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- W2059581621 abstract "Rainfall was collected in central Pennsylvania from 33 storms during autumn 1989 and spring 1990. The variability of 18O content among 33 storms and within 10 storms is described and also examined in terms of weather type (air mass source and frontal activity) and storm characteristics (rainfall amount, intensity and duration). From storm to storm, the 18O content expressed as δ18O varied greatly (+2.79 to −24.65‰), but showed greatest variability for the smaller rainstorms with low intensities. Also, 18O depletion was greatest for storms of Atlantic (−10.9‰) vs. Gulf (−6.2‰) origin. Within a storm, the 18O content varied greatly, but usually was depleted as the storm continued. For one storm, the δ18O decreased from −4.00 to −20.00‰ over a 10h span of continuous rainfall. The most rapid changes in δ18O (2–6‰ h−1) within a storm occurred mostly during storm intervals characterized by rapidly increasing rainfall intensities associated with moderate to high rainfall rates (more than 5 mm h−1). When these bursts occurred within longer storms, the most rapid changes in 18O content were associated with the higher rainfall intensities." @default.
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- W2059581621 date "1992-09-01" @default.
- W2059581621 modified "2023-10-12" @default.
- W2059581621 title "Intra- and inter-storm 18O trends for selected rainstorms in Pennsylvania" @default.
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- W2059581621 doi "https://doi.org/10.1016/0022-1694(92)90160-w" @default.
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