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Record #117200:
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MARC recordDistribution 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 |
LDR 01633naa#a2200000#a#4500 001 SPRI-117200 005 20231005005513.0 007 ta 008 231005s1992####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-117200 040 ## ‡aUkCU-P‡beng‡eaacr 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 948 3# ‡a20231005