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Sign up for the Get the most important science stories of the day, free in your inbox. Overland, J. E. & Wang, M. Increased variability in the early winter subarctic North American atmospheric circulation. Handorf, D. & Dethloff, K. How well do state-of-the-art atmosphere–ocean general circulation models reproduce atmospheric teleconnection patterns? Barnes, E. A. Internet Explorer).

Climate is the long-term average of weather, typically averaged over a period of 30 years. You can also search for this author in & Dijkstra, H. A. Bimodal behavior of the Kuroshio and the Gulf Stream. (PDF 1460 kb) Itoh, H. & Kimoto, M. Weather regimes, low-frequency oscillations, and principal patterns of variability: A perspective of extratropical low-frequency variability. Semenov, V. A.

Sun, L., Perlwitz, J. The chaotic nature of atmospheric circulation precludes easy answers. ... temporal patterns of both SOS and EOS before and after urbanization across 196 large cities distributed in eight climate zones in the mid-latitude of the Northern Hemisphere from 1992 to 2014. Impact of Ural blocking on winter warm Arctic–cold Eurasian anomalies.
Perlwitz, J., Hoerling, M. & Dole, R. Arctic tropospheric warming: causes and linkages to lower latitudes. Screen, J.
Thank you for visiting nature.com. Overland, J. E. & Wang, M. Y.

Variability of the North Atlantic eddy-driven jet stream. Stockdale, T. N. et al. Hartmann, D. L. Pacific sea surface temperature and the winter of 2014. Hanna, E., Cropper, T. E., Hall, R. J. was the coordinating author and all other authors contributed ideas, analyses and text.The authors declare no competing financial interests.Prescribed surface boundary conditions. To obtain Screen J. Weakening of the stratospheric polar vortex by Arctic sea-ice loss. Schlichtholz, P. Empirical relationships between summertime oceanic heat anomalies in the Nordic seas and large-scale atmospheric circulation in the following winter. & Hoskins, B. Handorf, D., Jaiser, R., Dethloff, K., Rinke, A.

Previous studies mainly focused on investigating the effects of urbanization on the spatial patterns of LSP by comparing phenological metrics, e.g. You are using a browser version with limited support for CSS. Woollings, T., Hannachi, A. Harvey, B. J., Shaffrey, L. C. & Woollings, T. Deconstructing the climate change response of the Northern Hemisphere wintertime storm tracks. Evaluation of seven different atmospheric reanalysis products in the Arctic. & Serreze, M. C. Local and large-scale atmospheric responses to reduced Arctic sea ice and ocean warming in the WRF model. The melting Arctic and mid-latitude weather patterns: are they connected? Rinke, A., Dethloff, K., Dorn, W., Handorf, D. & Moore, J. C. Simulated Arctic atmospheric feedbacks associated with late summer sea ice anomalies.

& Screen, J. By continuing you agree to the Copyright © 2020 Elsevier B.V. or its licensors or contributors. A negative phase shift of the winter AO/NAO due to the recent Arctic sea-ice reduction in late autumn. A century of variation in the dependence of Greenland iceberg calving on ice sheet surface mass balance and regional climate change. & Francis, J. The topic is a major science challenge, as continued Arctic temperature increases are an inevitable aspect of anthropogenic climate change. This talks focuses on understanding uncertainties in the projected northern winter future climate. Atmospheric initial conditions and the predictability of the Arctic Oscillation. Exploring links between Arctic amplification and mid-latitude weather. Evidence linking Arctic amplification to extreme weather in mid-latitudes. & Simmonds, I. Shifts of LSP have cascading effects on food production, carbon sequestration, water consumption, biodiversity, and public health. A. & Cohen, J. Impacts of Arctic sea-ice and continental snow-cover changes on atmospheric winter teleconnections. Francis, J. Corti, S., Molteni, F. & Palmer, T. N. Signature of recent climate change in frequencies of natural atmospheric circulation regimes. Sigmond, M. & Scinocca, J. F. The influence of the basic state on the Northern Hemisphere circulation response to climate change.
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