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 />
<strong>Lucknow</strong>, Allahabad, Patna and Kolkata. Both morning (0300 UTC) and evening (<strong>12</strong>00<br />
UTC) annual mean relative humidity trends are significantly increasing over the region.<br />
Annual mean total cloud cover is significantly increasing at Amritsar, Ambala and<br />
<strong>Lucknow</strong> and significantly decreasing at Gwalior for morning as well as evening hours.<br />
Annual total rainfall and rainy days trends are significantly increasing at Kolkata.<br />
Annual mean sunshine duration and annual mean wind speed trends are significantly<br />
decreasing over the IGP. Seasonally, winter mean maximum temperature is<br />
significantly decreasing at stations in the western part of the IGP and significantly<br />
increasing at stations in the eastern part of the IGP during post monsoon season. While<br />
winter mean minimum temperature is significantly decreasing at Amritsar and Ambala,<br />
it is significantly increasing at all other stations except at Varanasi (increasing but not<br />
significant). Winter mean DTR trends are decreasing significantly at most of the<br />
stations. Majority of stations are having significant decreasing trends in sunshine<br />
duration and wind speed in all seasons. Relative humidity and total cloud cover trends<br />
are similar to annual trends. Seasonal rainfall trends are significantly increasing at New<br />
Delhi (winter), Gwalior and Varanasi (summer), Kolkata (post monsoon) and<br />
significantly decreasing at Patna (post monsoon).<br />
RAINFALL PARTITIONING OF PATAN TALUKA<br />
(GUJARAT) FOR THE YEAR 2006 TO 2010 USING GEO-<br />
INFORMATICS BASED DATA FOR THORNTHWAITE<br />
MODEL AND SCS-CN MODEL<br />
Khushbu Bhojak 1 , B. Naveenchandra 1 , N. Srivastava 2 , Khalid<br />
Mahmood 2 and N.K. Sherasia 1<br />
1 Department of Civil Engineering, L.D. College of Engineering, Gujarat Technological University,<br />
Navrangpura, Ahmedabad 380 009, Gujarat.<br />
2Bhaskaracharya Institute for Space Applications and Geo-informatics, Near Ch-0 Circle, Indulal Yagnik<br />
Marg, Gandhianagar 382 007, Gujarat.<br />
email: kbhojak87@gmail.com, info@bisag.gujara.gov.in<br />
Present work describes a simple method for rainfall partitioning into runoff,<br />
evapo-transpiration and infiltration. For this purpose, Thornthwaite water balance and<br />
SCS-CN models have been used. Graphical User Interface (GUI) for Thornthwaite<br />
model is developed by U. S. Geological Survey. SCS –CN model developed by United<br />
States Department of Agriculture is widely used for quick runoff estimation. In Patan<br />
Taluka of Patan district, Gujarat there is a perennial problem of water scarcity. Hence, it<br />
is difficult to sustain agrarian and dairy economy. In order to understand basic<br />
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