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- W2052977083 abstract "Abstract Winter-month data obtained at United States Antarctic stations during the ICY are used to compute coefficients for regression equations relating the 100-mb. temperatures and heights to the 50-mb. heights. It is found upon trial that the layer thickness can be estimated as accurately from the 100-mb. temperature alone as from both the temperature and 100-mb. height; therefore, the simpler equations in only one variable are used. The average errors in computed heights are less than 2 dekameters and the extreme errors 6 dkm. or less when tests are performed on independent data. A measure of the average lapse rates within the layer between 100 mb. and 50 mb., derived from the same data as the equations mentioned above, proves to be as good a predictor as any of the regression equations. These mean lapse rates show a regular variation with both latitude and month. The largest values (greatest instability) occur in the coldest months and the highest latitudes, and the greatest layer stability in lower ..." @default.
- W2052977083 created "2016-06-24" @default.
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- W2052977083 date "1960-07-01" @default.
- W2052977083 modified "2023-09-30" @default.
- W2052977083 title "EXTRAPOLATION TO THE 50-MB. LEVEL FROM 100-MB. DATA IN ANTARCTICA*" @default.
- W2052977083 doi "https://doi.org/10.1175/1520-0493(1960)088<0251:ettmlf>2.0.co;2" @default.
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