Cold air advection in the Bering Sea
![](https://cimss.ssec.wisc.edu/satellite-blog/wp-content/uploads/sites/5/2021/01/ber_dnb-20210106_010004.png)
GOES-17 (GOES-West) “Red” Visible (0.64 µm) images (above) displayed cloud streets across the Bering Sea — cloud features that frequently occur in areas with a strong flow of cold air over warmer water. This northerly flow of cold air across the Bering Sea was due to a strong pressure gradient between... Read More