The Budyko hypothesis before Budyko: The hydrological legacy of Evald Oldekop
The Budyko hypothesis before Budyko: The hydrological legacy of Evald Oldekop
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DOI：
10.1016/j.jhydrol.2016.02.002
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发表时间：
2016-04
影响因子：
6.4
通讯作者：
V. Andréassian;Ü. Mander;T. Pae
中科院分区：
文献类型：
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作者：
V. Andréassian;Ü. Mander;T. Pae
在水文学术语中，Budyko假说是指地球表面长期的水和能量平衡在很大程度上取决于一个单一的干旱比φ=Ex/P（其中Pres代表长期降水量[mm/yr]和Ex代表长期最大蒸发量[mm/yr]）的假说。在这篇历史笔记中，我们分析了Evald Oldekop（1885-1952）的贡献，他不仅启发了Budyko的工作，而且在Thornthwaite引入潜在蒸散量概念之前三十多年提出了最大集水蒸发量的概念。
In the hydrological jargon, theBudyko hypothesisrefers to the hypothesis according to which the long-term water and energy balances of the Earth’s surface are largely dependent upon a single aridity ratioφ=Ex/P(wherePrepresents long-term precipitation [mm/yr] andExlong-term maximum evaporation [mm/yr]). In this historical note, we analyze the contribution of Evald Oldekop (1885–1952), who not only inspired Budyko’s work, but also proposed the concept of maximum catchment evaporation more than three decades before Thornthwaite introduced the concept of potential evapotranspiration.