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: 2,987 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,886
962
139
2,987
145
151
HTML: 1,886
PDF: 962
XML: 139
Total: 2,987
BibTeX: 145
EndNote: 151
Views and downloads (calculated since 07 Jan 2019)
Cumulative views and downloads
(calculated since 07 Jan 2019)
Total article views: 2,186 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
1,431
637
118
2,186
123
138
HTML: 1,431
PDF: 637
XML: 118
Total: 2,186
BibTeX: 123
EndNote: 138
Views and downloads (calculated since 31 Jul 2019)
Cumulative views and downloads
(calculated since 31 Jul 2019)
Total article views: 801 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
BibTeX
EndNote
455
325
21
801
22
13
HTML: 455
PDF: 325
XML: 21
Total: 801
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: 2,987 (including HTML, PDF, and XML)
Thereof 2,637 with geography defined
and 350 with unknown origin.
Total article views: 2,186 (including HTML, PDF, and XML)
Thereof 2,048 with geography defined
and 138 with unknown origin.
Total article views: 801 (including HTML, PDF, and XML)
Thereof 589 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...
