Recent centennial drought on the Tibetan Plateau is outstanding
within the past 3500 years

J 2025

Recent centennial drought on the Tibetan Plateau is outstanding within the past 3500 years

LIU, Yu; Huiming SONG; Zhisheng AN; Qiang LI; Steven W LEAVITT et al.

Základní údaje

Originální název

Recent centennial drought on the Tibetan Plateau is outstanding within the past 3500 years

Autoři

Vydání

Nature Communications, Heidelberger, Nature Research, 2025, 2041-1723

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10509 Meteorology and atmospheric sciences

Stát vydavatele

Německo

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 15.700 v roce 2024

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/25:00140762

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

Climate-change impacts; Hydrology

Štítky

14315030, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 5. 3. 2025 16:24, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

Given growing concerns about global climate change, it is critical to understand both historical and current shifts in the hydroclimate, particularly in regions critically entwined with global circulation. The Tibetan Plateau, the Earth's largest and highest plateau, is a nexus for global atmospheric processes, significantly influencing East Asian hydroclimate dynamics through the synergy of the Asian Monsoon and the Westerlies. Yet, understanding historical and recent hydroclimate fluctuations and their wide-ranging ecological and societal consequences remains challenging due to short instrumental observations and partly ambiguous proxy reconstructions. Here, we present a precisely-dated 3476-year precipitation reconstruction derived from tree-ring delta 18O data on the Tibetan Plateau, representing one of the few multi-millennia-long annually-resolved terrestrial delta 18O records to date. Our findings reveal that the 20th century drought extremes are severe within the past three millennia, and likely linked to the weakening of both the Asian Monsoon and Westerlies due to anthropogenic aerosol emissions. Additionally, our analyses identified three distinct stages (110 BC-AD 280, AD 330-770 and AD 950-1300) characterized by shifts toward arid hydroclimate conditions, corresponding to significant social unrest and dynasty collapses, which underscores the potential societal impacts of severe hydroclimatic shifts.

Citovat

LIU, Yu; Huiming SONG; Zhisheng AN; Qiang LI; Steven W LEAVITT; Ulf BÜNTGEN; Qiufang CAI; Ruoshi LIU; Congxi FANG; Changfeng SUN; Kerstin TREYDTE; Meng REN; Lidong MO; Yi SONG; Wenju CAI; Quan ZHANG; Weijian ZHOU; Achim BRAEUNING; Jussi GRIESSINGER; Deliang CHEN; Hans W LINDERHOLM; Ashish SINHA; Hai CHENG; Lu WANG; Ying LEI; Junyan SUN; Wei GONG; Xuxiang LI; Linlin CUI; Liang NING; Lingfeng WAN; Thomas W CROWTHER a Constantin M ZOHNER. Recent centennial drought on the Tibetan Plateau is outstanding within the past 3500 years. Nature Communications. Heidelberger: Nature Research, 2025, roč. 16, č. 1, s. 1-9. ISSN 2041-1723. Dostupné z: https://doi.org/10.1038/s41467-025-56687-z.

@article{2481898,
   author = {Liu, Yu and Song, Huiming and An, Zhisheng and Li, Qiang and Leavitt, Steven W and Büntgen, Ulf and Cai, Qiufang and Liu, Ruoshi and Fang, Congxi and Sun, Changfeng and Treydte, Kerstin and Ren, Meng and Mo, Lidong and Song, Yi and Cai, Wenju and Zhang, Quan and Zhou, Weijian and Braeuning, Achim and Griessinger, Jussi and Chen, Deliang and Linderholm, Hans W and Sinha, Ashish and Cheng, Hai and Wang, Lu and Lei, Ying and Sun, Junyan and Gong, Wei and Li, Xuxiang and Cui, Linlin and Ning, Liang and Wan, Lingfeng and Crowther, Thomas W and Zohner, Constantin M},
   article_location = {Heidelberger},
   article_number = {1},
   doi = {https://doi.org/10.1038/s41467-025-56687-z},
   keywords = {Climate-change impacts; Hydrology},
   language = {eng},
   issn = {2041-1723},
   journal = {Nature Communications},
   title = {Recent centennial drought on the Tibetan Plateau is outstanding within the past 3500 years},
   url = {https://doi.org/10.1038/s41467-025-56687-z},
   volume = {16},
   year = {2025}
}

TY  - JOUR
ID  - 2481898
AU  - Liu, Yu - Song, Huiming - An, Zhisheng - Li, Qiang - Leavitt, Steven W - Büntgen, Ulf - Cai, Qiufang - Liu, Ruoshi - Fang, Congxi - Sun, Changfeng - Treydte, Kerstin - Ren, Meng - Mo, Lidong - Song, Yi - Cai, Wenju - Zhang, Quan - Zhou, Weijian - Braeuning, Achim - Griessinger, Jussi - Chen, Deliang - Linderholm, Hans W - Sinha, Ashish - Cheng, Hai - Wang, Lu - Lei, Ying - Sun, Junyan - Gong, Wei - Li, Xuxiang - Cui, Linlin - Ning, Liang - Wan, Lingfeng - Crowther, Thomas W - Zohner, Constantin M
PY  - 2025
TI  - Recent centennial drought on the Tibetan Plateau is outstanding within the past 3500 years
JF  - Nature Communications
VL  - 16
IS  - 1
SP  - 1-9
EP  - 1-9
PB  - Nature Research
SN  - 20411723
KW  - Climate-change impacts
KW  - Hydrology
UR  - https://doi.org/10.1038/s41467-025-56687-z
N2  - Given growing concerns about global climate change, it is critical to understand both historical and current shifts in the hydroclimate, particularly in regions critically entwined with global circulation. The Tibetan Plateau, the Earth's largest and highest plateau, is a nexus for global atmospheric processes, significantly influencing East Asian hydroclimate dynamics through the synergy of the Asian Monsoon and the Westerlies. Yet, understanding historical and recent hydroclimate fluctuations and their wide-ranging ecological and societal consequences remains challenging due to short instrumental observations and partly ambiguous proxy reconstructions. Here, we present a precisely-dated 3476-year precipitation reconstruction derived from tree-ring delta 18O data on the Tibetan Plateau, representing one of the few multi-millennia-long annually-resolved terrestrial delta 18O records to date. Our findings reveal that the 20th century drought extremes are severe within the past three millennia, and likely linked to the weakening of both the Asian Monsoon and Westerlies due to anthropogenic aerosol emissions. Additionally, our analyses identified three distinct stages (110 BC-AD 280, AD 330-770 and AD 950-1300) characterized by shifts toward arid hydroclimate conditions, corresponding to significant social unrest and dynasty collapses, which underscores the potential societal impacts of severe hydroclimatic shifts.
ER  -

LIU, Yu; Huiming SONG; Zhisheng AN; Qiang LI; Steven W LEAVITT; Ulf BÜNTGEN; Qiufang CAI; Ruoshi LIU; Congxi FANG; Changfeng SUN; Kerstin TREYDTE; Meng REN; Lidong MO; Yi SONG; Wenju CAI; Quan ZHANG; Weijian ZHOU; Achim BRAEUNING; Jussi GRIESSINGER; Deliang CHEN; Hans W LINDERHOLM; Ashish SINHA; Hai CHENG; Lu WANG; Ying LEI; Junyan SUN; Wei GONG; Xuxiang LI; Linlin CUI; Liang NING; Lingfeng WAN; Thomas W CROWTHER a Constantin M ZOHNER. Recent centennial drought on the Tibetan Plateau is outstanding within the past 3500 years. \textit{Nature Communications}. Heidelberger: Nature Research, 2025, roč.~16, č.~1, s.~1-9. ISSN~2041-1723. Dostupné z: https://doi.org/10.1038/s41467-025-56687-z.

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