High-Pressure Systems Favor Sea-Breeze Convection Over Southeastern Texas (IMAGE)
Caption
Composite of geopotential heights [m] (contours) and anomalies (colors) at 700 Hectopascal (hPa) of air pressure for each SOM node. These nodes help unpack how high- and low-pressure systems and other climate factors contribute to Texas rainstorms.
Credit
Image courtesy of Wang, Die, Brookhaven National Laboratory
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Image courtesy of Wang, Die, Brookhaven National Laboratory
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Original content