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Ocean fronts as decadal thermostats modulating continental warming hiatus.
Sung, Mi-Kyung; An, Soon-Il; Shin, Jongsoo; Park, Jae-Heung; Yang, Young-Min; Kim, Hyo-Jeong; Chang, Minhee.
Afiliação
  • Sung MK; Climate and Environmental Research Institute, Korea Institute of Science and Technology, Seoul, Republic of Korea. mksung@kist.re.kr.
  • An SI; Department of Atmospheric Sciences/Irreversible Climate Change Research Center, Yonsei University, Seoul, Republic of Korea. sian@yonsei.ac.kr.
  • Shin J; Division of Environmental Science and Engineering, Pohang University of Science and Technology, Pohang, Republic of Korea. sian@yonsei.ac.kr.
  • Park JH; Woods Hole Oceanographic Institution, Woods Hole, MA, USA.
  • Yang YM; School of Earth and Environmental Sciences, Seoul National University, Seoul, Republic of Korea.
  • Kim HJ; Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environment Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and T
  • Chang M; Low-Carbon and Climate Impact Research Centre, School of Energy and Environment, City University of Hong Kong, Hong Kong SAR, China.
Nat Commun ; 14(1): 7777, 2023 Nov 27.
Article em En | MEDLINE | ID: mdl-38012176
ABSTRACT
Over the past decade, an unexpected cooling trend has been observed in East Asia and North America during winter. Climate model simulations suggest that this pattern of stalled warming, besides accelerated warming, will repeat throughout the course of global warming, influenced by the natural decade-long variations in the climate system. However, understanding the exact factors affecting the pace of warming remains a challenge. Here we show that a pause in warming over continental areas-namely, local warming hiatus-can be accompanied by excessive heat accumulation north of the ocean fronts. This oceanic condition, often manifesting in the form of marine heatwaves, constrains the subseasonal growth of atmospheric planetary waves, significantly increasing the likelihood of cold extremes in downstream continents. Our results underscore the importance of closely monitoring changing ocean fronts in response to human-induced warming, which can potentially reshape the inherent decade-long fluctuations within regional climates over the long term.

Texto completo: 1 Base de dados: MEDLINE Idioma: En Ano de publicação: 2023 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Idioma: En Ano de publicação: 2023 Tipo de documento: Article