Location via proxy:   [ UP ]  
[Report a bug]   [Manage cookies]                

Increasing Monsoon unpredictability and erraticism linked with rising Global Warming in the Indian subcontinent with a special reference to June 2013 excessive rainfall in Delhi. (Essay)

...Read more
Increasing Monsoon unpredictability and erraticism linked with rising Global Warming in the Indian subcontinent with a special reference to June 2013 excessive rainfall in Delhi. -Arpita Bhagat Monsoon in India is one of the most important weather phenomenon on which the entire countrys agricultural productivity and economics depends. According to Indian Meteorological Department (nodal agency for climatological observations and studies in the country), it is the seasonal reversals of the wind direction along the shores of the Indian Ocean, that blow from the southwest during one half of the year and from the northeast during the other half 1 . The former called the south-west monsoon is responsible for most of the rainfall received (June-September). Monsoons occur when the temperature on land is significantly warmer or cooler than the temperature of the ocean. These temperature imbalances are caused because the oceans and land absorb heat in different ways 2 . In addition, surface temperatures increase at a greater rate over land than ocean in simulations and observations of global warming 3 . Though the erraticism of India’s monsoons is fairly documented, research provides ample proof that global warming has added to the unpredictability and erraticism of the same. For instance, Menon et al. (2013), predict consistent increase in day-to-day rainfall variability in India under unmitigated climate change by using 20 comprehensive climate models that conclusively suggests the necessity of profound adaptation measures 4 . Also, according to predictions by Kumar et al. (2006), surface warming is monotonously widespread and extremes in both temperature and rainfall are expected to increase, especially in the west central India 5 . Delhi, located at 28.61°N 77.23°E, lies in Northern India, bordering states of Haryana on the north, west and south and Uttar Pradesh to the east 6 . Delhi features an atypical version of the humid subtropical climate, high variation between summer, winter temperatures and precipitation. Typically, the monsoon winds arrive in Delhi by either the end of June or the first week of July with Delhi receiving an average rainfall of 714 mm 7 . This year, the onset of monsoon was preponed, with the capital receiving its first showers on June 13 th 2013 8 . Plotting the data of Delhi average rainfall (mm) for the last five years and the percentage departure of the same, the following figure is obtained. 1 http://www.imd.gov.in/section/nhac/dynamic/Met_Glossary.htm 2 http://www.engineeringtoolbox.com/specific-heat-fluids-d_151.html 3 http://www.mit.edu/~pog/src/byrne_land_ocean_warming_contrast_2013.pdf 4 http://onlinelibrary.wiley.com/doi/10.1002/grl.50583/abstract 5 http://www.iisc.ernet.in/currsci/feb102006/334.pdf 6 The American Heritage Dictionary of the English Language (fourth ed.). Houghton Mifflin Company. 2000. 7 http://www.delhi.gov.in/DoIT/DOIT_DM/state%20profile.pdf 8 http://m.accuweather.com/cs/weather-blogs/andrews/south-west-monsoon-onset-four-weeks-early-1/14352257
Source: HYDROMET DIVISION, INDIA METEOROLOGICAL DEPARTMENT. So while last year rainfall received in June was just 10 mm, this year, its almost 53.4 mm, and 96% above normal average 9 . The peak and valleys in the graph above provides stance of both the erraticism and unpredictability of monsoon in Delhi. 9 Indian Meteorological Department, http://www.imd.gov.in/ -150 -100 -50 0 50 100 150 2008 2009 2010 2011 2012 2013 (till 23.6.2013) Delhi Rainfall (mm) & % departure from the long period averages of rainfall for the month of June between 2008- 2013 Arithmatic averages of Rainfall (mm) for Delhi % Departures of rainfall from the long period averages of rainfall for Delhi
Increasing Monsoon unpredictability and erraticism linked with rising Global Warming in the Indian subcontinent with a special reference to June 2013 excessive rainfall in Delhi. -Arpita Bhagat Monsoon in India is one of the most important weather phenomenon on which the entire country’s agricultural productivity and economics depends. According to Indian Meteorological Department (nodal agency for climatological observations and studies in the country), it is the seasonal reversals of the wind direction along the shores of the Indian Ocean, that blow from the southwest during one half of the year and from the northeast during the other half1. The former called the south-west monsoon is responsible for most of the rainfall received (June-September). Monsoons occur when the temperature on land is significantly warmer or cooler than the temperature of the ocean. These temperature imbalances are caused because the oceans and land absorb heat in different ways2. In addition, surface temperatures increase at a greater rate over land than ocean in simulations and observations of global warming3. Though the erraticism of India’s monsoons is fairly documented, research provides ample proof that global warming has added to the unpredictability and erraticism of the same. For instance, Menon et al. (2013), predict consistent increase in day-to-day rainfall variability in India under unmitigated climate change by using 20 comprehensive climate models that conclusively suggests the necessity of profound adaptation measures4. Also, according to predictions by Kumar et al. (2006), surface warming is monotonously widespread and extremes in both temperature and rainfall are expected to increase, especially in the west central India5. Delhi, located at 28.61°N 77.23°E, lies in Northern India, bordering states of Haryana on the north, west and south and Uttar Pradesh to the east6. Delhi features an atypical version of the humid subtropical climate, high variation between summer, winter temperatures and precipitation. Typically, the monsoon winds arrive in Delhi by either the end of June or the first week of July with Delhi receiving an average rainfall of 714 mm7. This year, the onset of monsoon was preponed, with the capital receiving its first showers on June 13th 20138. Plotting the data of Delhi average rainfall (mm) for the last five years and the percentage departure of the same, the following figure is obtained. 1 2 http://www.imd.gov.in/section/nhac/dynamic/Met_Glossary.htm http://www.engineeringtoolbox.com/specific-heat-fluids-d_151.html 3 http://www.mit.edu/~pog/src/byrne_land_ocean_warming_contrast_2013.pdf http://onlinelibrary.wiley.com/doi/10.1002/grl.50583/abstract 5 http://www.iisc.ernet.in/currsci/feb102006/334.pdf 6 The American Heritage Dictionary of the English Language (fourth ed.). Houghton Mifflin Company. 2000. 4 7 8 http://www.delhi.gov.in/DoIT/DOIT_DM/state%20profile.pdf http://m.accuweather.com/cs/weather-blogs/andrews/south-west-monsoon-onset-four-weeks-early-1/14352257 Delhi Rainfall (mm) & % departure from the long period averages of rainfall for the month of June between 20082013 150 100 50 0 2008 2009 2010 2011 2012 -50 2013 (till 23.6.2013) -100 -150 Arithmatic averages of Rainfall (mm) for Delhi % Departures of rainfall from the long period averages of rainfall for Delhi Source: HYDROMET DIVISION, INDIA METEOROLOGICAL DEPARTMENT. So while last year rainfall received in June was just 10 mm, this year, its almost 53.4 mm, and 96% above normal average9. The peak and valleys in the graph above provides stance of both the erraticism and unpredictability of monsoon in Delhi. 9 Indian Meteorological Department, http://www.imd.gov.in/ Distribution of Rainfall for India, June 2013 showing rain received in Delhi and the totally 34 % departure from average10. In Delhi, many living in low lying regions have been displaced or rendered homeless. The rising Yamuna river levels and road blockages has caused great destruction to property. A slum is submerged in floodwaters of the Yamuna River in New Delhi, India, June 20, 2013. The Indian capital has been put on flood alert after its main Yamuna River breached the danger mark following incessant rainfall since June 1611. Moving beyond Delhi, all of northern India, including states of Himachal Pradesh and Uttarakhand have received excess rainfall by as much as 375 percent causing mass scale death and destruction12 in the region due to resulting floods and landslides just in the month of June, 2013. Unfortunately, lack of preparedness on part of the officials has only added to the widespread havoc and proved the climate scientists’ right. 10 http://www.imd.gov.in/section/hydro/dynamic/seasonal-rainfall.htm http://english.sina.com/world/p/2013/0620/601259.html 12 http://en.wikipedia.org/wiki/2013_North_India_floods 11
Keep reading this paper — and 50 million others — with a free Academia account
Used by leading Academics
girolamo fiorentino
University of Salento
Renzo Taddei
Universidade Federal de São Paulo (UNIFESP)
Bas Verschuuren
Wageningen University
Reinaldo Imbrozio Barbosa
Instituto Nacional de Pesquisas da Amazônia