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Unraveling the influence of atmospheric evaporative demand on drought and its response to climate change

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Abstract
This review examines the role of the atmospheric evaporative demand (AED) in drought. AED is a complex concept and here we discuss possible AED definitions, the subsequent metrics to measure and estimate AED, and the different physical drivers that control it. The complex influence of AED on meteorological, environmental/agricultural and hydrological droughts is discussed, stressing the important spatial differences related to the climatological conditions. Likewise, AED influence on drought has implications regarding how different drought metrics consider AED in their attempts to quantify drought severity. Throughout the article, we assess literature findings with respect to: (a) recent drought trends and future projections; (b) the several uncertainties related to data availability; (c) the sensitivity of current drought metrics to AED; and (d) possible roles that both the radiative and physiological effects of increasing atmospheric CO2 concentrations may play as we progress into the future. All these issues preclude identifying a simple effect of the AED on drought severity. Rather it calls for different evaluations of drought impacts and trends under future climate scenarios, considering the complex feedbacks governing the climate system. This article is categorized under: Paleoclimates and Current Trends > Earth System Behavior
Keywords
Geography, Planning and Development, Atmospheric Science, Global and Planetary Change, atmospheric evaporative demand, drought, evaporation, evapotranspiration, STANDARDIZED PRECIPITATION INDEX, ERA-INTERIM REANALYSIS, REGULATED RIVER-BASIN, DIFFERENT TIME-SCALES, WATER-USE EFFICIENCY, LAND-USE CHANGES, PAN EVAPORATION, POTENTIAL EVAPOTRANSPIRATION, SOIL-MOISTURE, TREE MORTALITY

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MLA
Vicente‐Serrano, Sergio M., et al. “Unraveling the Influence of Atmospheric Evaporative Demand on Drought and Its Response to Climate Change.” WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE, vol. 11, no. 2, 2020, doi:10.1002/wcc.632.
APA
Vicente‐Serrano, S. M., McVicar, T. R., Miralles, D., Yang, Y., & Tomas‐Burguera, M. (2020). Unraveling the influence of atmospheric evaporative demand on drought and its response to climate change. WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE, 11(2). https://doi.org/10.1002/wcc.632
Chicago author-date
Vicente‐Serrano, Sergio M., Tim R. McVicar, Diego Miralles, Yuting Yang, and Miquel Tomas‐Burguera. 2020. “Unraveling the Influence of Atmospheric Evaporative Demand on Drought and Its Response to Climate Change.” WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE 11 (2). https://doi.org/10.1002/wcc.632.
Chicago author-date (all authors)
Vicente‐Serrano, Sergio M., Tim R. McVicar, Diego Miralles, Yuting Yang, and Miquel Tomas‐Burguera. 2020. “Unraveling the Influence of Atmospheric Evaporative Demand on Drought and Its Response to Climate Change.” WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE 11 (2). doi:10.1002/wcc.632.
Vancouver
1.
Vicente‐Serrano SM, McVicar TR, Miralles D, Yang Y, Tomas‐Burguera M. Unraveling the influence of atmospheric evaporative demand on drought and its response to climate change. WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE. 2020;11(2).
IEEE
[1]
S. M. Vicente‐Serrano, T. R. McVicar, D. Miralles, Y. Yang, and M. Tomas‐Burguera, “Unraveling the influence of atmospheric evaporative demand on drought and its response to climate change,” WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE, vol. 11, no. 2, 2020.
@article{8654376,
  abstract     = {{This review examines the role of the atmospheric evaporative demand (AED) in drought. AED is a complex concept and here we discuss possible AED definitions, the subsequent metrics to measure and estimate AED, and the different physical drivers that control it. The complex influence of AED on meteorological, environmental/agricultural and hydrological droughts is discussed, stressing the important spatial differences related to the climatological conditions. Likewise, AED influence on drought has implications regarding how different drought metrics consider AED in their attempts to quantify drought severity. Throughout the article, we assess literature findings with respect to: (a) recent drought trends and future projections; (b) the several uncertainties related to data availability; (c) the sensitivity of current drought metrics to AED; and (d) possible roles that both the radiative and physiological effects of increasing atmospheric CO2 concentrations may play as we progress into the future. All these issues preclude identifying a simple effect of the AED on drought severity. Rather it calls for different evaluations of drought impacts and trends under future climate scenarios, considering the complex feedbacks governing the climate system. This article is categorized under: Paleoclimates and Current Trends > Earth System Behavior}},
  articleno    = {{e632}},
  author       = {{Vicente‐Serrano, Sergio M. and McVicar, Tim R. and Miralles, Diego and Yang, Yuting and Tomas‐Burguera, Miquel}},
  issn         = {{1757-7780}},
  journal      = {{WILEY INTERDISCIPLINARY REVIEWS-CLIMATE CHANGE}},
  keywords     = {{Geography,Planning and Development,Atmospheric Science,Global and Planetary Change,atmospheric evaporative demand,drought,evaporation,evapotranspiration,STANDARDIZED PRECIPITATION INDEX,ERA-INTERIM REANALYSIS,REGULATED RIVER-BASIN,DIFFERENT TIME-SCALES,WATER-USE EFFICIENCY,LAND-USE CHANGES,PAN EVAPORATION,POTENTIAL EVAPOTRANSPIRATION,SOIL-MOISTURE,TREE MORTALITY}},
  language     = {{eng}},
  number       = {{2}},
  pages        = {{31}},
  title        = {{Unraveling the influence of atmospheric evaporative demand on drought and its response to climate change}},
  url          = {{http://doi.org/10.1002/wcc.632}},
  volume       = {{11}},
  year         = {{2020}},
}

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