R Zhang, R Sutton, G Danabasoglu… - Reviews of …, 2019 - Wiley Online Library
By synthesizing recent studies employing a wide range of approaches (modern observations, paleo reconstructions, and climate model simulations), this paper provides a …
L Landrum, MM Holland - Nature Climate Change, 2020 - nature.com
The Arctic is rapidly warming and experiencing tremendous changes in sea ice, ocean and terrestrial regions. Lack of long-term scientific observations makes it difficult to assess …
Polar amplification–the phenomenon where external radiative forcing produces a larger change in surface temperature at high latitudes than the global average–is a key aspect of …
SL Danielson, O Ahkinga, C Ashjian, E Basyuk… - Deep Sea Research …, 2020 - Elsevier
A temperature and salinity hydrographic profile climatology is assembled, evaluated for data quality, and analyzed to assess changes of the Bering and Chukchi Sea continental shelves …
The most pronounced warming in the historical global climate record prior to the recent warming occurred over the first half of the 20th century and is known as the Early Twentieth …
Near-term climate predictions—which operate on annual to decadal timescales—offer benefits for climate adaptation and resilience, and are thus important for society. Although …
M Fang, X Li, HW Chen, D Chen - Nature Communications, 2022 - nature.com
Enhanced warming in the Arctic (Arctic amplification, AA) in the last decades has been linked to several factors including sea ice and the Atlantic Multidecadal Oscillation (AMO) …
Z Zhang, X Sun, XQ Yang - Journal of Climate, 2018 - journals.ametsoc.org
Understanding the Interdecadal Variability of East Asian Summer Monsoon Precipitation: Joint Influence of Three Oceanic Signals in: Journal of Climate Volume 31 Issue 14 (2018) …
G Lohmann, M Butzin, N Eissner, X Shi… - Paleoceanography …, 2020 - Wiley Online Library
The past provides evidence of abrupt climate shifts and changes in the frequency of climate and weather extremes. We explore the nonlinear response to orbital forcing and then …