scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...
scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...
scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...
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STP12 Abstracts<br />
Berlin, 12 - 16 July <strong>2010</strong><br />
SCOSTEP Symposium <strong>2010</strong><br />
On characteristic features of global, polar <strong>an</strong>d equitorial temperature <strong>an</strong>d its possible<br />
linkage with solar activities.<br />
B<strong>an</strong>erjee Dhruba 1 , Bondyopadhaya Ramaprosad 2<br />
1 Faculty Member,Department of Physics,Swami Vivek<strong>an</strong><strong>an</strong>da <strong>Institut</strong>e of Science <strong>an</strong>d<br />
Technology,Kolkata- 145,India, 2 Professor,Mathematics Department,Jadavpur University,Kolkata-<br />
32,India<br />
The temperature of L<strong>an</strong>d <strong>an</strong>d Oce<strong>an</strong>, <strong>an</strong>d Global L<strong>an</strong>d -Oce<strong>an</strong> Temperature (GLOT) for the period<br />
1880-2006 have been consi<strong>der</strong>ed. Further, the L<strong>an</strong>d <strong>an</strong>d Oce<strong>an</strong> temperature during last century (1903-<br />
2006) for Polar region <strong>an</strong>d Equatorial region have been <strong>an</strong>alyzed <strong>an</strong>d compared.<br />
The <strong>an</strong>alysis reveals (i) the temperature <strong>an</strong>omaly curve of GLOT has always positive gradient<br />
but the gradient during 1947 to 2006 is almost 1.7 times that of during the 1880-1946.<br />
(ii)Although the overall trend is increasing from 1880 onwards there exists <strong>an</strong> oscillatory trend in both<br />
L<strong>an</strong>d <strong>an</strong>d Oce<strong>an</strong> temperature <strong>an</strong>omalies separately <strong>an</strong>d also in GLOT, but signific<strong>an</strong>tly in the last 26/<br />
27 years (i.e.1979/80 to 2006) the rate of increase of temperature for all three cases (L<strong>an</strong>d, Oce<strong>an</strong> <strong>an</strong>d<br />
GLOT), however, becomes much higher th<strong>an</strong> that of previous 100 years. Consistently with this trend,<br />
the correlation coefficient (c.c.) between temperature <strong>an</strong>omalies <strong>an</strong>d time during this period comes out<br />
to be quite high (+0.79 for both L<strong>an</strong>d <strong>an</strong>d Oce<strong>an</strong>, <strong>an</strong>d +0.86 for GLOT).Clearly, these are all<br />
signatures of the so called Global Warming.<br />
However, the comparison of the trend lines for temperature variation of Antarctic, Arctic <strong>an</strong>d<br />
Equatorial regions during last 100 years(1903-2006) indicate that the rate of increase of temperature is<br />
positive everywhere but signific<strong>an</strong>tly it is maximum in Antarctic ,which is almost double that of<br />
Arctic, <strong>an</strong>d almost four times that of Equatorial region. Further, in general, the nature of variation of<br />
Arctic <strong>an</strong>d Antarctic temperature are opposite in character. e.g. Arctic temp. curve exhibits long period<br />
oscillation from 1913 to1963 <strong>an</strong>d then continues to increase while Antarctic curve exhibits rapid<br />
fluctuation up to 1963/64 <strong>an</strong>d then increase rapidly. This also implies Global Warming exist but not<br />
uniform everywhere.<br />
When the trend of Global L<strong>an</strong>d-Oce<strong>an</strong> Temperature (GLOT) is compared with that for Sun’s<br />
Spot Number (SSN) for the period 1880-2006.It is found that the same monotonically increasing trend<br />
exists in the variation of SSN as well as in GLOT.Finally, the comparison of correlation coefficients<br />
between SSN <strong>an</strong>d Temperature in different regions (Arctic, Antarctic <strong>an</strong>d Equatorial) for different<br />
SSN r<strong>an</strong>ges revel that SSN is most capable to influence in Eqatorial region. But always exist some<br />
critical value of SSN (≈120) exceeding which solar influence becomes more effective.