Fig. 5: Analysis of geopotential height and wind responses. | npj Climate and Atmospheric Science

Fig. 5: Analysis of geopotential height and wind responses.

From: The role of Arctic sea ice loss in the interdecadal trends of the East Asian summer monsoon in a warming climate

Fig. 5

The 200 hPa latitudinal deviation field of geopotential height (shading, units: m) and wind (vector, units: m s−1) responses to ALL in June (a) and July (c). The 850 hPa latitudinal deviation field of geopotential height (shading, units: m) and wind (vector, units: m s−1) responses to ALL in June (b) and July (d). The 200 hPa latitudinal deviation field of geopotential height (shading, units: m) and wind (vector, units: m s-1) responses to SSTR in June (e) and July (g). The 850 hPa latitudinal deviation field of geopotential height (shading, units: m) and wind (vector, units: m s-1) responses to SSTR in June (f) and July (h). The 200 hPa geopotential height (shading, units: m) and wind (vector, units: m s-1) responses to ARC in June (i) and July (k). The 850 hPa geopotential height (shading, units: m) and wind (vector, units: m s-1) responses to ARC in June (j) and July (l). Stippling and red vectors indicate where the multimodel ensemble mean response is significant (90% confidence).

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