New Chapter IV-B-2 in CRC Press Entitled

INTRODUCTION RESOLUTION AND COVERAGE ISSUES i, Temporal and Spatial Resolution ii. Spatial Coverage DATA AND APPROACHES i. Wind-Driven Ice Motion and the Momentum Balance R ons . i Time-Series . Data and the CONCLUSIONS ACKNOWLEDGEMENTS BIBLIOGRAPHY TABLES FIGURES 1 a. INTRODUCTION difficulty in obs...

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Bibliographic Details
Main Authors: Oceanographic Applications Of, Mark R. Drinkwater
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: CRC Press 1995
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.17.5805
http://polar.jpl.nasa.gov/Publications/Drinkwater_IkedaBook_chp4_95.pdf
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Summary:INTRODUCTION RESOLUTION AND COVERAGE ISSUES i, Temporal and Spatial Resolution ii. Spatial Coverage DATA AND APPROACHES i. Wind-Driven Ice Motion and the Momentum Balance R ons . i Time-Series . Data and the CONCLUSIONS ACKNOWLEDGEMENTS BIBLIOGRAPHY TABLES FIGURES 1 a. INTRODUCTION difficulty in observing the polar sea-ice cover and its influence on the atmospheric and oceanic boundary layer is the ephemerality of active geophysical processes. Identifying of sea-ice formation, change and decay, is the key to successful measurement of these processes, Sea ice continuously adjusts to the ocean and atmosphere, and the magnitude or scale of corresponding changes is determined by the atmospheric and oceanographic forcing terms ranging spatially from meters to thousands of kilometers, and temporally from diurnal to Table indicates the spatial and temporal scales of key sea-ice variables of interest to sea-ice geophysicists and oceanographers. A conventional concern of hi