Lekshmi Mudra B
Changing global climatic scenario on environmental processes across India: its possible causes and impacts - Vellanikkara Academy of Climate Change Education and Research 2016 - 131 pages
MSc
Global warming is real. Polar ice is melting. Sea level is rising. One-third
of plant and animal species is likely to be extinct in the decades to come. Rise in
atmospheric temperature and sea surface temperature is likely to influence the
atmospheric and environmental processes. Keeping this in view, present study
was aimed with the objectives viz., to examine the rainfall variability across the
country and its possible causes; to access the land use and land cover change of
different parts of the country; to address the impacts of changing climatic
scenario to the environmental processes. Rainfall data, atmospheric variables
over land and ocean, land use and land cover data were collected from the India
Meteorological Department and Indian Institute of Tropical Meteorology. The
NCEP/NCAR reanalysis data were also used. The study was conducted in IITM
using the available resources like GIS. Rainfall and meteorological parameters
were analyzed during pre-climate and post-climate shift.
The mean all India annual rainfall showed a decline (32.7 mm) from pre-
climate shift period (1949-78) to post-climate shift period (1979-2014) when the
year 1978 was considered as the climate shift year. A significant decline in
monsoon rainfall led to the decline in annual rainfall since 75.2 per cent of it is
contributed during the monsoon season. Most of the geographical area of the
country was under dry and very dry zone during all the three seasons except
monsoon season. The zonal trends in all India rainfall indicated that the three
zones viz., the East Coast (N), the East Coast (S) and the North East India (NEI)
showed increase in rainfall while rainfall decline was noticed in all other zones
across the country viz., Central Peninsular India, Ganga Plains, North Central
India, North Mountainous India, North West India, South Peninsular India, West
Coast (S), and West Coast. Decline in rainfall over India could be explained as
due to changes that took place in land, ocean, and atmosphere continuum such as
the tropospheric and surface temperatures, mean sea level pressure, sea surface
temperature, geopotential height, precipitable water, and cloud amount.Weakening of the summer monsoon rainfall is the result of variability in different
meteorological parameters.
In recent years, the maximum increase in net cultivated area was observed
in the state of Manipur by 47.88 per cent from 2000 to 2013. All other
northeastern states showed a rise in area under net cultivation. Odisha showed a
maximum decline in net cultivation by 35.66 per cent over the period. Maximum
increase in built up area was observed in Arunachal Pradesh, which is five times
or more in 2013 than 2000. Maximum increase in forest cover observed in West
Bengal (57.16 %) while maximum decrease observed in Bihar (27.47 %)
followed by Punjab (27.14 %). Maximum increase in intermittent wood was
observed in Punjab by two times or more over the period from 2000 to 2013,
followed by Rajasthan (66.12 %). Maximum decline in intermittent wood
observed in Kerala (81.34 %) over the period. Maximum increase in grass land
reported in Arunachal Pradesh by three times or more while maximum decline
reported in Mizoram by 77.14 per cent. Maximum increase in barren land
observed in Arunachal Pradesh (81.93 %) followed by Punjab (81.03 %).
Maximum decrease in barren land was observed in West Bengal (53.61 %).
The mean surface air temperature over the globe was 14.67 o C over the
period from 1949 to 2014. It was increased by 0.3 o C during post climate shift
period (1979 to 2014). Analysis of all India annual mean temperature showed an
increase of 0.22 o C, with a mean of 24.4 o C over the period from 1949-2007.
Over India, the Central Peninsular India, South Peninsular India, West Coast (S),
and West Coast were experienced decline in annual rainfall because in those
zones monsoon rainfall also showed a decreasing trend. The Indian states spread
over these zones, viz. Madhya Pradesh, Maharashtra, Karnataka, Andhra Pradesh,
and Tamil Nadu showed an increase in area under barren land. The same process
did not match with the arrest in desertification over Rajasthan. It could be
explained due to large scale afforestation that took place in Rajasthan in addition
to irrigation facilities provided through the prestigious Indira Gandhi Canal
project.Global warming and climate change are now considered one of the most
serious threats to the society linked sectors as it had an adverse impact on natural
resources and vice versa. In these sectors it is therefore very important to adapt to
climate change for sustainable development. Addressing the impact of climate
change requires a good scientific understanding as well as coordinated action at
national, regional, and global level.
Climate Change Adaptation
551.6 / LEK/CH
Changing global climatic scenario on environmental processes across India: its possible causes and impacts - Vellanikkara Academy of Climate Change Education and Research 2016 - 131 pages
MSc
Global warming is real. Polar ice is melting. Sea level is rising. One-third
of plant and animal species is likely to be extinct in the decades to come. Rise in
atmospheric temperature and sea surface temperature is likely to influence the
atmospheric and environmental processes. Keeping this in view, present study
was aimed with the objectives viz., to examine the rainfall variability across the
country and its possible causes; to access the land use and land cover change of
different parts of the country; to address the impacts of changing climatic
scenario to the environmental processes. Rainfall data, atmospheric variables
over land and ocean, land use and land cover data were collected from the India
Meteorological Department and Indian Institute of Tropical Meteorology. The
NCEP/NCAR reanalysis data were also used. The study was conducted in IITM
using the available resources like GIS. Rainfall and meteorological parameters
were analyzed during pre-climate and post-climate shift.
The mean all India annual rainfall showed a decline (32.7 mm) from pre-
climate shift period (1949-78) to post-climate shift period (1979-2014) when the
year 1978 was considered as the climate shift year. A significant decline in
monsoon rainfall led to the decline in annual rainfall since 75.2 per cent of it is
contributed during the monsoon season. Most of the geographical area of the
country was under dry and very dry zone during all the three seasons except
monsoon season. The zonal trends in all India rainfall indicated that the three
zones viz., the East Coast (N), the East Coast (S) and the North East India (NEI)
showed increase in rainfall while rainfall decline was noticed in all other zones
across the country viz., Central Peninsular India, Ganga Plains, North Central
India, North Mountainous India, North West India, South Peninsular India, West
Coast (S), and West Coast. Decline in rainfall over India could be explained as
due to changes that took place in land, ocean, and atmosphere continuum such as
the tropospheric and surface temperatures, mean sea level pressure, sea surface
temperature, geopotential height, precipitable water, and cloud amount.Weakening of the summer monsoon rainfall is the result of variability in different
meteorological parameters.
In recent years, the maximum increase in net cultivated area was observed
in the state of Manipur by 47.88 per cent from 2000 to 2013. All other
northeastern states showed a rise in area under net cultivation. Odisha showed a
maximum decline in net cultivation by 35.66 per cent over the period. Maximum
increase in built up area was observed in Arunachal Pradesh, which is five times
or more in 2013 than 2000. Maximum increase in forest cover observed in West
Bengal (57.16 %) while maximum decrease observed in Bihar (27.47 %)
followed by Punjab (27.14 %). Maximum increase in intermittent wood was
observed in Punjab by two times or more over the period from 2000 to 2013,
followed by Rajasthan (66.12 %). Maximum decline in intermittent wood
observed in Kerala (81.34 %) over the period. Maximum increase in grass land
reported in Arunachal Pradesh by three times or more while maximum decline
reported in Mizoram by 77.14 per cent. Maximum increase in barren land
observed in Arunachal Pradesh (81.93 %) followed by Punjab (81.03 %).
Maximum decrease in barren land was observed in West Bengal (53.61 %).
The mean surface air temperature over the globe was 14.67 o C over the
period from 1949 to 2014. It was increased by 0.3 o C during post climate shift
period (1979 to 2014). Analysis of all India annual mean temperature showed an
increase of 0.22 o C, with a mean of 24.4 o C over the period from 1949-2007.
Over India, the Central Peninsular India, South Peninsular India, West Coast (S),
and West Coast were experienced decline in annual rainfall because in those
zones monsoon rainfall also showed a decreasing trend. The Indian states spread
over these zones, viz. Madhya Pradesh, Maharashtra, Karnataka, Andhra Pradesh,
and Tamil Nadu showed an increase in area under barren land. The same process
did not match with the arrest in desertification over Rajasthan. It could be
explained due to large scale afforestation that took place in Rajasthan in addition
to irrigation facilities provided through the prestigious Indira Gandhi Canal
project.Global warming and climate change are now considered one of the most
serious threats to the society linked sectors as it had an adverse impact on natural
resources and vice versa. In these sectors it is therefore very important to adapt to
climate change for sustainable development. Addressing the impact of climate
change requires a good scientific understanding as well as coordinated action at
national, regional, and global level.
Climate Change Adaptation
551.6 / LEK/CH