Great Salt Lake effect snowfall, some notes and an example
-
-
-
Series:
Details
-
NOAA Program & Office:
-
Description:"A lake effect snowfall along the Wasatch Front is typically a post cold frontal event in which the duration of snowfall downwind of the lee shore is extended in cold, northwest flow. Where one would normally expect snowfall to end with the passage of the upper level trough, lake effect snows usually continue for several hours after that event"--Introduction.
-
Content Notes:David M. Carpenter.
Includes bibliographical references (page 16). -
Subjects:
-
Document Type:
-
Place as Subject:
-
Rights Information:Public Domain
-
Compliance:Library
-
Download URL:
-
File Type:
-
Collection(s):
-
Main Document Checksum:urn:sha256:2f7fdbe952b3e8be010756a6b18dbd74a8e8a16c0770ae6e847a31b216f5f00b
The NOAA IR serves as an archival repository of NOAA-published products including scientific findings, journal articles,
guidelines, recommendations, or other information authored or co-authored by NOAA or funded partners. As a repository, the
NOAA IR retains documents in their original published format to ensure public access to scientific information.
You May Also Like
COLLECTION
National Weather Service (NWS)