Synoptic cryosphere-atmosphere interactions in the northern hemisphere from DMSP image analysis

A. M. Carleton

doi:10.1080/01431168508948437

Synoptic cryosphere-atmosphere interactions in the northern hemisphere from DMSP image analysis

A. M. Carleton

Geography

Research output: Contribution to journal › Article › peer-review

15 Scopus citations

Abstract

A climatology of Northern Hemisphere cyclonic cloud vortices is developed from high-resolution Defense Meteorological Satellite Program (DMSP) infrared imagery for mid-season months. The technique which is described involves pattern recognition using a detailed vortex classification system. Variations in hemispheric frequencies of successive vortex types are dominantly seasonal rather than latitudinal and imply a close association with surface (mainly cryosphere) variations. More extensive sea ice or snow cover in April and January is associated with increased cyclogenesis, indicating enhanced surface-atmosphere feedback. A significant relationship exists between cloud- vortex variations and the sea ice boundary, but not with the continental snowline.

Original language	English (US)
Pages (from-to)	239-261
Number of pages	23
Journal	International Journal of Remote Sensing
Volume	6
Issue number	1
DOIs	https://doi.org/10.1080/01431168508948437
State	Published - Jan 1985

All Science Journal Classification (ASJC) codes

Earth and Planetary Sciences(all)

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10.1080/01431168508948437

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title = "Synoptic cryosphere-atmosphere interactions in the northern hemisphere from DMSP image analysis",

abstract = "A climatology of Northern Hemisphere cyclonic cloud vortices is developed from high-resolution Defense Meteorological Satellite Program (DMSP) infrared imagery for mid-season months. The technique which is described involves pattern recognition using a detailed vortex classification system. Variations in hemispheric frequencies of successive vortex types are dominantly seasonal rather than latitudinal and imply a close association with surface (mainly cryosphere) variations. More extensive sea ice or snow cover in April and January is associated with increased cyclogenesis, indicating enhanced surface-atmosphere feedback. A significant relationship exists between cloud- vortex variations and the sea ice boundary, but not with the continental snowline.",

author = "Carleton, {A. M.}",

note = "Funding Information: Acknowledgments This research was supported by a National Science Foundation, Division of . Polar Programs, grant (NSF DPP 7920853) to Drs. Roger Barry (CIRES) and H. J. Zwally (NASA), and by a National Aeronautics and Space Administration Climate Research Program grant NAG-5-l42 to Dr. Barry. The DMSP imagery was made available through World Data Center A for Glaciology, University of Colorado, Boulder. I am grateful to Dr. Barry for comments on an initial version of this paper.",

year = "1985",

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doi = "10.1080/01431168508948437",

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AU - Carleton, A. M.

N1 - Funding Information: Acknowledgments This research was supported by a National Science Foundation, Division of . Polar Programs, grant (NSF DPP 7920853) to Drs. Roger Barry (CIRES) and H. J. Zwally (NASA), and by a National Aeronautics and Space Administration Climate Research Program grant NAG-5-l42 to Dr. Barry. The DMSP imagery was made available through World Data Center A for Glaciology, University of Colorado, Boulder. I am grateful to Dr. Barry for comments on an initial version of this paper.

PY - 1985/1

Y1 - 1985/1

N2 - A climatology of Northern Hemisphere cyclonic cloud vortices is developed from high-resolution Defense Meteorological Satellite Program (DMSP) infrared imagery for mid-season months. The technique which is described involves pattern recognition using a detailed vortex classification system. Variations in hemispheric frequencies of successive vortex types are dominantly seasonal rather than latitudinal and imply a close association with surface (mainly cryosphere) variations. More extensive sea ice or snow cover in April and January is associated with increased cyclogenesis, indicating enhanced surface-atmosphere feedback. A significant relationship exists between cloud- vortex variations and the sea ice boundary, but not with the continental snowline.

AB - A climatology of Northern Hemisphere cyclonic cloud vortices is developed from high-resolution Defense Meteorological Satellite Program (DMSP) infrared imagery for mid-season months. The technique which is described involves pattern recognition using a detailed vortex classification system. Variations in hemispheric frequencies of successive vortex types are dominantly seasonal rather than latitudinal and imply a close association with surface (mainly cryosphere) variations. More extensive sea ice or snow cover in April and January is associated with increased cyclogenesis, indicating enhanced surface-atmosphere feedback. A significant relationship exists between cloud- vortex variations and the sea ice boundary, but not with the continental snowline.

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Synoptic cryosphere-atmosphere interactions in the northern hemisphere from DMSP image analysis

Abstract

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