Matches in SemOpenAlex for { <https://semopenalex.org/work/W4295113599> ?p ?o ?g. }
- W4295113599 abstract "The origin of the temperature divergence between Holocene proxy reconstructions and model simulations remains controversial, but it possibly results from potential biases in the seasonality of reconstructions or in the climate sensitivity of models. Here we present an extensive dataset of Holocene seasonal temperatures reconstructed using 1310 pollen records covering the Northern Hemisphere landmass. Our results indicate that both summer and winter temperatures warmed from the early to mid-Holocene (~11-7 ka BP) and then cooled thereafter, but with significant spatial variability. Strong early Holocene warming trend occurred mainly in Europe, eastern North America and northern Asia, which can be generally captured by model simulations and is likely associated with the retreat of continental ice sheets. The subsequent cooling trend is pervasively recorded except for northern Asia and southeastern North America, which may reflect the cross-seasonal impact of the decreasing summer insolation through climatic feedbacks, but the cooling in winter season is not well reproduced by climate models. Our results challenge the proposal that seasonal biases in proxies are the main origin of model-data discrepancies and highlight the critical impact of insolation and associated feedbacks on temperature changes, which warrant closer attention in future climate modelling." @default.
- W4295113599 created "2022-09-10" @default.
- W4295113599 creator A5011276883 @default.
- W4295113599 creator A5013728584 @default.
- W4295113599 creator A5016663247 @default.
- W4295113599 creator A5026996153 @default.
- W4295113599 creator A5032558947 @default.
- W4295113599 creator A5047401798 @default.
- W4295113599 creator A5057044716 @default.
- W4295113599 creator A5076510971 @default.
- W4295113599 creator A5077155742 @default.
- W4295113599 date "2022-09-10" @default.
- W4295113599 modified "2023-10-14" @default.
- W4295113599 title "Holocene seasonal temperature evolution and spatial variability over the Northern Hemisphere landmass" @default.
- W4295113599 cites W1789796658 @default.
- W4295113599 cites W1867005924 @default.
- W4295113599 cites W1971261222 @default.
- W4295113599 cites W1977595786 @default.
- W4295113599 cites W1978863001 @default.
- W4295113599 cites W1978912552 @default.
- W4295113599 cites W2001715338 @default.
- W4295113599 cites W2003501861 @default.
- W4295113599 cites W2009503337 @default.
- W4295113599 cites W2012592445 @default.
- W4295113599 cites W2013878295 @default.
- W4295113599 cites W2017290357 @default.
- W4295113599 cites W2020232508 @default.
- W4295113599 cites W2025145183 @default.
- W4295113599 cites W2030660905 @default.
- W4295113599 cites W2043842533 @default.
- W4295113599 cites W2051671961 @default.
- W4295113599 cites W2057286384 @default.
- W4295113599 cites W2059175769 @default.
- W4295113599 cites W2059845258 @default.
- W4295113599 cites W2085482846 @default.
- W4295113599 cites W2095092516 @default.
- W4295113599 cites W2099358694 @default.
- W4295113599 cites W2102746137 @default.
- W4295113599 cites W2103983252 @default.
- W4295113599 cites W2107691545 @default.
- W4295113599 cites W2111308529 @default.
- W4295113599 cites W2112617203 @default.
- W4295113599 cites W2114683154 @default.
- W4295113599 cites W2114832130 @default.
- W4295113599 cites W2116644098 @default.
- W4295113599 cites W2129523241 @default.
- W4295113599 cites W2132106900 @default.
- W4295113599 cites W2135916824 @default.
- W4295113599 cites W2139199775 @default.
- W4295113599 cites W2139857660 @default.
- W4295113599 cites W2142644033 @default.
- W4295113599 cites W2150352749 @default.
- W4295113599 cites W2150844611 @default.
- W4295113599 cites W2156208893 @default.
- W4295113599 cites W2163409669 @default.
- W4295113599 cites W2168517632 @default.
- W4295113599 cites W2170402872 @default.
- W4295113599 cites W2171420618 @default.
- W4295113599 cites W2182526330 @default.
- W4295113599 cites W2280042168 @default.
- W4295113599 cites W2341326188 @default.
- W4295113599 cites W2521993234 @default.
- W4295113599 cites W2564016286 @default.
- W4295113599 cites W2587240583 @default.
- W4295113599 cites W2605968767 @default.
- W4295113599 cites W2618061159 @default.
- W4295113599 cites W2621383805 @default.
- W4295113599 cites W2622037578 @default.
- W4295113599 cites W2785210185 @default.
- W4295113599 cites W2786514163 @default.
- W4295113599 cites W2792523942 @default.
- W4295113599 cites W2793387090 @default.
- W4295113599 cites W2801170423 @default.
- W4295113599 cites W2898148723 @default.
- W4295113599 cites W2900605668 @default.
- W4295113599 cites W2901082478 @default.
- W4295113599 cites W2924516531 @default.
- W4295113599 cites W2947408052 @default.
- W4295113599 cites W2948226965 @default.
- W4295113599 cites W2948550777 @default.
- W4295113599 cites W2972562165 @default.
- W4295113599 cites W2984135768 @default.
- W4295113599 cites W2984514134 @default.
- W4295113599 cites W2994905779 @default.
- W4295113599 cites W2999331770 @default.
- W4295113599 cites W3013089870 @default.
- W4295113599 cites W3013517662 @default.
- W4295113599 cites W3015391807 @default.
- W4295113599 cites W3019172449 @default.
- W4295113599 cites W3043108592 @default.
- W4295113599 cites W3087364100 @default.
- W4295113599 cites W3090841701 @default.
- W4295113599 cites W3093091979 @default.
- W4295113599 cites W3123157889 @default.
- W4295113599 cites W3145323572 @default.
- W4295113599 cites W3182406209 @default.
- W4295113599 cites W3200799064 @default.
- W4295113599 cites W3201897249 @default.
- W4295113599 cites W3216633077 @default.
- W4295113599 cites W4213456692 @default.