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Record #117200:

Distribution of mean δ¹⁸O values of surface snow layers and their dependence on air temperature in Enderby Land--east Queen Maud Land, Antarctica / Kazuhide Satow, Okitsugu Watanabe.

Title: Distribution of mean δ¹⁸O values of surface snow layers and their dependence on air temperature in Enderby Land--east Queen Maud Land, Antarctica / Kazuhide Satow, Okitsugu Watanabe.
Author(s): Satow, Kazuhide.
Watanabe, Okitsugu.
Date: 1992.
In: National Institute of Polar Research. Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology. (1992.), Vol. 5 (1992)
Abstract: δ¹⁸O values decrease linearly with elevation, distance from coast, and, especially, mean annual surface temperatures in temperature range from -20 to -55°C. Relationship with temperature is similar to that derived from simple model in which air mass is progressively cooled under Rayleigh conditions as it moves inland. This suggests that δ¹⁸O values are closely related to condensation temperature at top of inversion layer where snowfall precipitation is formed.
Notes:

National Institute of Polar Research. Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology. Vol. 5 :120-127 (1992).

Keywords: 551.578.46 -- Snow cover and snow patches.
54 -- Chemistry.
54.027 -- Isotope analysis.
E10 -- Glaciology: snow and avalanches.
(*7) -- Antarctic regions.
(*73) -- Dronning Maud Land.
(*741) -- Enderby Land.
SPRI record no.: 117200

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100 1# ‡aSatow, Kazuhide.
245 10 ‡aDistribution of mean δ¹⁸O values of surface snow layers and their dependence on air temperature in Enderby Land--east Queen Maud Land, Antarctica /‡cKazuhide Satow, Okitsugu Watanabe.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1992.
300 ## ‡ap. 120-127 :‡bdiags., map.
500 ## ‡aNational Institute of Polar Research. Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology. Vol. 5 :120-127 (1992).
520 3# ‡aδ¹⁸O values decrease linearly with elevation, distance from coast, and, especially, mean annual surface temperatures in temperature range from -20 to -55°C. Relationship with temperature is similar to that derived from simple model in which air mass is progressively cooled under Rayleigh conditions as it moves inland. This suggests that δ¹⁸O values are closely related to condensation temperature at top of inversion layer where snowfall precipitation is formed.
650 07 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a54 -- Chemistry.‡2udc
650 07 ‡a54.027 -- Isotope analysis.‡2udc
650 07 ‡aE10 -- Glaciology: snow and avalanches.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*73) -- Dronning Maud Land.‡2udc
651 #7 ‡a(*741) -- Enderby Land.‡2udc
700 1# ‡aWatanabe, Okitsugu.
773 0# ‡7nnas ‡tNational Institute of Polar Research. Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology. ‡gVol. 5 (1992) ‡wSPRI-89893
917 ## ‡aUnenhanced record from Muscat, imported 2019
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