About The Product
Published by means of the yank Geophysical Union as a part of the Antarctic learn Series.
In a 1971 clinical Committee on Antarctic study record that reviewed polar contrasts in sea ice, Lyn Lewis and Willy Weeks made the next remark: "People who learn sea ice within the Arctic Basin are frequently asked in the event that they have ever studied ice in Antarctica, they usually solution 'why trouble, it is the standard stuff." Noting this used to be "fortunately actual to a substantial extent," they extra "It is obvious that destiny paintings will count seriously at the logistics amenities to be had to permit floor observations past the quick ice side in any respect seasons of the 12 months. of virtually equivalent significance may be the improvement of tools and recording gear fitted to use within the polar setting" (Lewis, E. L., and W. F. Weeks, Sea Ice: a few Polar Contrasts, in, Antarctic Ice and Water Masses, edited by way of G. Deacon, medical Committee on Antarctic learn, Cambridge, 23-34, 1971).
Lewis and Weeks made no particular point out of Earth-orbiting satellites, on which the 1st passive microwave sensor grew to become operational in December 1972. below a 12 months later the enormous Weddell Polynya was once saw for the 1st time. possibly greater than the other improvement, this unforeseen characteristic illustrated the capability to enormously extend our wisdom of sea ice throughout the program of spaceborne distant sensing. at the same time, it acted as a catalyst for an important bring up within the point of study.
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Additional resources for Antarctic Sea Ice: Physical Processes, Interactions and Variability
P. Gloersen, A. Chang, and A. Rango, 1986. J. J. C. L. J. Zwally, Arctic and River Basin, J. Geophys. , IOI, 6679-6688, 1996. , S. Patil, and H. , 1992. microwaveradiometer (SMMR) data, IEEE Trans. , Surface-basedpassivemicrowave observaGeosc. Rein. , GE-œO,452-467, 1982. , and H. Eicken, The sea ice thicknessdisTrans. Geosc. Rein. , GE-œd,378-382, 1986. tribution in the northwestern Weddell Sea, J. W. Lohanick, Temporal variaphys. , 96, 4821-4837, 1991. , Snow on seaice: Competing effectsin shaplate spring and early summer near Mould Bay NWT, ing climate, J.
Geophys. , 95, 5359-5369, 1990. , J. R. T. D. R. C. Wackerman, Aircraft active and passive microwave validation of sea ice concentrationfrom the defensemeteorologicalsatellite program special sensormicrowave imager, J. Geophys. , 96, 21,989-22,008, 1991. J. and 16 others, NASA sea ice validation program for the DMSP SSM/I: Final report, NASA Tech. Memo. , 1992. , P. Gloersen, T. Schmugge,T. J. Zwally, Microwave emission from snow and ital snow depth data from Martin Jeffries, Hajo Eicken, glacier ice, J.
4. -) 4O •o 3o :: . o • 20'': December Plate 3. Mean monthly snow depths for the months July through December from the years 1988-1994. The open ocean area is white. Black pixels indicate areas where more than 3 years of monthly averageshave flagged values resulting from melting effectsidentified using temporal information as described in section • MARKUS AND CAVALIERI: SNOW 60 DEPTH - I• I• DISTRIBUTION OVER SEA ICE 33 Sea embaymentsoccur during summer. During the summer months, there is greater variability in the number of values averagedfor each pixel becauseof rapidly changingice concentrationsgiving the maps a speckle appearance.
Antarctic Sea Ice: Physical Processes, Interactions and Variability