Persistent multi-scale fluctuations shift European hydroclimate to its millennial boundaries

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F18%3A77014" target="_blank" >RIV/60460709:41330/18:77014 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/68378289:_____/18:00489364

Výsledek na webu

<a href="http://dx.doi.org/10.1038/s41467-018-04207-7" target="_blank" >http://dx.doi.org/10.1038/s41467-018-04207-7</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1038/s41467-018-04207-7" target="_blank" >10.1038/s41467-018-04207-7</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Persistent multi-scale fluctuations shift European hydroclimate to its millennial boundaries

Popis výsledku v původním jazyce

In recent years, there has been growing concern about the effect of global warming on water resources, especially at regional and continental scales. The last IPCC report on extremes states that there is medium confidence about an increase on European drought frequency during twentieth century. Here we use the Old World Drought Atlas palaeoclimatic reconstruction to show that when Europes hydroclimate is examined under a millennial, multi-scale perspective, a significant decrease in dryness can be observed since 1920 over most of central and northern Europe. On the contrary, in the south, drying conditions have prevailed, creating an intense north-to-south dipole. In both cases, hydroclimatic conditions have shifted to, and in some regions exceeded, their millennial boundaries, remaining at these extreme levels for the longest period of the 1000 year long record.

Název v anglickém jazyce

Persistent multi-scale fluctuations shift European hydroclimate to its millennial boundaries

Popis výsledku anglicky

In recent years, there has been growing concern about the effect of global warming on water resources, especially at regional and continental scales. The last IPCC report on extremes states that there is medium confidence about an increase on European drought frequency during twentieth century. Here we use the Old World Drought Atlas palaeoclimatic reconstruction to show that when Europes hydroclimate is examined under a millennial, multi-scale perspective, a significant decrease in dryness can be observed since 1920 over most of central and northern Europe. On the contrary, in the south, drying conditions have prevailed, creating an intense north-to-south dipole. In both cases, hydroclimatic conditions have shifted to, and in some regions exceeded, their millennial boundaries, remaining at these extreme levels for the longest period of the 1000 year long record.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10501 - Hydrology

Projekt

<a href="/cs/project/GA16-16549S" target="_blank" >GA16-16549S: Půdní a hydrologické sucho v měnícím se klimatu</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2018

Kód důvěrnosti údajů

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

Název periodika

Nature Communications

ISSN

2041-1723

e-ISSN

2041-1723

Svazek periodika

9

Číslo periodika v rámci svazku

1767

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

12

Strana od-do

1-12

Kód UT WoS článku

000431206400008

EID výsledku v databázi Scopus

2-s2.0-85046467964