On the Variation of Heat Exchange and Evaporation at the Sea Surface in the Western North Pacific Ocean

Hishida, Kozo; Nishiyama, Katsunobu

doi:10.5928/kaiyou1942.25.1

Cited by 8 publications

(4 citation statements)

References 7 publications

(6 reference statements)

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“…When only the first part of Berliand's formula is used, the estimates are about 0.015 cal cm -• min -2 greater than the observations, but the agreement is even less adequate if the complete formula is used. The complete formula has been used in a number of recent studies [Hishida and Nishiyama, 1969;Roden, 1974], normally with the nonlinear cloud factor discussed previously. In areas with frequent stratiform clouds the use of Berliand's formula with the nonlinear cloud factor gives estimates appreciably greater than the data reported here indicate.…”

Section: Mean Daily Values Of Net Long-wave Radiation Were Determinedmentioning

confidence: 99%

Insolation and net long-wave radiation off the Oregon coast

Reed¹,

Halpern²

1975

J. Geophys. Res.

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Insolation, net radiation, and various oceanic and atmospheric variables were measured at sites 13 and about 120 km off the coast of Oregon in July and August 1973. A total often 24‐hour stations were occupied. The daily mean net solar radiation ranged from 0.10 to 0.40 cal cm−2 min−1, and large spatial variations of radiation in this upwelling region were present. The daily mean values were not closely related to the proportion of sky covered with clouds, but a mean from all the stations was in reasonable agreement with one cloud formula. The net long‐wave radiation varied from about −0.01 cal cm−2 min−1 under overcast skies to −0.10 cal cm−2 min−1 under clear skies. Daily mean values appear closely related to cloud amount, and a cloud factor of 1 ‐ 0.9C, as suggested by previous workers, seems appropriate for stratocumulus clouds. The measured clear‐sky net long‐wave radiation is appreciably less than that given by numerous widely used formulas but is supported by other observations and by a formula derived by Anderson.

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Section: Mean Daily Values Of Net Long-wave Radiation Were Determinedmentioning

confidence: 99%

Insolation and net long-wave radiation off the Oregon coast

Reed¹,

Halpern²

1975

J. Geophys. Res.

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“…[13][14][15]) and geophysics (e.g. [16][17][18][19]) can be solved by means of cumbersome numerical schemes or empirical approaches (see methods in Refs. [13][14][15][16][17][18][19]).…”

Section: Introductionmentioning

confidence: 99%

“…[16][17][18][19]) can be solved by means of cumbersome numerical schemes or empirical approaches (see methods in Refs. [13][14][15][16][17][18][19]). The present paper is devoted to the problem of evaporation of a volatile component in solid-gas systems separated by a thin layer of liquid.…”

Section: Introductionmentioning

confidence: 99%

The Stefan problem for unsteady-state evaporation of a volatile component in the solid–liquid–gas systems: Exact analytical solution

Alexandrov

Malygin

2010

International Journal of Heat and Mass Transfer

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“…1). Such systems are found in other technologies of material production (see, among others, [8][9][10][11]), geophysics [12][13][14] and medical physics [15]. A reversible chemical reaction and a processes of evaporation have been studied by various research ( [16][17][18]).…”

Section: Introductionmentioning

confidence: 99%

Mathematical model on surface reaction diffusion in the presence of front chemical reaction

Permikin

Zverev

2013

International Journal of Heat and Mass Transfer

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a b s t r a c tThe article discusses a mathematical model of solid-phase diffusion over substance surface accompanied a frontal chemical reaction. The purpose of our article is to describe the concentration distribution and surface reacted layer growth. The model is a system parabolic equations, complicated with the presence of mobile front. It takes account of diffusive fluxes redistribution, sublimation from the surface, chemical reaction reversibility. The asymptotic approximation of the obtained nonlinear problem is constructed. Numerical solution was also carried out. Both numerical and analytical solutions conform to each other in a wide range of parameter changes, whereas observed differences are explained. It was obtained that the reaction front at the substrate surface grows as the fourth root of time in the assumed absence of evaporation and reaction reversibility. In the presence of evaporation the logarithmic distribution law ln(t) is obtained. The theoretical possibility of sharp deceleration and stop of reaction product layer growth is obtained.

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On the Variation of Heat Exchange and Evaporation at the Sea Surface in the Western North Pacific Ocean

Cited by 8 publications

References 7 publications

Insolation and net long-wave radiation off the Oregon coast

Insolation and net long-wave radiation off the Oregon coast

The Stefan problem for unsteady-state evaporation of a volatile component in the solid–liquid–gas systems: Exact analytical solution

Mathematical model on surface reaction diffusion in the presence of front chemical reaction

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