Fig. 10: Relatively consistent tropospheric responses but contrasting stratospheric responses are found between different PAMIP models in response to projected Arctic sea ice loss. | npj Climate and Atmospheric Science

Fig. 10: Relatively consistent tropospheric responses but contrasting stratospheric responses are found between different PAMIP models in response to projected Arctic sea ice loss.

From: Attributing climate and weather extremes to Northern Hemisphere sea ice and terrestrial snow: progress, challenges and ways forward

Fig. 10: Relatively consistent tropospheric responses but contrasting stratospheric responses are found between different PAMIP models in response to projected Arctic sea ice loss.

Zonally averaged DJF zonal wind response (ms−1) plotted as a function of latitude (°N) and height (pressure) for the ensemble mean of each of the models. The boxes show the regions used to compute the zonal wind response index. Stippling indicates where the ensemble mean response is significant (95% confidence interval). Contours show the climatological zonal mean winds (contour interval 5 ms−1 with negative contours dotted). This figure is taken from Smith et al. (2022), and as part of that article is licensed under a Creative Commons Attribution 4.0 International License: http://creativecommons.org/licenses/by/4.0/. From: https://www.nature.com/articles/s41467-022-28283-y.

Back to article page