| 拉萨旱涝说 |
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| 引用本文： | 徐近之.拉萨旱涝说[J].气象学报,1937,13(1):24-38. |
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| 作者姓名： | 徐近之 |
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| 摘 要： | 西极遐荒,为世瞩目,拉萨测候,弹指两年,所址虽未如理想,记载之价值已彰;客岁情形,仆尝揭其大要,昭告邦人君子矣。惟是记载时浅,所见不过一斑,加以他无文献可徵,立论流於武断,势所不免,今岁一切,回异乎是;幸羁旅之身犹在,躬自得之,疑窦可去。於二年极短之时间,发如此其大之隐谜,谓非时曾而何。旱欤涝
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| 关 键 词： | 情形 旱涝 西南 雨季 理想 月平均 地表温度 平均温度 藏南 平均雨量 |
The Drought and Flood of Lhasa. |
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| Ginntze Hs&#;.The Drought and Flood of Lhasa.[J].Acta Meteorologica Sinica,1937,13(1):24-38. |
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| Authors: | Ginntze Hs&#; |
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| Abstract: | Two years' rainfall record at Lhasa reveals wide fluctuation and the amount in 1936 is about eleven times the amount in 2935. In 1936 the amount of rainfall received in Nlay, June, July, August and September was 4986.8mm, more than 70% of this amount was contributed by the exceptionally strong southwest monsoon climbing over the lofty ranges of the Himalayas and the other 20% contributed by thunderstorms. |
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