Overview of Observed Clausius-Clapeyron Scaling of Extreme Precipitation in Midlatitudes

This paper presents an overview of recent observational studies on the Clausius-Clapeyron precipitation-temperature (P-T) scaling in midlatitudes. As the capacity of air to hold moisture increases in connection with increasing temperature, extreme precipitation events may become more abundant and in...

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Main Authors: Marta Martinkova, Jan Kysely
Format: Article
Language:English
Published: MDPI AG 2020-07-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/8/786
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author Marta Martinkova
Jan Kysely
author_facet Marta Martinkova
Jan Kysely
author_sort Marta Martinkova
collection DOAJ
description This paper presents an overview of recent observational studies on the Clausius-Clapeyron precipitation-temperature (P-T) scaling in midlatitudes. As the capacity of air to hold moisture increases in connection with increasing temperature, extreme precipitation events may become more abundant and intense. The capacity of air to hold moisture is governed by the Clausius-Clapeyron (CC) relation, approximately 7% per °C. Departures from this, so called super-CC scaling and sub-CC scaling, are consequences of different factors (moisture availability, type of precipitation, annual cycle, the percentile of precipitation intensity and regional weather patterns). Since the moisture availability and enhanced convection were considered as the most important drivers governing the P-T scaling, dew point temperature as a scaling variable is discussed in detail and methods of disaggregation of precipitation events into convective and non-convective are also reviewed.
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spelling doaj.art-8cdd072b2e544de9bd9b8e6374960ac22023-11-20T07:58:22ZengMDPI AGAtmosphere2073-44332020-07-0111878610.3390/atmos11080786Overview of Observed Clausius-Clapeyron Scaling of Extreme Precipitation in MidlatitudesMarta Martinkova0Jan Kysely1Institute of Atmospheric Physics, Czech Academy of Sciences, 14100 Prague 4, Czech RepublicInstitute of Atmospheric Physics, Czech Academy of Sciences, 14100 Prague 4, Czech RepublicThis paper presents an overview of recent observational studies on the Clausius-Clapeyron precipitation-temperature (P-T) scaling in midlatitudes. As the capacity of air to hold moisture increases in connection with increasing temperature, extreme precipitation events may become more abundant and intense. The capacity of air to hold moisture is governed by the Clausius-Clapeyron (CC) relation, approximately 7% per °C. Departures from this, so called super-CC scaling and sub-CC scaling, are consequences of different factors (moisture availability, type of precipitation, annual cycle, the percentile of precipitation intensity and regional weather patterns). Since the moisture availability and enhanced convection were considered as the most important drivers governing the P-T scaling, dew point temperature as a scaling variable is discussed in detail and methods of disaggregation of precipitation events into convective and non-convective are also reviewed.https://www.mdpi.com/2073-4433/11/8/786Clausius-Clapeyron scalingprecipitation extremesmidlatitudes
spellingShingle Marta Martinkova
Jan Kysely
Overview of Observed Clausius-Clapeyron Scaling of Extreme Precipitation in Midlatitudes
Atmosphere
Clausius-Clapeyron scaling
precipitation extremes
midlatitudes
title Overview of Observed Clausius-Clapeyron Scaling of Extreme Precipitation in Midlatitudes
title_full Overview of Observed Clausius-Clapeyron Scaling of Extreme Precipitation in Midlatitudes
title_fullStr Overview of Observed Clausius-Clapeyron Scaling of Extreme Precipitation in Midlatitudes
title_full_unstemmed Overview of Observed Clausius-Clapeyron Scaling of Extreme Precipitation in Midlatitudes
title_short Overview of Observed Clausius-Clapeyron Scaling of Extreme Precipitation in Midlatitudes
title_sort overview of observed clausius clapeyron scaling of extreme precipitation in midlatitudes
topic Clausius-Clapeyron scaling
precipitation extremes
midlatitudes
url https://www.mdpi.com/2073-4433/11/8/786
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