Extended Data Fig. 6: Seasonal Maximum Covariance Analysis (MCA) between the 1000 hPa geopotential height (GPH) (Z1000) and precipitation of the study area, with the spatial patterns of the first mode of Z1000 and precipitation in the MCA for the study period (2005-2020). | Nature Geoscience

Extended Data Fig. 6: Seasonal Maximum Covariance Analysis (MCA) between the 1000 hPa geopotential height (GPH) (Z1000) and precipitation of the study area, with the spatial patterns of the first mode of Z1000 and precipitation in the MCA for the study period (2005-2020).

From: Sustained decrease in inland East Antarctic surface mass balance between 2005 and 2020

Extended Data Fig. 6: Seasonal Maximum Covariance Analysis (MCA) between the 1000 hPa geopotential height (GPH) (Z1000) and precipitation of the study area, with the spatial patterns of the first mode of Z1000 and precipitation in the MCA for the study period (2005-2020).The alternative text for this image may have been generated using AI.

a, SON b, DJF c, MAM and d, JJA. Areas of significance heterogeneous Pearson correlation (P < 0.05, two-sided) are shown within the yellow contours and marked with black dots. The red line indicates the study transect.

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