Holocene seasonal temperature evolution and spatial variability over the Northern Hemisphere landmass
The study reconstructed Holocene seasonal temperatures using 1,310 pollen records covering the Northern Hemisphere landmass, and show that both summer and winter temperatures peaked at ~7 ka BP, but with significant spatial variability.
Main Authors: | Wenchao Zhang, Haibin Wu, Jun Cheng, Junyan Geng, Qin Li, Yong Sun, Yanyan Yu, Huayu Lu, Zhengtang Guo |
---|---|
Format: | Article |
Language: | English |
Published: |
Nature Portfolio
2022-09-01
|
Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-022-33107-0 |
Similar Items
-
Seasonally dependent increases in subweekly temperature variability over Southern Hemisphere landmasses detected in multiple reanalyses
by: P. Martineau, et al.
Published: (2024-01-01) -
Observed earlier start of the growing season from middle to high latitudes across the Northern Hemisphere snow-covered landmass for the period 2001–2014
by: Xiaona Chen, et al.
Published: (2020-01-01) -
Projected 21st century changes in snow water equivalent over Northern Hemisphere landmasses from the CMIP5 model ensemble
by: H. X. Shi, et al.
Published: (2015-10-01) -
Response of Westerly Jet Over the Northern Hemisphere to Astronomical Insolation During the Holocene
by: Peng Zhou, et al.
Published: (2020-07-01) -
Landmasses and Railways, Bertrand Fleuret
by: Jan Baetens
Published: (2010-08-01)