Skip to main content

ETHNOS_APP

Home • Search • Journals • List 0

Re-examining urban rainfall enhancement over North America

Bibliographic Data

ID15546794
AuthorsS C Pryor (0000-0003-4847-3440, Cornell University, corresponding author), R J Barthelmie (0000-0003-0403-6046, Cornell University), Xin Zhou (0000-0003-2640-6431, Cornell University), George J Huffman (0000-0003-3858-8308, Goddard Space Flight Center)
Year2025
Volume20
Issue3
Pages034035-034035
Publication date2025-02-12
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/adb507
OpenAlexW4407399929
LanguageEN
References cited1

Quantifying intensification/suppression of precipitation over urban areas relative to their rural surroundings can inform efforts to reduce urban flooding. Few studies have systematically addressed whether urban areas exhibit a higher/lower probability of precipitation and/or higher/lower annual total precipitation and/or intensification/weakening of intense precipitation events relative to nearby rural areas across a range of hydroclimatic conditions and urban contexts. Here we address this literature gap using the IMERG V07 data set and analyses of rural and urban samples drawn from 47 conurbations across North America. Specifically, we quantify whether/how precipitation regimes over the urban grid cells differ from those in rural grid cells located 100–250 km from the city center and at a similar elevation. As in previous research, there is evidence that both the probability of precipitation and annual total precipitation are typically higher in the urban grid cells. However, most conurbations have lower upper percentile precipitation rates in the urban sample and lower median precipitation rates above the 95th percentile than are present in samples drawn from rural grid cells. Thus, these conurbations are not, on average, intensifying high-magnitude precipitation events over urban grid cells. Further, the total volume of water accumulated at the surface during events of equivalent duration is not systematically higher over the urban areas, and 20 year return period values of 30 min and wettest pentad precipitation are also not systematically higher over the urban areas. The nature of urban modification of precipitation is a strong function of the prevailing hydroclimate. For example, the heaviest rainfall periods are enhanced over urban grid cells within regional hydroclimates where the overall probability of precipitation and annual total precipitation are low. Conversely, there is evidence for urban suppression of the highest percentile precipitation rates in wetter hydroclimates

Atmospheric sciences · Climatology · Geography · Meteorology · Environmental Science · Flood Risk Assessment and Management · Tropical and Extratropical Cyclones Research · Urban Heat Island Mitigation · Geology

  • Changes in observed climate extremes in global urban areas

    Open Access•Vimal Mishra, Auroop R Ganguly et al.•Environmental Research Letters•2015

Citation velocityhistorical
Highly citedNo

Tools

Open DOIOpen Access
Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae