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Record #123652:

The calculation of surface temperature and albedo of Arctic sea ice from AVHRR / Ronald W. Lindsay, D.A. Rothrock.

Title: The calculation of surface temperature and albedo of Arctic sea ice from AVHRR / Ronald W. Lindsay, D.A. Rothrock.
Author(s): Lindsay, Ronald W.
Rothrock, D. A.
Date: 1993.
In: Annals of Glaciology. (1993.), Vol. 17 (1993)
Abstract: Temperature estimate uses split window correction incorporating regression coefficients appropriate for Arctic atmosphere. Albedo estimate is found assuming clear and dry atmosphere. Both estimates are made with published correction techniques. Inherent errors due to uncertainty of atmospheric interference are judged to be 2 to 5°C in surface temperature and 0.10 to 0.20 in surface albedo. Cloudy regions are masked manually using data from all five channels. Relationship between temperature and albedo is shown for sample scene. Model calculations based on surface energy balance permit albedo and temperature to be related to ice thickness and snow-cover thickness and to assess further accuracy of surface estimates.
Notes:

Annals of Glaciology. Vol. 17 :391-397 (1993).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
536.5 -- Temperature measurement and control.
536 -- Heat.
551.521.32 -- Albedo. Radiation, terrestrial and atmospheric.
53.087.23 -- Remote sensing.
629.783 -- Satellites.
E3 -- Glaciology: instruments and methods.
(*60) -- Arctic Ocean and adjacent waters.
SPRI record no.: 123652

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245 14 ‡aThe calculation of surface temperature and albedo of Arctic sea ice from AVHRR /‡cRonald W. Lindsay, D.A. Rothrock.
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500 ## ‡aAnnals of Glaciology. Vol. 17 :391-397 (1993).
520 3# ‡aTemperature estimate uses split window correction incorporating regression coefficients appropriate for Arctic atmosphere. Albedo estimate is found assuming clear and dry atmosphere. Both estimates are made with published correction techniques. Inherent errors due to uncertainty of atmospheric interference are judged to be 2 to 5°C in surface temperature and 0.10 to 0.20 in surface albedo. Cloudy regions are masked manually using data from all five channels. Relationship between temperature and albedo is shown for sample scene. Model calculations based on surface energy balance permit albedo and temperature to be related to ice thickness and snow-cover thickness and to assess further accuracy of surface estimates.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a536.5 -- Temperature measurement and control.‡2udc
650 07 ‡a536 -- Heat.‡2udc
650 07 ‡a551.521.32 -- Albedo. Radiation, terrestrial and atmospheric.‡2udc
650 07 ‡a53.087.23 -- Remote sensing.‡2udc
650 07 ‡a629.783 -- Satellites.‡2udc
650 07 ‡aE3 -- Glaciology: instruments and methods.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
700 1# ‡aRothrock, D. A.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 17 (1993) ‡wSPRI-60773
917 ## ‡aUnenhanced record from Muscat, imported 2019
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