Sea surface effects on the sea surface temperature estimation by remote sensing—Part 2

Yokoyama, Ryuzo; Tanba, S.; Souma, T.

doi:10.1080/01431169608948704

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Cited by 10 publications

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“…The upper few meters of the ocean warm and then cool over the course of a diurnal cycle. Under very light wind speed conditions (less than 2 m/s) the upper few meters of the ocean can warm several degrees (Stramma et al, 1986;Yokoyama and Konda, 1996). For these conditions, turbulence is thought to be suppressed by the positive buoyancy flux due to penetrative solar radiation (Webster et al, 1996;Soloviev and Lukas, 1997).…”

Section: Introductionmentioning

confidence: 99%