European warm-season temperature and hydroclimate since 850 CE

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F19%3A00507777" target="_blank" >RIV/86652079:_____/19:00507777 - isvavai.cz</a>

Alternative codes found

RIV/00216224:14310/19:00113480

Result on the web

<a href="https://iopscience.iop.org/article/10.1088/1748-9326/ab2c7e" target="_blank" >https://iopscience.iop.org/article/10.1088/1748-9326/ab2c7e</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1088/1748-9326/ab2c7e" target="_blank" >10.1088/1748-9326/ab2c7e</a>

Result language

angličtina

Original language name

European warm-season temperature and hydroclimate since 850 CE

Original language description

The long-term relationship between temperature and hydroclimate has remained uncertain due to the short length of instrumental measurements and inconsistent results from climate model simulations. This lack of understanding is particularly critical with regard to projected drought and flood risks. Here we assess warm-season co-variability patterns between temperature and hydroclimate over Europe back to 850 CE using instrumental measurements, tree-ring based reconstructions, and climate model simulations. We find that the temperature-hydroclimate relationship in both the instrumental and reconstructed data turns more positive at lower frequencies, but less so in model simulations, with a dipole emerging between positive (warm and wet) and negative (warm and dry) associations in northern and southern Europe, respectively. Compared to instrumental data, models reveal a more negative co-variability across all timescales, while reconstructions exhibit a more positive co-variability. Despite the observed differences in the temperature-hydroclimate co-variability patterns in instrumental, reconstructed and model simulated data, we find that all data types share relatively similar phase-relationships between temperature and hydroclimate, indicating the common influence of external forcing. The co-variability between temperature and soil moisture in the model simulations is overestimated, implying a possible overestimation of temperature-driven future drought risks.

Czech name

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Czech description

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Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

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OECD FORD branch

10509 - Meteorology and atmospheric sciences

Project

<a href="/en/project/EF16_019%2F0000797" target="_blank" >EF16_019/0000797: SustES - Adaptation strategies for sustainable ecosystem services and food security under adverse environmental conditions</a><br>

Continuities

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

Publication year

2019

Confidentiality

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

Name of the periodical

Environmental Research Letters

ISSN

1748-9326

e-ISSN

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Volume of the periodical

14

Issue of the periodical within the volume

8

Country of publishing house

GB - UNITED KINGDOM

Number of pages

17

Pages from-to

084015

UT code for WoS article

000478753700002

EID of the result in the Scopus database

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