Troubled galaxy Destroyed Dreams: Chapter 254
Palash Biswas
Iranians fired up over election
UN set to adopt tougher N.Korea sanctions
Monsoon delayed, may reach city by June 20Times of India - 16 hours ago NAGPUR: It's a delayed monsoon, at least for central India. There are no signs of the south-west monsoon reaching Vidarbha and central India for another ... India soybean ends up on monsoon lull; soyoil eases Reuters India Monsoon stuck for a week: Met Office Times of India India soybean futures rise on monsoon delay Reuters India India soybean seen up on monsoon lull, Malaysia palmReuters India - 12 hours ago MUMBAI, June 12 (Reuters) - Indian soybean and soyoil futures may open higher on Friday on forecast of a week-long monsoon lull and tracking gains in ... India soybean ends up on monsoon lull; outlook bullish Reuters India India guar futures up on lower acreage, monsoon lull Reuters India India chana, guar up on demand, subdued monsoon Reuters India Airlines offering heavy discounts this monsoonTimes of India - 17 hours ago ... offers are in fact attempts to shore up the bottom line during the lean period of monsoon, generally spread over the months of July to September. ... Monsoon session of legislatureExpress Buzz - 12 hours ago BANGALORE: The monsoon session of the state legislature will begin from July 9 and is likely to be held till July 24. The state Cabinet which met here on ... Karnataka Assembly session from Jul 9 SahilOnline Move to ban sex, violence in films Mangalorean.com Monsoon effect: Airlines slash fares to boost demandMoneycontrol.com - Jun 11, 2009 With demand still not optimal and monsoons around the corner, most carriers have slashed airfare in a bid to woo passengers back to the plane. ... Guar: Firm on poor monsoon advancementCommodity Online - 7 hours ago Guar futures which surged by almost 3% in the last 2-3 days on the IMD's prediction that the monsoon rains are expected to extend the weak phase for next 1 ... India guar seed futures lower on profit-taking Reuters India NCDEX Guar Seed July Sell below 1800 Commodity Online NCDEX Guar June buy on dip at 1750-1760 Commodity Online HC order won't affect pre-monsoon workSakaal Times - 10 hours ago There was concern that the High Court order would prevent the municipal corporation from carrying out the annual pre-monsoon trimming. ... Eight new trees for every tree cut: PMC Times of India PMC to shift stray dogs from Phursungi, Urali Times of India Ready for the rains? Sakaal Times Centre readies plan to flush out Maoists after monsoonEconomic Times - Jun 10, 2009 The post-monsoon offensive is expected to be a time-bound counter-operation that will essentially focus on the extremist-infested ... MSU to sow 700 saplings of medicinal plants this monsoonIndian Express - 21 hours ago Prof Arun Arya, head of Botany department, said: “We are going to plant all the trees during monsoon. The university authorities have already granted ... Jet, SpiceJet offer monsoon specialsMoneycontrol.com - Jun 10, 2009 Jet Airways, Jet Airways Konnect, JetLite and SpiceJet are offering special fares for a limited period ending June 13. Spice's offer is between June 10 and ... |
I woke up this morning while the Telephone rang once again!
It was a call from United sates once again!
Chetan, the nephew of Rajesh Rahul was calling! He has gone through my blogs and was asking for Feed backs! He wants to know more. I suggested him to talk to our friend URMILESH, a senior journalist in Hindustan Times based in New Delhi. He informed me that he has already talked to URMILEH two years back while he was in India.
URMILESH saw Rajesh Rahul last in 2000. Since then he MISSED and no one knows his whereabouts.
`My villagers got a news from MUMBAI some six years ago that Rajesh was seen in Mumbai, but we couldnot trace out', he repented.
I stayed with URMILESH in JNU. I landed in JNU from ALLAHABAD University where I had some serious difference of opinion with my research guide as I wanted to work on the Impact of Industrialisation and Urbanisation on Indian English Novel.
Manglesh Dabral was the literary editor in AMRIT Prabhat. I was writing for the newspaper since I landed in Allahabad directly from the Himalayas. I had applied for editorial job there, but the recruiting journalist , the powerful news editor Jagadish Mathur rejected my application as he declared me disqualified. Anil Sinha from Patna and some others were recruited.
In those days, I had already stopped to get any help from home and had to earn. Bhairab Prasad Gupta, Amarkant and Markendey helped me a lot. Shailesh Matiyani was also very cooperative. In those days, the writers, artists and poets based in Allahabad were connected like a family.I was staying with Shekhar Joshi in 100, Lukerganj. Manglesh and Biren Dangwal were staying in LOOKERGANJ just a BLOCK away. I was treated as a KUMUNI Student and all the Kumauni people in Allahabad were in my side.
Back in Nainital I had been associated with CHIPKO Movement as well as UTTARAKHAND Sangharsha Bahini. Then I was working for Nainital Samachar and Pahar. I was a regular contributor in Dainik Parvatiya.Since GIC days, I had been writing.
But I found it quite difficult for sustenance in Allahabad as Allahabad had Never been a Catchy Date Line. During seventies, Nainital was a better Date Line and after all I was at home.
I shifted to MOMFORDGANJ. I had some translation job in Mitra Prakashan, nothing else. I had to walk from Momfordganj to Mitra Prakashan Office or Northern India group. I got some friends in PSO as well as SFI who helped me a lot and I also got some TUTIONS. Ramji Roy, Chittya Ranjan Singh, Rajendra Mangaj,Neelabh, DK Yadav, Ravi and Nisha were amongst my friend circle.
But I could not manage my sustenance very well. Then, Manglesh and Birenda suggested me to shift in JNU as I could work as a FREE Lance journalist there and could join the centralised Mainstream of Indian Intelligentsia.
I left ALLAHABAD with URMILESH and stayed with him in POORVANCHAL. Very soon I was in the team. It was URMILESH who introduced me to Gorakh Pandey and Rajesh Rahul.
We NEVER encountered the PLAINS but our life style was very PLAIN. We could be convinced by anyone logically. When URMILESH visited Dhanbad and suggested me to spend some time there as a journalist, I NEVER knew the Fall OUT.
Ironically, URMILESH had to leave JNU due to his ENCOUNTER with DR NAMVAR Singh, then the Dean of Humanities. He also turned to be a Journalist.
All these memories come back like Potential MONSOON.
While Chetan enquired about Rahul`s marital status ,I was Swept by MONSOON Memories in our childhood. He is ADAMENT to everything about his uncle. We discussed the REACTION on us after the SUICIDE of our friend, philosopher and Poet Gorakh Pandey. We Never know whether it connects to the Disillusionment leading to personality Disorder and Drug addiction.
But I tried to convince Chetan that he should be proud of his MISSING Uncle as he had been more committed to anyone of us!
WHY RAJESH DISconnected HIMSELF FROM HIS FAMILY back in Azamgarh, Chetan wanted to know again and again. And it was to be in another time which lands me right into my Childhood.
I told Chetan that, sometimes , Family also outcasts the member. As it happened with my CHHOTOKAKA.
We believed that he could do anything! He was a TECHNICAL Wizard and could repair any Damn thing.
He was very smart and attractive and was very popular among the ladies.Thus, he was not happy with the arranged Marriage thurst Upon him.
Shankar Roy had been the main activists there. In Dhanbad and Ranchi , we were active as NAV JANVADI Snaskritik Morcha and so many meetings held at our home. There Professor Prabhakar Singh, Manmohan Pathak, Dr BB Sharma, Madan Kashyap, Srinarayan Samir often joined us. Maheshwar and BB Pandey also visited us.
Greatest Atom Bomb happens to be the Himalayas | Palash Speaks
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Bibilography: Water Related Hazards in the Himalaya
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Floods in Bangladesh: History, dynamics and rethinking the role of ...
Appendix 5.10: 1978 – A ''dry year'' for Bangladesh .......... 336 ... cesses in the Himalayas and the floods in the lowlands; ...
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The holy Himalaya: a geographical interpretation of Garhwal - Google Books Result
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FLASH FLOODS: CAUSES, CONSEQUENCES AND ITS MANAGEMENT IN INDIAN ...
The flash floods of Bhagirathi in 1978, Sutlej in 1993 and 2000 and ... river basins of the Indian Himalayas suggest that the river was blocked many times, ...
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FLOOD MANAGEMENT IN GANGA-BRAHMAPUTRA-MEGHNA
18 Nov 1986 ... According to the flood cycle in the Ganges, the flow goes down from October ... on the other side of the Himalayas before it enters Arunachal Pradesh. .... Out of these years, the floods of 1978 and 2000 were most severe ...
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1978 : • Tatopani village settled on lower terrace (+30 m) of the. Kali Gandaki ... evidence for past floods and aggradation induced by landsliding ...
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LEARNINGS FROM THE YAMUNA FLOODS OF AUGUST 2008
21 Aug 2008 ... The flood in 1978 is considered as the highest flood in recent memory ... Himalayas stretching up till the month of March 2008 in some areas ...
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Hydrological Disasters - Google Books Result
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grave danger: deforestation in the Himalayas aggravating floods”. ..... In 1978 and 1986, years of very low flood dimension in Bangladesh, the ...
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Low-frequency of southern Asian monsoon variability using a 295-year record from the Dasuopu ice core in the central Himalayas
Tibetan Plateau Research Institute, Chinese Academy of Science, Beijing, China
Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Science, Lanzhou, China
Tibetan Plateau Research Institute, Chinese Academy of Science, Beijing, China
Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Science, Lanzhou, China
Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA
A better understanding of the spatial and temporal variability of rainfall in the Himalayas should be extremely important to improve our understanding of Asian monsoon dynamics. There is little that is understood about rainfall variability at the high Himalayas with elevation over 7000 m a.s.l. Here a high-resolution snow accumulation record from a well dated Dasuopu ice core from central Himalayas reflects low-frequency variability of monsoon precipitation over the last 295-year. MultiDecadal to centennial variations in the Dasuopu snow accumulation (DSA) are in-phase (out-of-phase) with that in monsoon rainfall of northeast Indian, Nepal and Bangladesh (southern India) over the period 1901–1995. The record shows the monsoon in central Himalayas had weakened in 18th century and strengthened throughout much of 19th and early 20th century, and then weakening again from early 1920s to the present.
Monsoon Climate Changes Influence Himalayas
Posted on: Tuesday, 11 November 2008, 10:15 CST
Data from seafloor drilling in South China Sea establish new record
Throughout history, the changing fortunes of human societies in Asia have been linked to variations in the precipitation resulting from seasonal monsoons.
A new paper published online this week in the journal Nature Geoscience suggests that variations in monsoon climate over longer time scales also influenced the evolution of the Himalaya mountain chain, the world's highest.
The climate over much of Asia is dominated by seasonal winds that carry moist air over the Pacific Ocean into East Asia and over the Indian Ocean into South Asia.
The East and South Asian monsoons are responsible for most of the rainfall in these regions. Although the time when these monsoon patterns were first established is unknown, many lines of evidence suggest that they first came about at least 24 million years ago.
The new study uses geochemical data from an Ocean Drilling Project sediment core extracted from the seafloor of the South China Sea to establish a record of the East Asian monsoon climate over that time interval.
"This synthesis of climate and tectonic studies, from Himalayan rocks to ocean floor sediments, has revealed the ancient history of a dynamic part of our planet," said James Dunlap, program director in the National Science Foundation (NSF)'s Division of Earth Sciences, which funded the research. "These results will guide us in our efforts to better understand the potential for change on Earth today."
Sediments in this core were eroded from the drainage area of the Pearl River system in China, according to Peter Clift, a geologist at the University of Aberdeen in Scotland and lead author of the paper. "Their chemistry records the relative intensity through time of chemical weathering in an area that received the bulk of its precipitation from East Asian monsoon storms."
Many researchers believe that a geologically "abrupt" uplift of the Tibetan Plateau--the largest high-altitude region on Earth, with an average elevation of more than 4,000 meters (13,000 feet)--8 to 10 million years ago caused a major intensification in the monsoon climate.
"South China Sea data do not support that interpretation," said Kip Hodges, a co-author of the paper and geologist at Arizona State University.
The pattern in the core suggests a steady increase in East Asian monsoon intensity from 23 to 10 million years ago, followed by a steady weakening until about 4 million years ago.
"After that, the intensity began to increase once more," said Hodges. "The implication is that either the development of the plateau was not as abrupt as we might have thought, or that an abrupt uplift of the plateau at 8 to 10 million years caused a change in precipitation patterns that was not recorded in East Asia."
Another controversy surrounds the degree of coupling between the South and East Asian monsoons. Could one have varied in intensity differently from the other?
The team compared the South China Sea record with less complete sedimentary records from the Arabian Sea and Bay of Bengal--which contain sediments that were eroded from the Himalaya, where the principal rainfall comes from South Asian monsoon storms--to argue for a linkage between the two monsoon systems over most of the past 23 million years.
The most interesting correlation was found when the team compared the sedimentary records to cooling age patterns in the Himalaya.
Compilations of the cooling ages obtained by Hodges and other researchers show that the periods of high East Asian monsoon intensity matched well with high frequencies of cooling ages, implying a relationship between monsoon intensity and erosion in the Himalaya.
"It implies, once again, that Earth is a complex system," said Hodges. "We cannot begin to fully understand mountain building without appreciating the roles of the hydrosphere and atmosphere in the evolution of mountain ranges."
But Hodges cautions that the results of this study are suggestive. "It is important to confirm our interpretations by generating a more comprehensive cooling age dataset from regions of the Himalaya that have not yet been studied because of logistical constraints or political instability."
Adds Clift, "We need more complete offshore sedimentary records from the Arabian Sea and Bengal Fan to make a solid case for linkages between the South and East Asian monsoon systems."
Other co-authors of the paper include D. Heslop of the Universität Bremen, Germany, R. Hannigan of Arkansas State University, and H. Van Long of the University of Aberdeen.
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Image Caption: Machupuchare in the Annapurna Range of the Himalaya in central Nepal is a mountain influenced by monsoons. Credit: Kip Hodges
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Monsoon
India’s climate is dominated by monsoons. Monsoons are strong, often violent winds that change direction with the season. Monsoon winds blow from cold to warm regions because cold air takes up more space than warm air. Monsoons blow from the land toward the sea in winter, and from the sea toward land in the summer.
India’s winters are hot and dry. The monsoon winds blow from the northeast and carry little moisture. The temperature is high because the Himalayas form a barrier that prevents cold air from passing onto the subcontinent. Additionally, most of India lies between the Tropic of Cancer and the equator, so the sun’s rays shine directly on the land. The temperature can reach as high as 110oF during the Indian winter.
The summer monsoons roar onto the subcontinent from the southwest. The winds carry moisture from the Indian Ocean and bring heavy rains from June to September. The torrential rainstorms often cause violent landslides. Entire villages have been swept away during monsoon rains. Despite the potential for destruction, the summer monsoons are welcomed in India. Farmers depend on the rains to irrigate their land. Additionally, a great deal of India’s electricity is generated by water power provided by the monsoon rains.
Pakistan is much drier than India. The summer monsoon winds in India bring moisture from the Indian Ocean; Pakistan is north of the ocean and receives much less rain. The Thar Desert is on the border between India and Pakistan. It covers more than 77,000 square miles, about the size of Nebraska.
Monsoon
From Wikipedia, the free encyclopedia
A monsoon is a seasonal prevailing wind that lasts for several months. The term was first used in English in India, Bangladesh, Pakistan, and neighboring countries to refer to the big seasonal winds blowing from the Indian Ocean and Arabian Sea in the southwest bringing heavy rainfall to the area.[1] In hydrology, monsoon rainfall is considered to be that which occurs in any region that receives the majority of its rain during a particular season. This allows other regions of the world such as North America, South America, Sub-Saharan Africa, Australia and East Asia to qualify as monsoon regions.[2] In terms of total precipitation and total area covered, the monsoons affecting the Indian subcontinent dwarf the North American monsoon, and the South Asian monsoon affects a larger number of people, owing to the high density of population in that part of the world.
[edit] Etymology and definition
The English monsoon came from Portuguese monção, ultimately from Arabic mawsim (موسم "season"), "perhaps partly via early modern Dutch monsun".[3] The definition includes major wind systems that change direction seasonally.
"Most summer monsoons have a dominant westerly component and a strong tendency to ascend and produce copious amounts of rain (because of the condensation of water vapor in the rising air). The intensity and duration, however, are not uniform from year to year. Winter monsoons, by contrast, have a dominant easterly component and a strong tendency to diverge, subside, and cause drought."[4][edit] History
Strengthening of the Asian monsoon has been linked to the uplift of the Tibetan Plateau after the collision of India and Asia around 50 million years ago.[5] Many geologists believe the monsoon first became strong around 8 million years ago based on records from the Arabian Sea and the record of wind-blown dust in the Loess Plateau of China. More recently, plant fossils in China and new long-duration sediment records from the South China Sea led to a timing of the monsoon starting 15-20 million years ago and linked to early Tibetan uplift.[6] Testing of this hypothesis awaits deep ocean sampling by the Integrated Ocean Drilling Program.[7] The monsoon has varied significantly in strength since this time, largely linked to global climate change, especially the cycle of the Pleistocene ice ages.[8] Timing of the monsoon strengthening of the Indian Monsoon of around 5 million years ago was suggested due to an interval of closing of the Indonesian Seaway to cold thermocline waters passage from the Pacific to the Indian Ocean which is believed to have resulted in an increased sea surface temperature in the Indian Ocean, which increased gyral circulation and then caused an increased intensity of the monsoon.[9] Sinha et al. (2006) identified five episodes during the Quaternary at 2.22 (PL-1), 1.83 (PL-2), 0.68 (PL-3), 0.45 (PL-4) and 0.04 Ma (PL-5), of weakening of Leeuwin Current (Western Australia) and postulated that the weakening of the LC would have an effect on the sea surface temperature (SST) in the Indian Ocean, as the Indonesian throughflow generally warms the Indian Ocean. Thus these five intervals could probably be those of considerable lowering of SST in the Indian Ocean and would definitely have influenced Indian monsoon intensity. They ( Sinha et al., 2006) stated that that during the weak LC there is the possibility of reduced intensity of Indian winter monsoon and strong summer monsoon, because of change in the Indian Ocean dipole due to reduction in net heat input to the Indian Ocean through the Indonesian throughflow. Thus a better understanding of the possible links between El Nino, Western Pacific Warm Pool (WPWP), Indonesian throughflow, wind pattern off Western Australia, and ice volume expansion and contraction can be obtained by studying the behaviour of the LC during Quaternary at close stratigraphic intervals.[10]
[edit] Process
Monsoons are caused by the larger amplitude of the seasonal cycle of land temperature compared to that of nearby oceans. This differential warming happens because heat in the ocean is mixed vertically through a "mixed layer" that may be fifty meters deep, through the action of wind and buoyancy-generated turbulence, whereas the land surface conducts heat slowly, with the seasonal signal penetrating perhaps a meter or so. Additionally, the specific heat capacity of liquid water is significantly higher than that of most materials that make up land. Together, these factors mean that the heat capacity of the layer participating in the seasonal cycle is much larger over the oceans than over land, with the consequence that the air over the land warms faster and reaches a higher temperature than the air over the ocean.[11] Heating of the air over the land reduces the air's density, creating an area of low pressure. This produces a wind blowing toward the land, bringing moist near-surface air from over the ocean. Rainfall is caused by the moist ocean air being lifted upwards by mountains, surface heating, convergence at the surface, divergence aloft, or from storm-produced outflows at the surface. However the lifting occurs, the air cools due to expansion, which in turn produces condensation.
In winter, the land cools off quickly, but the ocean retains heat longer. The cold air over the land creates a high pressure area which produces a breeze from land to ocean.[11] Monsoons are similar to sea and land breezes, a term usually referring to the localized, diurnal (daily) cycle of circulation near coastlines, but they are much larger in scale, stronger and seasonal.[12]
[edit] Monsoon Systems
As monsoons have become better understood, the term monsoon has been broadened to include almost all of the phenomena associated with the annual weather cycle within the tropical and subtropical land regions of the earth.
Even more broadly, it is now understood that in the geological past, monsoon systems must have always accompanied the formation of supercontinents such as Pangaea, with their extreme continental climates.[citation needed]
[edit] Northeast Monsoon (Southern Asia and Australasia)
In Southern Asia, the northeastern monsoons take place from December to early March. The temperature over central Asia is less than 25°C as it is the northern hemisphere winter, therefore creating a zone of high pressure there. The jet stream in this region splits into the southern subtropical jet and the polar jet. The subtropical flow directs northeasterly winds to blow across southern Asia, creating dry air streams which produce clear skies over India. Meanwhile, a low pressure system develops over South-East Asia and Australasia and winds are directed toward Australia known as a monsoon trough.
[edit] Northern Indian Ocean Monsoon
[edit] South-West Summer Monsoon
The southwestern summer monsoons occur from June through September. The Great Indian Desert (Thar Desert) and adjoining areas of the northern and central Indian subcontinent heats up considerably during the hot summers. This causes a low pressure area over the northern and central Indian subcontinent. To fill this void, the moisture-laden winds from the Indian Ocean rush in to the subcontinent. These winds, rich in moisture, are drawn towards the Himalayas, creating winds blowing storm clouds towards the subcontinent. However the Himalayas act like a high wall and do not allow the winds to pass into Central Asia, forcing them to rise. With the gain in altitude of the clouds, the temperature drops and precipitation occurs. Some areas of the subcontinent receive up to 10,000 mm of rain.
The southwest monsoon is generally expected to begin around the start of June and dies down by the end of September. The moisture-laden winds on reaching the southernmost point of the Indian peninsula, due to its topology, become divided into two parts:
- Arabian Sea Branch of the SW Monsoon
- Bay of Bengal Branch of the SW Monsoon
The Arabian Sea Branch of the SW Monsoon first hits the Western Ghats of the coastal state of Kerala, India and hence Kerala is the first state in India to receive rain from the South-West Monsoon. This branch of the monsoon moves northwards along the Western Ghats giving rain to the coastal areas west of the Western Ghats. It is to be noted that the eastern parts 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 SW Monsoon flows over the Bay of Bengal heading towards North-Eastern India and Bengal, picking up more moisture from the Bay of Bengal. Its hits the Eastern Himalaya and provides a huge amount of rain to the regions of North-East India, Bangladesh and West Bengal. Mawsynram, situated on the southern slopes of the Eastern Himalaya in Shillong, India is one of the wettest places on Earth. After striking the Eastern Himalaya it turns towards the West, travels over the Indo-Gangetic Plain, at a rate of roughly 1–2 weeks per state[citation needed], pouring rain all along its way.
The monsoon accounts for 80 percent of the rainfall in the country[citation needed]. Indian agriculture (which accounts for 25 percent of the GDP and employs 70 percent of the population) is heavily dependent on the rains, especially crops like cotton, rice, oilseeds and coarse grains. A delay of a few days in the arrival of the monsoon can, and does, badly affect the economy, as evidenced in the numerous droughts in India in the 90s.
The monsoon is widely welcomed and appreciated by city-dwellers as well, for it provides relief from the climax of summer heat in June.[13] However, because of the lack of adequate infrastructure in place, most major cities are often adversely affected as well. The roads, already shoddy, take a battering each year; houses and streets at the bottom of slopes and beside rivers are waterlogged, slums are flooded, and the sewers and the rare hurricane drain start to back up and pour out toxic filth rather than drain it away. This translates into various minor casualties most of the time; lack of city infrastructure coupled with changing climate patterns also causes severe damage to and loss of property and life. Bangladesh and some regions of India like in Assam and places of West Bengal experiences heavy flood, which claims huge number of lives and huge loss of property and causes severe damage to economy, as evidenced in the Mumbai floods of 2005. Also in the recent past, areas in India that used to receive scanty rainfall throughout the year, like the Thar Desert, have surprisingly ended up receiving floods due to the prolonged monsoon season.
June 1 is regarded as the date of onset of the monsoon in India, which is the average date on which the monsoon strikes Kerala over the years for which scientific data is available with the Indian Meteoreological Department.
[edit] North-East Monsoon (Retreating Monsoon)
Around September, with the sun fast retreating south, the northern land mass of the Indian subcontinent begins to cool off rapidly. With this air pressure begins to build over northern India. The Indian Ocean and its surrounding atmosphere still holds its heat. This causes the cold wind to sweep down from the Himalayas and Indo-Gangetic Plain towards the vast spans of the Indian Ocean south of the Deccan peninsular. This is known as the North-East Monsoon or Retreating Monsoon.
While traveling towards the Indian Ocean, the dry cold wind picks up some moisture from the Bay of Bengal and pours it over peninsular India. Cities like Chennai, which get less rain from the South-West Monsoon, receives rain from the Retreating Monsoon. About 50% - 60% of the rain received by the state of Tamil Nadu is from the North-East Monsoon[citation needed].
It is worth noting that North-East Monsoon (or the Retreating Monsoon) is not able to bring as much rain as the South-West Monsoon.
[edit] North American Monsoon
The North American Monsoon (NAM) occurs from late June or early July into September, originating over Mexico and spreading into the southwest United States by mid-July. It affects Mexico along the Sierra Madre Occidental as well as Arizona, New Mexico, Nevada, Utah, Colorado, West Texas, and California. It pushes as far west as the Peninsular Ranges and Transverse Ranges of southern California, but rarely reaches the coastal strip (a wall of desert thunderstorms only a half-hour's drive away is a common summer sight from the sunny skies along the coast during the monsoon). The North American monsoon is known to many as the Summer, Southwest, Mexican or Arizona monsoon.[14][15] It is also sometimes called the Desert Monsoon as a large part of the affected area are the Mojave and Sonoran Deserts.
[edit] African Monsoon
The monsoon of western sub-Saharan Africa is the result of the seasonal shifts of the Intertropical Convergence Zone and the great seasonal temperature and humidity differences between the Sahara and the equatorial Atlantic Ocean. It migrates northward from the equatorial Atlantic in February, reaches western Africa on June 22, then moves back to the south by October.[16] The dry, northeasterly trade winds, and their more extreme form, the harmattan, are interrupted by the northern shift in the ITCZ and resultant southerly, rain-bearing winds during the summer. The semiarid Sahel and Sudan depend upon this pattern for most of their precipitationed area is desert.
[edit] European Monsoon
The European Monsoon (more correctly known as the Return of the Westerlies) is the result of by a resurgence of westerly winds from the Atlantic, where they become loaded with wind and rain.[17] These Westerly winds are a common phenomenon during the European winter, but they ease as Spring approaches in late March and through April and May. Regular as clockwork, the winds suddenly pick up again in June, which is why this phenomenon is also referred to as "the return of the westerlies".[18]
The rain usually arrives in two waves, at the beginning of June and again in mid to late June. The European monsoon is not a monsoon in the traditional sense in that it doesn't meet all the requirements to be classified as such. Instead the Return of the Westerlies is more regarded as a conveyor belt that delivers a series of low pressure centres to Western Europe where they create unseasonable weather. These storms generally feature significantly lower than average temperatures, fierce rain or hail, thunder and strong winds.[19]
The Return of the Westerlies affects Europe's Northern Atlantic coastline, more precisely the British Isles, the Benelux, Western Germany, Northern France and parts of Scandinavia.
[edit] See also
[edit] References
- ^ American Meteorological Society Glossary of Meteorology. Monsoon. Retrieved on 2008-03-14.
- ^ International Committee of the Third Workshop on Monsoons. The Global Monsoon System: Research and Forecast. Retrieved on 2008-03-16.
- ^ OED online
- ^ "Monsoon". Britannica. http://www.britannica.com/eb/article-9053445/monsoon. Retrieved on 2007-05-15.
- ^ ROYDEN, L.H., BURCHFIEL, B.C., VAN DER HILST, Rob, WHIPPLE, K.X., HODGES, K.V., KING, R.W., and CHEN, Zhiliang. UPLIFT AND EVOLUTION OF THE EASTERN TIBETAN PLATEAU. Retrieved on 2008-05-11.
- ^ P. D. Clift, M. K. Clark, and L. H. Royden. An Erosional Record of the Tibetan Plateau Uplift and Monsoon Strengthening in the Asian Marginal Seas. Retrieved on 2008-05-11.
- ^ Integrated Ocean Drilling Program. Earth, Oceans, and Life. Retrieved on 2008-05-11.
- ^ Anil K. Gupta and Ellen Thomas. Initiation of Northern Hemisphere glaciation and strengthening of the northeast Indian monsoon: Ocean Drilling Program Site 758, eastern equatorial Indian Ocean. Retrieved on 2008-05-11.
- ^ M. S. SRINIVASAN and D. K. SINHA. Ocean circulation in the tropical Indo-Pacific during early Pliocene (5.6-4.2 Ma) : Paleobiogeographic and isotopic evidence. Retrieved on 2008-05-11.
- ^ Sinha,D.K., Singh,A.K. and Tiwari,M (2006). Palaeoceanographic and palaeoclimatic history of ODP site 763A (Exmouth Plateau), South-east Indian Ocean: 2.2 Ma record of planktic foraminifera. CURRENT SCIENCE, VOL. 90, NO. 10, 25 May 2006
- ^ a b Oracle Thinkquest Education Foundation. monsoons: causes of monsoons. Retrieved on 2008-05-22.
- ^ BBC Weather. The Asian Monsoon. Retrieved on 2008-05-22.
- ^ Official Web Site of District Sirsa, India. District Sirsa. Retrieved on 2008-12-27.
- ^ Arizona State University Department of Geography. Basics of Arizona Monsoon. Retrieved on 2008-02-29.
- ^ New Mexico Tech. Lecture 17: 1. North American Monsoon System. Retrieved on 2008-02-29.
- ^ Innovations Report. Monsoon in West Africa: Classic continuity hides a dual-cycle rainfall regime. Retrieved on 2008-05-25.
- ^ Visser, S.W. (1953). Some remarks on the European monsoon. Birkhäuser: Basel.
- ^ The Guardian. The Question: What is the European monsoon? Retrieved on 2009-06-09.
- ^ The Times. 'European Monsoon' to blame for cold and rainy start to June Retrieved on 2009-06-09.
- Initial text from the Goddard Space Flight Center's public domain Distributed Active Archive Center
[edit] External links
Wikinews has related news: Asian monsoon rains force millions to flee |
- National Weather Service: The North American Monsoon
- North American Monsoon Experiment
- East Asian Monsoon Experiment
- Influence of monsoon winds
- Meet the Indian monsoons at PBS.org
- Arizona Central monsoon page
- Basics of the Arizona Monsoon
- AMMA - African Monsoon Multidisciplinary Analyses
- Flooding of urban areas due to Monsoon showers, Phnom Penh-Cambodia > Video attachment
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chain, the Himalaya.
The climate over much of Asia is dominated by seasonal winds that carry moist air over the Pacific Ocean into East Asia and over the Indian Ocean into South Asia. The East and South Asian monsoons are responsible for most of the rainfall in these regions. Although the time when these monsoon patterns were first established is unknown, many lines of evidence suggest that they first came about at least 24 million years ago.
The new study uses geochemical data from an Ocean Drilling Project sediment core extracted from the seafloor of the South China Sea to establish a record of the East Asian monsoon climate over that time interval.
"Sediments in this core were eroded from the drainage area of the Pearl River system in China, and their chemistry records the relative intensity through time of chemical weathering in an area that received the bulk of its precipitation from East Asian monsoon storms," explains Peter Clift, lead author of the study and a professor of geology and petroleum geology at the University of Aberdeen in Scotland.
Many researchers believe that a geologically "abrupt" uplift of the Tibetan Plateau – the largest high-altitude region on Earth, with an average elevation of more than 4,000 meters (13,000 feet) – at 8 to10 million years ago caused a major intensification in the monsoon climate.
"South China Sea data do not support that interpretation," says Kip Hodges, a co-author of the paper and director of the School of Earth and Space Exploration in the College of Liberal Arts and Sciences at Arizona State University. "Other than a brief drop between about 17 and 15 million years ago, the pattern in the core suggests a steady increase in East Asian monsoon intensity from 23 to 10 million years ago, followed by a steady weakening until about 4 million years ago. After that, the intensity began to increase once more. The implication is that either the development of the plateau was not as abrupt as we might have thought, or that an abrupt uplift of the plateau at 8 to 10 million years caused a change in precipitation patterns that was not recorded in East Asia."
Another controversy surrounds the degree of coupling between the South and East Asian monsoons. Could one have varied in intensity differently from the other?
The team compared the South China Sea record with less-complete sedimentary records from the Arabian Sea and Bay of Bengal – which contain sediments that were eroded from the Himalaya, where the principal rainfall comes from South Asian monsoon storms – to argue for a linkage between the two monsoon systems over most of the past 23 million years.
"The really exciting moment in this research came when we began to compare patterns from one record to another and found broad agreement," says Clift.
The most interesting correlation was found when the team compared the sedimentary records to cooling age patterns in the Himalaya. Hodges and his students have spent years using isotopic dating techniques to determine the cooling ages of thousands of bedrock and sediment samples from all over the Himalaya.
"Most people are familiar with the use of such techniques to determine the crystallization ages of minerals and rocks," says Hodges. "They also can be used to determine when a mineral cooled through a certain temperature. The principal mechanism by which samples cool in mountainous regions is erosion, so a high frequency of minerals with the same cooling age generally means a high rate of erosion at that time."
Compilations of the cooling ages obtained by Hodges' group and other researchers show that the periods of high East Asian monsoon intensity matched well with high frequencies of cooling ages, implying a relationship between monsoon intensity and erosion in the Himalaya.
"While it makes sense intuitively that heavy rainfall should be correlated with more aggressive erosion, it is important to see such direct evidence of the coupling between the processes that define the evolution of mountain ranges and climatic processes," Hodges explains. "It implies, once again, that Earth is a complex system, and we cannot begin to fully understand mountain building without appreciating the roles of the hydrosphere and atmosphere in the evolution of mountain ranges."
But Hodges cautions that the results of this study are suggestive.
"It is important to confirm our interpretations by generating a more comprehensive cooling age dataset from regions of the Himalaya that have not yet been studied because of logistical constraints or political instability."
Adds Clift, "We really need more complete offshore sedimentary records from the Arabian Sea and Bengal Fan to make a solid case for linkages between the South and East Asian monsoon systems."
http://www.scientificblogging.com/news_releases/erosion_linked_monsoon_intensity_himalayas
Article: Monitoring the monsoon in the Himalayas: Observations in Central Nepal, June 2001
ABSTRACT
The Monsoon Himalayan Precipitation Experiment (MOHPREX) occurred during June 2001 along the south slopes of the Himalayas in central Nepal. Radiosondes were launched around the clock from two sites, one in the Marsyandi River basin on the eastern footslopes of the Annapurna range, and one farther to the southwest near the border with India. The flights supported rainfall and other hydrometeorological observations (including surface winds) from the Marsyandi network that has been operated in this region since the spring of 1999. The thermodynamic profiles obtained from the soundings support the observed nocturnal maximum in rainfall during the monsoon, with total column moisture ...
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The Himalayas and the Tibetan PlateauForty-five million years ago the Indian subcontinent, once a part of the supercontinent of Gondwanaland-- which had started to break up 167 million years ago-- collided with the continent of Asia. The forces moving the Indian continental plate continued pushing it under Asia. The land above was raised up to create the enormous Himalayan mountains - the tallest in the world- and the Tibetan Plateau - the largest area of high altitude land in the world. The Tibetan Plateau has an area of almost 1 million square miles (2.5 million square kilometers), with an average elevation of 14,700 feet (4,500 meters) in height. The Monsoon WindsMost winds blow in the same direction even if they only blow for part of the year. The Monsoon wind blows in opposite directions at different times of the year. As the Northern hemisphere warms in spring and summer the Monsoon wind changes directions and instead of blowing towards Africa it blows from Africa across the Indian Ocean, India and over the Himalayan Mountains into China and across the Tibetan Plateau. The monsoon reaches India in June and blows through September. The summer monsoon is a warm wind from the tropics. As it crosses the Indian Ocean it picks up vast amounts of water from the evaporation of water warmed by the sun. Rainfall as the Monsoon crosses the Himalayas and the Tibetan PlateauAs the monsoon wind comes to the Himalayan Mountains and the Tibetan Plateau, of course it has to rise to get over them. As winds rise over mountains, especially warm, moist winds, the water they contain condenses out as rain. This is called orographic lifting precipitation. But if you are on parts of the Tibetan Plateau underneath the warm, wet monsoon rising over the tallest mountains and the highest terrain in the world you don’t care what it is called - you just get very wet. Some places under the Monsoon get up to 10,000 millimeters - 400 inches - of rain a year. One inch of rain is a pretty strong rain. 400 inches is like a heavy rain every day of the year, except this falls in only four months. As the air of the monsoon descends north of the Tibetan Plateau, the opposite happens. The air is compressed as air pressure increases, relative humidity falls and you get hot, dry winds. The same winds that drench the mountains and parts of the plateau dry the Gobi and the Takla Makan deserts. Takla Makan translates roughly to “go in and you won’t come out.” The Himalayas and the Tibetan Plateau The two largest rivers of China, the Yangtze and the Yellow (Huang He) Rivers also flow from the Tibetan Plateau across the coastal plain of China to the Sea. Every year the rivers rise as they bring to the coastal plains some of the enormous amount of water that fell as rain from the Monsoon over a thousand miles away. In some years the rivers rise over their banks and flood; sometimes these floods are huge. The rivers bring more than water. The Tibetan plateau is still rising and thus is still being eroded away by these rains. The rivers are notably muddy (the Yellow River is named for its color) - full of sediment. Much of the fertile Coastal Plain of China was built up by the sediment deposits from the floods of these rivers.
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Understanding The Settlements, Ctd Atlantic Online UN vows to stay in NW Pakistan despite deadly attackReuters India - Jun 11, 2009 By Nita Bhalla NEW DELHI - The United Nations has no plans to suspend or reduce its activities in Pakistan despite Tuesday's bomb attack that killed nine people, including two foreign UN staff, in the northern city of Peshawar, UN agencies say. New bomb blast hits Pakistan city BBC News Suicide attack kills one, injures 14 in Pakistan's Peshawar Times of India Libya earmarks 11.8 bln to draw foreign investmentguardian.co.uk - 2 hours ago By Daniel Flynn and Francesca Piscioneri ROME, June 12 (Reuters) - Libya's Muammar Gaddafi, promising Italy priority access to an 11.8 billion euro plan to attract foreign investment, said on Friday his oil-rich nation could act as a gateway for ... Video: Raw Video: Gadhafi Visits Italy for 1st Time The Associated Press Obama Takes His Health Care Case to the PublicNew York Times - 13 hours ago President Obama discussing his plan to overhaul health care on Thursday in a gymnasium at Southwest High in Green Bay, Wis. By SHERYL GAY STOLBERG and ROBERT PEAR GREEN BAY, Wis. Video: Obama Confronts Critics on Health Care Overhaul The Associated Press Obama confronts critics on health care overhaul The Associated Press Kercher accused 'under pressure'BBC News - 5 hours ago The woman accused of British student Meredith Kercher's murder has told her Italian trial she felt "under pressure" from police to name a suspect. Quotes from testimony of US student The Associated Press Britain's former PM Thatcher breaks arm in fallReuters India - 2 hours ago LONDON (Reuters) - Former British prime minister Margaret Thatcher was taken to hospital on Friday after breaking her arm in a fall at her London home, her spokesman said. Lady Thatcher treated after fall BBC News |
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