Albedo Variations and Surface Energy Balance in Different Snow-Ice Media in Antarctica

• Published in: Defence Science Journal
• Main Author: Mishra, V.D.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Defence Scientific Information & Documentation Centre (DESIDOC), DRDO 2013
• Subjects: Antarc*; Antarctica; Astrid Coast
• Online Access: https://publications.drdo.gov.in/ojs/index.php/dsj/article/view/3849; https://doi.org/10.14429/dsj.49.3849

The present study is aimed at investigating the radiation budget in different snow-ice media (shelf ice,continental ice and natural snow) at three different elevated sites in the general area of Prince Astrid Coast of EastAntarctica. Measurements of the dependence of albedo in different snow and ice media on solar elevation angle,cloud cover, liquid water content, grain size, etc. can be interpreted in terms of single and multiple scatteringradiative transfer theory. Detailed albedo measurements were carried out during summer and winter in differentsnow and ice media in 1997-98 at different selected sites at Antarctica. The average albedo values were found to behigh (90 per cent) in snow medium, moderate (83 per cent) in shelf ice and very low (50 per cent) in continentalice medium. The albedo was found to be a function of cloud amount, increasing with the amount and thickness. Inwhite-out condition during blizzards, high albedo (average 83 per cent) was found as compared to clear sky day(76 per cent) and after blizzard (average 78 per cent). It showed dependence on the type and age of snow also. Newsnowfall over old snow displayed higher values (90 per cent) than older snow (70 per cent) and decreased with theageof snow from 13- 16 per cent. Naturalmelt-water in snowpack increases from 1- 10 per cent, resulting in albedodecay from 7-10 per cent. As the minimum solar elevation angle in Antarctica goes to 3O, strong qualitativeanalyses have been ma e of the dependenceof albedo on the solar elevation angle. Albedo values showed diurnalhysteresis and m in values were found to be higher than evening values at the same angle of elevation. Thedependence was 4 sligh or solar elevations during day time when 0 % 12-IS0, but became larger with low angleswhen 8 = 3-12'. Solar insolations were also calculated for different months in order to calculate short waveradiation absorbed by snow and ice media. Insolations in different months at different selected sites lie in theranges 10-540 lnlday (August-October), 350-911 lnlday ...