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首页|期刊导航|北京大学学报(自然科学版)|定量研究地球轨道参数和温室气体浓度变化对中全新世气候的影响

定量研究地球轨道参数和温室气体浓度变化对中全新世气候的影响

亢一博 杨海军

北京大学学报(自然科学版)2024,Vol.60Issue(4):607-614,8.
北京大学学报(自然科学版)2024,Vol.60Issue(4):607-614,8.DOI:10.13209/j.0479-8023.2024.039

定量研究地球轨道参数和温室气体浓度变化对中全新世气候的影响

Quantifying the Influence of Changes in Earth's Orbital Parameters and Greenhouse Gases Concentrations on Mid-Holocene Climate

亢一博 1杨海军1

作者信息

  • 1. 复旦大学大气与海洋科学系,上海 200438
  • 折叠

摘要

Abstract

According to the latest Paleoclimate Model Intercomparison Project (PMIP4) protocol,differences between the mid-Holocene and pre-industrial climates were investigated using the fully coupled climate model CESM1.0.The impact of the earth's orbital parameters (ORB) and greenhouse gases (GHG) on mid-Holocene climate change were quantified.Three simulation experiments showed that compared with the pre-industrial simulation,the simulated mid-Holocene was warmer in the high-latitude of the northern Hemisphere,colder in the rest of the world,wetter in most of the northern hemisphere,and drier in the southern hemisphere.The ORB led to warming in the mid-to-high latitudes globally,while GHG played a role in lowering global temperatures and reducing precipitation in the mid-to-high latitudes.These differences in turn induced changes in atmospheric and oceanic circulation,ultimately resulting in differences in the Earth's meridional heat transport.In terms of the variation in total meridional heat transport,ORB exerted approximately five times the climate impact compared with GHG.This study carried positive implications for deepening the understanding of the mid-Holocene climate and its response to various external forcings.

关键词

中全新世/全球气候/地球轨道参数/温室气体/经向热量输送

Key words

mid-Holocene/global climate/earth's orbital parameter/greenhouse gases/meridional heat transport

引用本文复制引用

亢一博,杨海军..定量研究地球轨道参数和温室气体浓度变化对中全新世气候的影响[J].北京大学学报(自然科学版),2024,60(4):607-614,8.

基金项目

国家自然科学基金(42230403,41725021)资助 (42230403,41725021)

北京大学学报(自然科学版)

OA北大核心CSTPCD

0479-8023

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