气候变化研究进展 ›› 2011, Vol. 7 ›› Issue (6): 393-399.
• 气候系统变化 • 上一篇 下一篇
王艳君1,刘波2,翟建青3,苏布达3,罗勇4,张增信5
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摘要: 针对“蒸发悖论”科学问题,从长江流域实际蒸发量变化的原因着手,探讨实际蒸发量与潜在蒸发量之间的关系。研究结果表明:一般情况下当干燥度指数R<0.8时,实际蒸发量与潜在蒸发量为明显的正相反关系,当0.81.0时,实际蒸发量与潜在蒸发量为明显的互补关系。
关键词: 蒸发悖论, 蒸发互补, 潜在蒸发量, 实际蒸发量, 长江流域, evaporation paradox, complementary relationship, potential evaporation, actual evaporation, Yangtze River basin
Abstract: For the scientific issue of “evaporation paradox” the relationship between actual and potential evaporation in the Yangtze River basin was studied in this paper. The results show that roughly when the dryness index R<0.8, the actual evaporation is positively correlated with potential evaporation; when 0.8 1.0, their relationship is complementary.
王艳君 刘波 翟建青 苏布达 罗勇 张增信. 长江流域潜在蒸发量和实际蒸发量的关系[J]. 气候变化研究进展, 2011, 7(6): 393-399.
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