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Record #123637:

Seasonal variations in brightness temperature for central Antarctica / Cornelis J. Van der Veen, Kenneth C. Jezek.

Title: Seasonal variations in brightness temperature for central Antarctica / Cornelis J. Van der Veen, Kenneth C. Jezek.
Author(s): Van der Veen, Cornelis J.
Jezek, Kenneth C.
Date: 1993.
In: Annals of Glaciology. (1993.), Vol. 17 (1993)
Abstract: Radiative-transfer model developed by Zwally (1977) is modified and coupled to one-dimensional time-dependent temperature model in order to calculate seasonal variation in brightness temperature. By comparing this with observed records, radiative properties of firn can be determined. By retaining scattering as source term in radiative transfer function, agreement between model-derived scattering and absorption coefficients and those calculated from Mie/Rayleigh scattering theory can be obtained. Horizontal brightness temperature is not linked to vertical one through common power reflection coefficient.
Notes:

Annals of Glaciology. Vol. 17 :300-306 (1993).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.24 -- Ice sheets and caps.
551.324.412 -- Land ice, temperature.
551.324.414 -- Land ice, radiation to and from.
519.673 -- Modelling.
551.578.46 -- Snow cover and snow patches.
551.521 -- Radiation, atmospheric.
536.5 -- Temperature measurement and control.
E5 -- Glaciology: land ice.
(*7) -- Antarctic regions.
SPRI record no.: 123637

MARCXML

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100 1# ‡aVan der Veen, Cornelis J.
245 10 ‡aSeasonal variations in brightness temperature for central Antarctica /‡cCornelis J. Van der Veen, Kenneth C. Jezek.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 300-306 :‡bdiags., table.
500 ## ‡aAnnals of Glaciology. Vol. 17 :300-306 (1993).
520 3# ‡aRadiative-transfer model developed by Zwally (1977) is modified and coupled to one-dimensional time-dependent temperature model in order to calculate seasonal variation in brightness temperature. By comparing this with observed records, radiative properties of firn can be determined. By retaining scattering as source term in radiative transfer function, agreement between model-derived scattering and absorption coefficients and those calculated from Mie/Rayleigh scattering theory can be obtained. Horizontal brightness temperature is not linked to vertical one through common power reflection coefficient.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc
650 07 ‡a551.324.412 -- Land ice, temperature.‡2udc
650 07 ‡a551.324.414 -- Land ice, radiation to and from.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a551.521 -- Radiation, atmospheric.‡2udc
650 07 ‡a536.5 -- Temperature measurement and control.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
700 1# ‡aJezek, Kenneth C.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 17 (1993) ‡wSPRI-60773
917 ## ‡aUnenhanced record from Muscat, imported 2019
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