Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/84754
Title: Stable Isotopes of Precipitation During Tropical Sumatra Squalls in Singapore
Authors: He, Shaoneng
Goodkin, Nathalie F.
Kurita, Naoyuki
Wang, Xianfeng
Rubin, Charles Martin
Keywords: El Nino
Stratiform Zone
Issue Date: 2018
Source: He, S., Goodkin, N. F., Kurita, N., Wang, X., & Rubin, C. M. (2018). Stable Isotopes of Precipitation During Tropical Sumatra Squalls in Singapore. Journal of Geophysical Research: Atmospheres, 123(7), 3812-3829.
Series/Report no.: Journal of Geophysical Research: Atmospheres
Abstract: Sumatra Squalls, organized bands of thunderstorms, are the dominant mesoscale convective systems during the intermonsoon and southwest monsoon seasons in Singapore. To understand how they affect precipitation isotopes, we monitored the δ value of precipitation daily and continuously (every second and integrated over 30 s) during all squalls in 2015. We found that precipitation δ18O values mainly exhibit a “V”‐shape pattern and less commonly a “W”‐shape pattern. Variation in δ18O values during a single event is about 1 to 6‰ with the lowest values mostly observed in the stratiform zone, which agrees with previous observations and modeling simulations. Reevaporation can significantly affect δ values, especially in the last stage of the stratiform zone. Daily precipitation is characterized by periodic negative shifts in δ value, largely associated with the squalls rather than moisture source change. The shifts can be more than 10‰, larger than intraevent variation. Initial δ18O values of events are highly variable, and those with the lowest values also have the lowest initial values. Therefore, past convective activities in the upwind area can significantly affect the δ18O, and convection at the sampling site has limited contribution to isotopic variability. A significant correlation between precipitation δ18O value and regional outgoing longwave radiation and rainfall in the Asian monsoon region and western Pacific suggests that regional organized convection probably drives stable isotopic compositions of precipitation. A drop in the frequency of the squalls in 2015 is related to weak organized convection in the region caused by El Niño.
URI: https://hdl.handle.net/10356/84754
http://hdl.handle.net/10220/45120
ISSN: 2169-897X
DOI: 10.1002/2017JD027829
Rights: ©2018 The Authors American Geophysical Union (AGU). This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made.
Fulltext Permission: open
Fulltext Availability: With Fulltext
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