Preprints
https://doi.org/10.5194/nhess-2021-46
https://doi.org/10.5194/nhess-2021-46

  18 Feb 2021

18 Feb 2021

Review status: a revised version of this preprint was accepted for the journal NHESS and is expected to appear here in due course.

Changes in drought features at European level over the last 120 years

Monica Ionita1 and Viorica Nagavciuc1,2 Monica Ionita and Viorica Nagavciuc
  • 1Alfred Wegner Institute Helmholtz Center for Polar and Marine Research, Bremerhaven, Germany
  • 2Forest Biometrics Laboratory – Faculty of Forestry, ”Stefan cel Mare” University of Suceava, Suceava, Romania

Abstract. In this study we analyze the drought features at European level over the period 1901–2019, using three drought indices: the Standardized precipitation (SPI), the Standardized Precipitation Evapotranspiration Index (SPEI) and the self-calibrated Palmer Drought Severity Index (scPDSI). The results based on the SPEI and scPDSI indices point out to the fact that central Europe (CEU) and the Mediterranean region (MED) are becoming dryer, due to an increase in the potential evapotranspiration and the mean air temperature, while the northern part of Europe (NEU) is becoming wetter. By contrast, the SPI drought index does not reveal these changes in the drought variability, mainly due to the fact that the precipitation does not exhibit a significant change, especially over CEU. SPEI12 indicates a significant increase both in the frequency and area over the last three decades for MED and CEU, while SPI12 is not capturing these features. By analyzing the joint probability of compound events (e.g. high temperatures/droughts), we show that the potential evapotranspiration and the mean air temperature are becoming essential components for drought occurrence over CEU and MED. This, together with the projected increase in the potential evapotranspiration under a warming climate, has significant implications concerning the future occurrence of drought events, especially for MED and CEU regions.

Monica Ionita and Viorica Nagavciuc

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on nhess-2021-46', Anonymous Referee #1, 23 Mar 2021
  • RC2: 'Comment on nhess-2021-46', Anonymous Referee #2, 26 Mar 2021

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on nhess-2021-46', Anonymous Referee #1, 23 Mar 2021
  • RC2: 'Comment on nhess-2021-46', Anonymous Referee #2, 26 Mar 2021

Monica Ionita and Viorica Nagavciuc

Monica Ionita and Viorica Nagavciuc

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Short summary
By analyzing the joint probability of compound events (e.g. high temperatures/droughts), we show that the potential evapotranspiration and the mean air temperature are becoming essential components for drought occurrence over Central Europe (CEU) and the Mediterranean region (MED). This, together with the projected increase in the potential evapotranspiration under a warming climate, has significant implications concerning the future occurrence of drought events over these regions.
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