The response of the hydrological cycle to temperature changes in recent and distant climatic history

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F22%3A91278" target="_blank" >RIV/60460709:41330/22:91278 - isvavai.cz</a>

Výsledek na webu

<a href="https://progearthplanetsci.springeropen.com/articles/10.1186/s40645-022-00489-0" target="_blank" >https://progearthplanetsci.springeropen.com/articles/10.1186/s40645-022-00489-0</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1186/s40645-022-00489-0" target="_blank" >10.1186/s40645-022-00489-0</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The response of the hydrological cycle to temperature changes in recent and distant climatic history

Popis výsledku v původním jazyce

The relationship between the hydrological cycle and the temperature is rather complex and of great importance to human socioeconomic activities. The prevailing theory suggests that as temperature increases the hydrological cycle is intensified. Practically, this means more and heavier precipitation. However, the exact magnitude of hydrological cycle response and its spatiotemporal characteristics is still under investigation. Looking back in Earths hydroclimatic history, it is easy to find some periods where global temperature was substantially different than present. Here, we examine some of these periods to present the current knowledge about past hydrological cycle variability, specifically precipitation, and its relationship to temperature. The periods under investigation are the Mid Miocene Climate Optimum, the Eemian Interglacial Stage, the Last Glacial Maximum, the Heinrich and Dansgaard Oeschger Events, the Bolling-Allerod, the Younger Dryas, the 8,2 ka event, the Medieval Climate Anomaly, an

Název v anglickém jazyce

The response of the hydrological cycle to temperature changes in recent and distant climatic history

Popis výsledku anglicky

The relationship between the hydrological cycle and the temperature is rather complex and of great importance to human socioeconomic activities. The prevailing theory suggests that as temperature increases the hydrological cycle is intensified. Practically, this means more and heavier precipitation. However, the exact magnitude of hydrological cycle response and its spatiotemporal characteristics is still under investigation. Looking back in Earths hydroclimatic history, it is easy to find some periods where global temperature was substantially different than present. Here, we examine some of these periods to present the current knowledge about past hydrological cycle variability, specifically precipitation, and its relationship to temperature. The periods under investigation are the Mid Miocene Climate Optimum, the Eemian Interglacial Stage, the Last Glacial Maximum, the Heinrich and Dansgaard Oeschger Events, the Bolling-Allerod, the Younger Dryas, the 8,2 ka event, the Medieval Climate Anomaly, an

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10501 - Hydrology

Projekt

—

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2022

Kód důvěrnosti údajů

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

Název periodika

PROGRESS IN EARTH AND PLANETARY SCIENCE

ISSN

2197-4284

e-ISSN

—

Svazek periodika

9

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

37

Strana od-do

1-37

Kód UT WoS článku

000803951300001

EID výsledku v databázi Scopus

2-s2.0-85131003364