Lack of cold temperatures is driving recent high‑summer warming in the southern Rocky Mountains
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F25%3A00639835" target="_blank" >RIV/86652079:_____/25:00639835 - isvavai.cz</a>
Výsledek na webu
<a href="https://link.springer.com/article/10.1007/s00484-025-02904-9" target="_blank" >https://link.springer.com/article/10.1007/s00484-025-02904-9</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00484-025-02904-9" target="_blank" >10.1007/s00484-025-02904-9</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Lack of cold temperatures is driving recent high‑summer warming in the southern Rocky Mountains
Popis výsledku v původním jazyce
We present a 483-year-long tree-ring chronology from a high-elevation Engelmann spruce stand in central Colorado. Over 800,000 density measurements produce a maximum latewood density (MXD) record, which together with tree-ring widths, is used to assess the climatic influences on radial tree growth. Variability in MXD is strongly related to local and regional August maximum temperatures (T-max) for 127 years of overlapping instrumental climate data. A single-predictor reconstruction based on the MXD record explains > 50% of the variance in regional August T-max is presented and considered robust for the period 1662-2021. The estimates of past temperature variability display phases of continuous cold conditions that are beyond the range of the instrumental record, including the 1830s. Our results further indicate that August T-max have been higher since the early 1990s than for any other 30-year period in the past 350 years. This recent increase occurs on top of multi-centennial warming, and appears to be driven mainly by less frequent cold summers rather than an increase in warm extremes.
Název v anglickém jazyce
Lack of cold temperatures is driving recent high‑summer warming in the southern Rocky Mountains
Popis výsledku anglicky
We present a 483-year-long tree-ring chronology from a high-elevation Engelmann spruce stand in central Colorado. Over 800,000 density measurements produce a maximum latewood density (MXD) record, which together with tree-ring widths, is used to assess the climatic influences on radial tree growth. Variability in MXD is strongly related to local and regional August maximum temperatures (T-max) for 127 years of overlapping instrumental climate data. A single-predictor reconstruction based on the MXD record explains > 50% of the variance in regional August T-max is presented and considered robust for the period 1662-2021. The estimates of past temperature variability display phases of continuous cold conditions that are beyond the range of the instrumental record, including the 1830s. Our results further indicate that August T-max have been higher since the early 1990s than for any other 30-year period in the past 350 years. This recent increase occurs on top of multi-centennial warming, and appears to be driven mainly by less frequent cold summers rather than an increase in warm extremes.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10509 - Meteorology and atmospheric sciences
Návaznosti výsledku
Projekt
<a href="/cs/project/EH22_008%2F0004635" target="_blank" >EH22_008/0004635: AdAgriF - Pokročilé metody redukce emisí a sekvestrace skleníkových plynů v zemědělské a lesní krajině pro mitigaci změny klimatu</a><br>
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2025
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
International Journal of Biometeorology
ISSN
0020-7128
e-ISSN
1432-1254
Svazek periodika
69
Číslo periodika v rámci svazku
6
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
12
Strana od-do
1475-1486
Kód UT WoS článku
001456489800001
EID výsledku v databázi Scopus
2-s2.0-105001525052