12-14 September, 2011, Lucknow - Earth Science India
12-14 September, 2011, Lucknow - Earth Science India
12-14 September, 2011, Lucknow - Earth Science India
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National Conference on <strong>Science</strong> of Climate Change and <strong>Earth</strong>’s Sustainability: Issues and Challenges ‘A Scientist-People Partnership’<br />
<strong>12</strong>-<strong>14</strong> <strong>September</strong>, <strong>2011</strong>, <strong>Lucknow</strong><br />
troposphere over Afro-Asian highlands, the monsoon is stronger, La Niña condition in<br />
the Pacific and intense rainfall across <strong>India</strong>, while reverse was the changes during<br />
cooler troposphere. In recent years, the Asian-<strong>India</strong>n monsoon circulation is weaker and<br />
rainfall across <strong>India</strong> because of cooler upper troposphere over Tibet-Himalaya-China-<br />
Mongolia-Manchuria sector and warmer lower troposphere over the surrounding water<br />
bodies (Pacific, <strong>India</strong>n, Atlantic and Southern Oceans). In general, the troposphere over<br />
the southern hemisphere is warming at a faster rate due to large water bodies compared<br />
to that over northern hemisphere, so there is lesser exchange of the mass-moisture<br />
between the two hemispheres. During boreal summer, decreasing trend is seen in the<br />
intensity of the general atmospheric circulation over the period 1949-2009.<br />
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