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International Journal of Climatology
Open accessAbstract
In dry (wet) summers, the rainout on the southwest and southeast monsoon moisture transporting pathways is stronger (weaker) than normal, which, however, co-occurs with a higher (lower) δ18Op value in the basin, indicating that the local rainout caused by the local rainfall seems to be the dominant control of the δ18Op in dry (wet) summers. The figure shows the composite spatial distribution of the water vapour flux (vector), anomalous δ18Op (shaded, red for positive and blue for negative anomalies) and precipitation (contour, solid for positive and dashed for negative anomalies) in the Asian monsoon region in dry and wet summers. The red square represents the location of the Dongting Lake basin; the solid (or dashed) red and orange contours indicate the position of WPSH in 5880 and 5870 geopotential height meters, respectively, in normal (or dry/wet) summers; the water vapour flux is shown that reaches 0.1 confidence limits for the t test.
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The European mountain cryosphere: a review of its current state, trends, and future challenges
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Osman, M. B., Tierney, J. E., Zhu, J., Tardif, R., Hakim, G. J., King, J., & Poulsen, C. J. (2021) · Nature · doi:10.1038/s41586-021-03984-4 · Cited by 574
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Metadata
- Venue
- International Journal of Climatology
- Publisher
- Wiley
- Published
- 2006-03-07
- ISSN
- 0899-8418 (ISSN-L)
- OpenAlex
- W4231746097
- Cited by
- 2,231
- References
- 0
- Type
- paratext
- Language
- en
- Open access
- green
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