| Temperature & Sea Level Pressure -
The intensity of the storm is easily identified by the labeled isobars. Changes in temperature
can be seen by the color contours. The coldest air is located on the north and west side of the cyclone. The counterclockwise
airflow around the cyclone leads to a southward progression of cold air. Similarily, warm air is transported northward on the
eastern side of the cyclone as it moves west to east across the country.
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