17 O-excess in tropical cyclones reflects local rain re-evaporation more than moisture source conditions
O-17-excess is a relatively new water isotope parameter that could potentially provide useful information about the hydrological cycle. Previous works focusing on O-17-excess in polar regions suggest that it primarily tracks moisture source relative humidity, but little is known about how to interpret O-17-excess data in lower latitudes. Here we present quasi-hourly triple oxygen isotope data of precipitation collected from two tropical cyclones in Texas and Louisiana in 2020 to understand the impacts of environmental and meteorological processes on the(17)O-excess of low-to mid-latitude precipitation. We find that at both hourly time scales and the event scale,O-17-excess is strongly correlated to changes in on-site rainfall intensity and relative humidity, which is consistent with the theory that the isotopic fraction at ion associated with rain re-evaporation lowers the(17)O-excess of the remaining droplet. In addition, although evaporative conditions at the moisture source region may also influence( 17)O-excess of water vapor transported to the precipitation site, their impacts are likely over printed by the post-condensation rain re-evaporation processes. Our results thus suggest that O-17-excess can be used as a proxy for local rather than source region evaporative conditions during tropical cyclones.
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https://n2t.org/ark:/85065/d7df6wc9
eng
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2016-01-01T00:00:00Z
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2024-03-28T00:00:00Z
Copyright author(s). This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License.
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