Mediterranean winter snowfall variability over the past millennium

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F19%3A00493123" target="_blank" >RIV/86652079:_____/19:00493123 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/00216224:14310/19:00113746

Výsledek na webu

<a href="https://rmets.onlinelibrary.wiley.com/doi/full/10.1002/joc.5814" target="_blank" >https://rmets.onlinelibrary.wiley.com/doi/full/10.1002/joc.5814</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1002/joc.5814" target="_blank" >10.1002/joc.5814</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Mediterranean winter snowfall variability over the past millennium

Popis výsledku v původním jazyce

The brevity of the instrumental record limits our understanding of snowfall variability and its directional patterns in the Mediterranean region. Here, we develop a 1,208-year-long (800–2017 CE) reconstruction of central Mediterranean snowfall variability based on documentary evidence from Italy. The record suggests that the recent reduction in Italian snowfall intensity is not unprecedented over the past millennium, since comparable patterns of low snowfall intensity also occurred during the Medieval Climate Anomaly. Increased snowfall during the Little Ice Age, however, was most likely associated with a shift of the Atlantic multi-decadal variability towards negative values, and this overall cold phase further coincided with increased volcanic activity. Our findings on natural snowfall variability over the central Mediterranean in the past millennium provide a unique winter proxy for validating output from climate model simulations.

Název v anglickém jazyce

Mediterranean winter snowfall variability over the past millennium

Popis výsledku anglicky

The brevity of the instrumental record limits our understanding of snowfall variability and its directional patterns in the Mediterranean region. Here, we develop a 1,208-year-long (800–2017 CE) reconstruction of central Mediterranean snowfall variability based on documentary evidence from Italy. The record suggests that the recent reduction in Italian snowfall intensity is not unprecedented over the past millennium, since comparable patterns of low snowfall intensity also occurred during the Medieval Climate Anomaly. Increased snowfall during the Little Ice Age, however, was most likely associated with a shift of the Atlantic multi-decadal variability towards negative values, and this overall cold phase further coincided with increased volcanic activity. Our findings on natural snowfall variability over the central Mediterranean in the past millennium provide a unique winter proxy for validating output from climate model simulations.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10509 - Meteorology and atmospheric sciences

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2019

Kód důvěrnosti údajů

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

Název periodika

International Journal of Climatology

ISSN

0899-8418

e-ISSN

—

Svazek periodika

39

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

11

Strana od-do

384-394

Kód UT WoS článku

000459638400029

EID výsledku v databázi Scopus

2-s2.0-85052402868