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David R. Easterling

University of Illinois Urbana-Champaign

ORCID: 0000-0001-9691-0647

Publishes on Climate variability and models, Meteorological Phenomena and Simulations, Atmospheric and Environmental Gas Dynamics. 201 papers and 30.2k citations.

201Publications
30.2kTotal Citations

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Top publicationsby citations

Climate Extremes: Observations, Modeling, and Impacts
Cited by 4.9k

One of the major concerns with a potential change in climate is that an increase in extreme events will occur. Results of observational studies suggest that in many areas that have been analyzed, changes in total precipitation are amplified at the tails, and changes in some temperature extremes have been observed. Model output has been analyzed that shows changes in extreme events for future climates, such as increases in extreme high temperatures, decreases in extreme low temperatures, and increases in intense precipitation events. In addition, the societal infrastructure is becoming more sensitive to weather and climate extremes, which would be exacerbated by climate change. In wild plants and animals, climate-induced extinctions, distributional and phenological changes, and species' range shifts are being documented at an increasing rate. Several apparently gradual biological changes are linked to responses to extreme weather and climate events.

Changes in Climate Extremes and their Impacts on the Natural Physical Environment
Sonia I. Seneviratne, Neville Nicholls, David R. Easterling et al.|Cambridge University Press eBooks|2012
Cited by 2.4kOpen Access

Chapter 3 of Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation. A Special Report of Working Groups I and II of the Intergovernmental Panel on Climate Change (IPCC). This chapter addresses changes in weather and climate events relevant to extreme impacts and disasters.

Maximum and Minimum Temperature Trends for the Globe
Cited by 1.6k

Analysis of the global mean surface air temperature has shown that its increase is due, at least in part, to differential changes in daily maximum and minimum temperatures, resulting in a narrowing of the diurnal temperature range (DTR). The analysis, using station metadata and improved areal coverage for much of the Southern Hemisphere landmass, indicates that the DTR is continuing to decrease in most parts of the world, that urban effects on globally and hemispherically averaged time series are negligible, and that circulation variations in parts of the Northern Hemisphere appear to be related to the DTR. Atmospheric aerosol loading in the Southern Hemisphere is much less than that in the Northern Hemisphere, suggesting that there are likely a number of factors, such as increases in cloudiness, contributing to the decreases in DTR.

Observed Variability and Trends in Extreme Climate Events: A Brief Review<sup>*</sup>
David R. Easterling, Jenni L. Evans, Pavel Groisman et al.|Bulletin of the American Meteorological Society|2000
Cited by 1.3kOpen Access

Variations and trends in extreme climate events have only recently received much attention. Exponentially increasing economic losses, coupled with an increase in deaths due to these events, have focused attention on the possibility that these events are increasing in frequency. One of the major problems in examining the climate record for changes in extremes is a lack of high-quality, long-term data. In some areas of the world increases in extreme events are apparent, while in others there appears to be a decline. Based on this information increased ability to monitor and detect multidecadal variations and trends is critical to begin to detect any observed changes and understand their origins.