1970
DOI: 10.1175/1520-0450(1970)009<0215:trbotp>2.0.co;2
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The Radiation Balance of the Planet Earth from Radiation Measurements of the Satellite Nimbus II

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Cited by 54 publications
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“…Raschke and Bandeen (1970) present the first indications of OLR diurnal cycle characteristics using noonminus-midnight differences, identifying large OLR diurnal cycles over land in desert and convective regions. Short and Wallace (1980) also used day-night differences to investigate diurnal variations in cloudiness, demonstrating early morning peaks in both high and low clouds over convective and marine stratocumulus (MSc) regions, respectively.…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…Raschke and Bandeen (1970) present the first indications of OLR diurnal cycle characteristics using noonminus-midnight differences, identifying large OLR diurnal cycles over land in desert and convective regions. Short and Wallace (1980) also used day-night differences to investigate diurnal variations in cloudiness, demonstrating early morning peaks in both high and low clouds over convective and marine stratocumulus (MSc) regions, respectively.…”
Section: Introductionmentioning
confidence: 99%
“…Initial interest in the outgoing longwave radiation (OLR) diurnal cycle stemmed from attempts to determine the Earth energy budget from sun-synchronous satellite measurements (Raschke and Bandeen 1970). Raschke and Bandeen (1970) present the first indications of OLR diurnal cycle characteristics using noonminus-midnight differences, identifying large OLR diurnal cycles over land in desert and convective regions.…”
Section: Introductionmentioning
confidence: 99%
“…The diurnal cycle contributes significantly to variability in many geophysical variables including clouds, temperature, radiation, and precipitation (e.g., Gray and Jacobson 1977;Minnis and Harrison 1984;Hartmann and Recker 1986;Harrison et al 1988;Yang and Slingo 2001;Taylor 2012) and influences many geophysical processes (e.g., cloud formation, surface turbulence, and surface evaporation rates; Caldwell et al 2005;Strong et al 2005). Understanding and characterizing diurnal cycle features is critical for both Earth system modeling (Bechtold et al 2004;Del Genio and Wu 2010) and placing satellite observations of Earth into proper context (Raschke and Bandeen 1970;Short and Wallace 1980;Loeb et al 2009;Taylor and Loeb 2013).…”
Section: Introductionmentioning
confidence: 99%
“…For instance, the diurnal cycle is stronger over land than ocean (e.g., Raschke and Bandeen 1970;Harrison et al 1988). The strongest surface temperature diurnal cycles on Earth are found in subtropical deserts (e.g., Atacama Desert) and drive significant diurnal cycle Denotes Open Access content.…”
Section: Introductionmentioning
confidence: 99%
“…So far, satellite observations of the global radiation budget have been carried out by Raschke andBandeen (1970), Vonder Haar andSuomi (1971), and more recently by Smith et al (1977), Taylor and Stowe (1984), Jacobowitz et al (1984), and so on. At present, however, a method to derive I* from satellite data is not yet available.…”
Section: Introductionmentioning
confidence: 99%