Holocene temperature response to external forcing: assessing the linear response and its spatial and temporal dependence
Lingfeng Wan,Zhengyu Liu,Jian Liu,Weiyi Sun,and Bin Liu
Lingfeng Wan
Key Laboratory for Virtual Geographic Environment, Ministry of
Education; State Key Laboratory Cultivation Base of Geographical Environment
Evolution of Jiangsu Province; Jiangsu Center for Collaborative Innovation
in Geographical Information Resource Development and Application; School of
Geography Science, Nanjing Normal University, Nanjing, 210023, China
Jiangsu Provincial Key Laboratory for Numerical Simulation of Large
Scale Complex Systems, School of Mathematical Science, Nanjing Normal
University, Nanjing, 210023, China
Key Laboratory for Virtual Geographic Environment, Ministry of
Education; State Key Laboratory Cultivation Base of Geographical Environment
Evolution of Jiangsu Province; Jiangsu Center for Collaborative Innovation
in Geographical Information Resource Development and Application; School of
Geography Science, Nanjing Normal University, Nanjing, 210023, China
Jiangsu Provincial Key Laboratory for Numerical Simulation of Large
Scale Complex Systems, School of Mathematical Science, Nanjing Normal
University, Nanjing, 210023, China
Open Studio for the Simulation of Ocean-Climate-Isotope, Qingdao
National Laboratory for Marine Science and Technology, Qingdao, 266237,
China
Weiyi Sun
Key Laboratory for Virtual Geographic Environment, Ministry of
Education; State Key Laboratory Cultivation Base of Geographical Environment
Evolution of Jiangsu Province; Jiangsu Center for Collaborative Innovation
in Geographical Information Resource Development and Application; School of
Geography Science, Nanjing Normal University, Nanjing, 210023, China
Jiangsu Provincial Key Laboratory for Numerical Simulation of Large
Scale Complex Systems, School of Mathematical Science, Nanjing Normal
University, Nanjing, 210023, China
Bin Liu
Key Laboratory for Virtual Geographic Environment, Ministry of
Education; State Key Laboratory Cultivation Base of Geographical Environment
Evolution of Jiangsu Province; Jiangsu Center for Collaborative Innovation
in Geographical Information Resource Development and Application; School of
Geography Science, Nanjing Normal University, Nanjing, 210023, China
Jiangsu Provincial Key Laboratory for Numerical Simulation of Large
Scale Complex Systems, School of Mathematical Science, Nanjing Normal
University, Nanjing, 210023, China
Viewed
Total article views: 2,969 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,874
958
137
2,969
143
150
HTML: 1,874
PDF: 958
XML: 137
Total: 2,969
BibTeX: 143
EndNote: 150
Views and downloads (calculated since 07 Jan 2019)
Cumulative views and downloads
(calculated since 07 Jan 2019)
Total article views: 2,171 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,419
636
116
2,171
121
137
HTML: 1,419
PDF: 636
XML: 116
Total: 2,171
BibTeX: 121
EndNote: 137
Views and downloads (calculated since 31 Jul 2019)
Cumulative views and downloads
(calculated since 31 Jul 2019)
Total article views: 798 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
455
322
21
798
22
13
HTML: 455
PDF: 322
XML: 21
Total: 798
BibTeX: 22
EndNote: 13
Views and downloads (calculated since 07 Jan 2019)
Cumulative views and downloads
(calculated since 07 Jan 2019)
Viewed (geographical distribution)
Total article views: 2,969 (including HTML, PDF, and XML)
Thereof 2,620 with geography defined
and 349 with unknown origin.
Total article views: 2,171 (including HTML, PDF, and XML)
Thereof 2,034 with geography defined
and 137 with unknown origin.
Total article views: 798 (including HTML, PDF, and XML)
Thereof 586 with geography defined
and 212 with unknown origin.
The linearity of the climate response is strong on orbital and millennial scales throughout the Holocene but poor on the centennial and decadal scale. The regions of strong linear response on the millennial scale are mostly consistent with the orbital scale, notably western Eurasian, North Africa, the subtropical North Pacific, the tropical Atlantic and the Indian Ocean. This finding can improve our understanding of the regional climate response to various climate forcings.
The linearity of the climate response is strong on orbital and millennial scales throughout the...