °C. The cold waves can affect the metropolis till the middle of the month, after which a warming trend begins in the

neg: Climatic regions of India The region towards the North, East and South of the Tropical Desert zone running from Southern Punjab, Haryana and, Western Uttar Pradesh to Gird and Malwa regions in Western Madhya Pradesh and eastern fringes of Rajasthan and from there onwards to the Central Gujarat and Kathiawar regions of Gujarat state experience this climate type. India's capital city Delhi lies in this climatic zone. This climate is a transitional climate falling between tropical desert and humid sub-tropical zone, with temperatures which are less extreme than the desert climate. The annual rainfall is between 30 and 65 cm but is very unreliable

neg: Maini semi-arid climate, with very hot summers and cold winters. Winter starts in mid-November and ends in late-March, while summer months are from May to September. The mean maximum summer temperature surpasses during the hottest month, and the mean minimum temperature is . The mean minimum temperature during winter is , while the maximum is . Here the rainfall occurs in both winter and summer because it is a monsoon region which comes under both the Malakand and Hazara zonal rainfall regions. Due to western disturbances, the winter rainfall shows a higher record between the months of February and April. Wind

neg: Pinus albicaulis communities is attributed to various causes, most significantly infection with white pine blister rust, recent outbreaks of mountain pine beetles (2000–2014), disturbances in wildland fire ecology (including fire suppression), forest succession, and climate change. A study in the mid-2000s showed that whitebark pine had declined by 41 percent in the western Cascades due to two primary threats: blister rust and pine beetles. Whitebark deaths in North Cascades National Park doubled from 2006 to 2011. Many stands of "Pinus albicaulis" across the species entire natural range are infected with white pine blister rust ("Cronartium ribicola"), a fungal disease introduced from Europe.

neg: Rajouri the night of 15 September 1965, was later awarded the title "King of Rajouri" by the Government of Pakistan. Rajouri is located at . It has an average elevation of 915 metres (3001 feet). The climate of Rajouri is somewhat cooler than the other areas of Duggardesh plains. Summers are short and pleasant. The summer temperature generally does not exceed 41 degrees. Winters are cool and chilly characterized with rainfall due to western disturbances. Snowfall is scanty but may occur in cool months like that of December 2012. Average rainfall is 769 millimetres (26.3 in) in the wettest months. At

neg: Climate of Quetta ends in late May, with average temperatures close to . Unlike most of Pakistan, however, Quetta does not have a monsoon of sustained, heavy rainfall. The highest rainfall during a 24-hour period is recorded on 17 December 2000; the highest monthly rainfall is , which was recorded in March, 1982; and the highest annual rainfall recorded is in 1982. The principle mode of precipitation in winter is snow, falls mostly in December, January, February and sometimes even in March. The monthly breakup of the weather in Quetta is as follows: January is the coldest month in Quetta, and Western Disturbances

neg: Climate of Quetta causes rainfall with occasional snowfall in the city. The highest temperature on record on 28 January 1987; and the lowest temperature is , recorded on 8 January 1970. The highest monthly rainfall recorded was in 1982; while the most rain in a 24-hours period was on 30 January 1982. January is the most probable month for snow. Western disturbances are at the peak of their season, and the combination of wintriness makes this month most suitable for the season's heavy snow. All the decades of this month are crucial for the snow to fall. During the past years the city

neg: Courtallam Courtallam Courtallam or Kuttalam, Spa of South India, is a panchayat town situated at a mean elevation of on the Western Ghats in Tirunelveli District of Tamil Nadu, India. Many seasonal and few perennial rivers such as the Chittar River, the Manimuthar River, the Pachaiyar River and the Thamirabarani River originate in this region. The numerous waterfalls and cascades along with the ubiquitous health resorts in the area have earned it the title the Spa of South India. The falls carry a good amount of water only when there is a rain on the hills. The season begins from June

neg: Charles Alfred Elliott directors, under the provisions of the Government of India Act 1853 (16 & 17 Vict c 95), one of fifteen members of the civil service of the East India Company (Despatch, 1 October 1856). He was learning his work unattached to any district, when the mutiny broke out at Meerut, and he was then posted on 12 June 1857 as assistant magistrate to Mirzapur in the Benares division of the North Western Provinces. That large district of 5238 square miles was the scene of fierce conflicts with the rebels. Elliott led several small expeditions from headquarters to quell disturbances, was

neg: Sangaria, India &""tallest mandir of the Asia"". Udaasin Panth is the branch of the Snaatan Dharma originate by Lord Guru Nanak Dev elder son Baba Shri chand Bhagwan. One Of The Most Popular Area In Sangaria Is Maharaja Aggarsain Park, situated in Gupta Colony, ward 04. sangaria is the one of the fully developed area of rajasthan. Sangaria, situated at 29°5′N to 30°6′N and 74°3′E to 75°3′E, shares its boundaries with Haryana state to the east, Sriganganagar district to the west, Punjab state to the north and Churu district to the south. The geographical area of the district is . The climate

neg: El Cajas National Park the Cuenca area. Two of the four rivers of Cuenca originate from Cajas, the Tomebamba and Yanuncay rivers which eventually drain into the Amazon river. The Paute river also links to the Amazon. As the park straddles the continental divide, its western drainage, the Balao and Cañar link to the Pacific ocean. The modern road crosses the continental divide at the pass "Tres Cruces" (4,255 m). This section is the most western part of the continental divide of South Americas. The climate shows an average temperature of 13.2 °C and an average annual precipitation of 1,072 mm. Clouds typically drift

neg: Pichu Pichu removal of the western flank of the volcano was also originally considered to be the result of glacial erosion. A series of hills at the base of Pichu Pichu may be erosion products of moraines or moraines proper associated with the volcano. The climate of the region is relatively dry, with most precipitation falling during the summer months. The Poroto and Polobaya rivers originate at the foot of Pichu Pichu and are tributaries of the Rio Chili. The proposed Yanaorco–Paltaorco reservoir would also draw water from the mountain. Between elevation, shrub vegetation occurs on Pichu Pichu and the neighbouring volcanoes,

neg: Big Bear Mountain Big Bear Mountain Big Bear Mountain is a 5,641 ft summit at the western edge of the North Cascades, in Snohomish County of Washington state. It is located midway between Three Fingers to its north, and Liberty Mountain to its south. Big Bear Mountain is situated in the Boulder River Wilderness on land administered by the Mount Baker-Snoqualmie National Forest. Big Bear Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced