1962
DOI: 10.1175/1520-0450(1962)001<0552:rbsria>2.0.co;2
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Relation between Solar Radiation Income and Cloud Type in the Arctic

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Cited by 41 publications
(17 citation statements)
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“…Whilst satellite retrieval of radiance data over high-latitude regions has been continuing for over two decades, the interpretation of these data is difficult and often ambiguous. The existing cloud climatological data for the Arctic agree upon the fundamental characteristic, namely, in winter the sky is relatively cloud-free but in summer it is generally fairly cloudy (Vowinckel, 1962). Certain features of the Arctic cloud climatology, such as the multiple layering of summertime stratiform clouds, have been analysed in detail by Herman (1977Herman ( , 1980 and Jayaweera (1977Jayaweera ( , 1982.…”
Section: Introductionmentioning
confidence: 95%
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“…Whilst satellite retrieval of radiance data over high-latitude regions has been continuing for over two decades, the interpretation of these data is difficult and often ambiguous. The existing cloud climatological data for the Arctic agree upon the fundamental characteristic, namely, in winter the sky is relatively cloud-free but in summer it is generally fairly cloudy (Vowinckel, 1962). Certain features of the Arctic cloud climatology, such as the multiple layering of summertime stratiform clouds, have been analysed in detail by Herman (1977Herman ( , 1980 and Jayaweera (1977Jayaweera ( , 1982.…”
Section: Introductionmentioning
confidence: 95%
“…Arctic cloud climatologies have been presented by Vowinckel (1962) and Huschke (1969), by Henderson (1967) for the Beaufort Sea and by Voskresenskiy and Chukanin (1959) for low clouds in the eastern Arctic. Most of these analyses drew heavily upon surface station observations although the usefulness of routine weather reconnaissance flights was illustrated in the analyses of Henderson (1967) and Huschke (1969).…”
Section: Introductionmentioning
confidence: 99%
“…This numerator is essentially the basis of the Angstrom-Savinov parameterization of observed insolation in terms of fractional cloudcover (Sivkov, 1971). The denominator of this equation represents the enhancement of intensity due to multiple reflection between cloudbase and the snowcover (see Liljequist, 1956, Vowinckel andOrvig, 1962).…”
Section: Parameterization Fc)uationsmentioning
confidence: 99%
“…It was found that such accurate insolation models could typically be categorized into three groups: exponential models [5][6][7][8][9][10], atmospheric transmission models [11][12][13] and time series models [14][15][16]. It was assessed that transmission models and time series models were generally not applicable to rural Australia due to their reliance on unavailable climate data such as cloud density in the case of transmission models, or daily insolation data for a large period of time in the case of time series models.…”
Section: H�o Hmentioning
confidence: 99%