Some Observations of Alaskan Glacier Winds in Midsummer

ABSTRACT. Characteristics of glacier winds observed at midsummer on the Worthington and Castner glaciers are described. In each case there is a diurnal double maximum in windspeed, one slightly before sunrise and the other in the mid-afternoon. When a daytime glacier wind is absent at Castner a very...

Full description

Bibliographic Details
Main Authors: N A Streten, G Wendlerl
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1052.8185
http://pubs.aina.ucalgary.ca/arctic/Arctic21-2-98.pdf
id ftciteseerx:oai:CiteSeerX.psu:10.1.1.1052.8185
record_format openpolar
spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1052.8185 2023-05-15T14:19:47+02:00 Some Observations of Alaskan Glacier Winds in Midsummer N A Streten G Wendlerl The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1052.8185 http://pubs.aina.ucalgary.ca/arctic/Arctic21-2-98.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1052.8185 http://pubs.aina.ucalgary.ca/arctic/Arctic21-2-98.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic21-2-98.pdf text ftciteseerx 2020-04-12T00:17:12Z ABSTRACT. Characteristics of glacier winds observed at midsummer on the Worthington and Castner glaciers are described. In each case there is a diurnal double maximum in windspeed, one slightly before sunrise and the other in the mid-afternoon. When a daytime glacier wind is absent at Castner a very regular night downslope circulation is often observed. Text Arctic Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description ABSTRACT. Characteristics of glacier winds observed at midsummer on the Worthington and Castner glaciers are described. In each case there is a diurnal double maximum in windspeed, one slightly before sunrise and the other in the mid-afternoon. When a daytime glacier wind is absent at Castner a very regular night downslope circulation is often observed.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author N A Streten
G Wendlerl
spellingShingle N A Streten
G Wendlerl
Some Observations of Alaskan Glacier Winds in Midsummer
author_facet N A Streten
G Wendlerl
author_sort N A Streten
title Some Observations of Alaskan Glacier Winds in Midsummer
title_short Some Observations of Alaskan Glacier Winds in Midsummer
title_full Some Observations of Alaskan Glacier Winds in Midsummer
title_fullStr Some Observations of Alaskan Glacier Winds in Midsummer
title_full_unstemmed Some Observations of Alaskan Glacier Winds in Midsummer
title_sort some observations of alaskan glacier winds in midsummer
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1052.8185
http://pubs.aina.ucalgary.ca/arctic/Arctic21-2-98.pdf
genre Arctic
genre_facet Arctic
op_source http://pubs.aina.ucalgary.ca/arctic/Arctic21-2-98.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1052.8185
http://pubs.aina.ucalgary.ca/arctic/Arctic21-2-98.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
_version_ 1766291514418266112