A positive altitude gradient of isotopes in the precipitation over the Tianshan Mountains: Effects of moisture recycling and sub-cloud evaporation
A negative stable isotope-altitude gradient is commonly observed on the windward side of a
mountain. However, after the precipitation passes over a mountain range to the leeward
side, the altitude effect becomes ambiguous as a result of an orographic rain shadow in
addition to other complex processes such as sub-cloud evaporation and additional moisture
mixing. In this study, we found a positive precipitation δ 18 O-altitude gradient with a value of
0.12‰/100 m in the Urumqi River catchments on the leeward side of the Tianshan …
mountain. However, after the precipitation passes over a mountain range to the leeward
side, the altitude effect becomes ambiguous as a result of an orographic rain shadow in
addition to other complex processes such as sub-cloud evaporation and additional moisture
mixing. In this study, we found a positive precipitation δ 18 O-altitude gradient with a value of
0.12‰/100 m in the Urumqi River catchments on the leeward side of the Tianshan …
[引用][C] A positive altitude gradient of isotopes in the precipitation over the Tianshan Mountains: effects of moisture recycling and sub-cloud evaporation.
KYL Kong YanLong, PZH Pang ZhongHe - 2016 - cabidigitallibrary.org
A negative stable isotope-altitude gradient is commonly observed on the windward side of a
mountain. However, after the precipitation passes over a mountain range to the leeward
side, the altitude effect becomes ambiguous as a result of an orographic rain shadow in
addition to other complex processes such as sub-cloud evaporation and additional moisture
mixing. In this study, we found a positive precipitation δ18O-altitude gradient with a value of
0.12 per mil/100 m in the Urumqi River catchments on the leeward side of the Tianshan …
mountain. However, after the precipitation passes over a mountain range to the leeward
side, the altitude effect becomes ambiguous as a result of an orographic rain shadow in
addition to other complex processes such as sub-cloud evaporation and additional moisture
mixing. In this study, we found a positive precipitation δ18O-altitude gradient with a value of
0.12 per mil/100 m in the Urumqi River catchments on the leeward side of the Tianshan …
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