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

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F20%3A00531851" target="_blank" >RIV/68378289:_____/20:00531851 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/60460709:41330/20:82197

Výsledek na webu

<a href="https://www.mdpi.com/2073-4433/11/8/786/htm" target="_blank" >https://www.mdpi.com/2073-4433/11/8/786/htm</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.3390/atmos11080786" target="_blank" >10.3390/atmos11080786</a>

Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

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

Popis výsledku anglicky

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.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10509 - Meteorology and atmospheric sciences

Projekt

<a href="/cs/project/GA20-28560S" target="_blank" >GA20-28560S: Řídící mechanismy extrémů v reanalýze a klimatických modelech</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2020

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Atmosphere

ISSN

2073-4433

e-ISSN

—

Svazek periodika

11

Číslo periodika v rámci svazku

8

Stát vydavatele periodika

CH - Švýcarská konfederace

Počet stran výsledku

16

Strana od-do

786

Kód UT WoS článku

000564761600001

EID výsledku v databázi Scopus

2-s2.0-85089557918