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Fine-scale processes regulate the response of extreme events to global climate change
Open accessAbstract
We find that extreme temperature and precipitation events are likely to respond substantially to anthropogenically enhanced greenhouse forcing and that fine-scale climate system modifiers are likely to play a critical role in the net response. At present, such events impact a wide variety of natural and human systems, and future changes in their frequency and/or magnitude could have dramatic ecological, economic, and sociological consequences. Our results indicate that fine-scale snow albedo effects influence the response of both hot and cold events and that peak increases in extreme hot events are amplified by surface moisture feedbacks. Likewise, we find that extreme precipitation is enhanced on the lee side of rain shadows and over coastal areas dominated by convective precipitation. We project substantial, spatially heterogeneous increases in both hot and wet events over the contiguous United States by the end of the next century, suggesting that consideration of fine-scale processes is critical for accurate assessment of local- and regional-scale vulnerability to climate change.
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“A weakening of orographic rain shadows related to changes in precipitation extremes has previously been noted in simulations of climate warming over North America [22, 75].”
From Precipitation Extremes Under Climate Change (2015) · cites this paper as [22]
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Metadata
- Authors
- Diffenbaugh, N. S., Pal, J. S., Trapp, R. J., & Giorgi, F.
- Affiliations
- The Abdus Salam International Centre for Theoretical Physics (ICTP) (IT)
- Venue
- Proceedings of the National Academy of Sciences
- Publisher
- National Academy of Sciences
- Published
- 2005-10-19
- Volume
- 102
- Issue
- 44
- Pages
- 15774-15778
- ISSN
- 0027-8424 (ISSN-L)
- 1091-6490
- PMC
- PMC1276070
- OpenAlex
- W2055570283
- Cited by
- 498
- References
- 50
- Citations by year
- 2026: 9 · 2025: 15 · 2024: 18 · 2023: 18 · 2022: 22 · 2021: 23 · 2020: 23 · 2019: 16 · 2018: 19 · 2017: 16 · 2016: 20 · 2015: 35 · 2014: 34 · 2013: 45 · 2012: 37
- FWCI
- 18.35
- Type
- journal article
- Language
- en
- Open access
- green
- europepmc.org
- Locations
- Proceedings of the National Academy of Sciences (publishedVersion)
- Europe PMC (PubMed Central) (publishedVersion)
- PubMed Central (publishedVersion)
- PubMed (publishedVersion)
- Funders
- National Science Foundation (0315677)
- Purdue University
- Abdus Salam International Centre for Theoretical Physics
- Purdue Climate Change Research Center, Purdue University
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate Change and Environmental Impact
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
- Keywords
- temperature extremes, heavy rainfall, climate change response, snow-albedo feedback, rain shadow, convective precipitation, greenhouse forcing, regional climate projections, contiguous United States, climate change vulnerability
- MeSH terms
- Climate, Cold Temperature, Geography, Hot Temperature, Rain, Snow, Temperature, United States
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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