地理研究 ›› 1985, Vol. 4 ›› Issue (1): 14-21.doi: 10.11821/yj1985010002
• 论文 •
陈永申, 李克让, 沙万英
Chen Yongshen, Li Kerang, Sha Wanying
Abstract: To estimate the total heating intensity transported upwards from the sea surface to atmosphere over the Northwest Pacific ocean, the authors employed the following formula.Qa=QLE±QH+QEF where Q, denotes the total heating intensity, QLE the latent heat of evaporation QH the sensible heat exchange and QEF the effective longwave radiation.Results indicate that the largest center of the Qa occurs over the Kuro-shio warm current but not coincides with the largest absorbed radiation. The values of the annual tolal heating intensity was mainly determined in winter and autumn. A large proportion of the surplus solar energy absorbed at the sea surface during sumer is stored by the oceans, and is released to the atmosphere during the colder seasons when there is a deficiency in solar energy. By the same mechanism much of the solar energy absorbed at the low latitudes is transported by ocean currents and released to the atmosphere at the higher latitues where receipt of solar energy is also comparatively deficient.
陈永申, 李克让, 沙万英. 西北太平洋海面总加热强度的时空特征[J]. 地理研究, 1985, 4(1): 14-21.
Chen Yongshen, Li Kerang, Sha Wanying. SPACE-TIME CHARACTERISTICS OF THE TOTAL HEATING INTENSITY OF THE SEA SURFACE OVER THE NORTHWEST PACTIFIC[J]. GEOGRAPHICAL RESEARCH, 1985, 4(1): 14-21.
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