Call number:
ZSP-201-82/26
In:
CRREL Report, 82-26
Description / Table of Contents:
The Caribou-Poker Creeks Research Watershed is a small (101.5-sq km) drainage basin located 48 km northwest of Fairbanks, Alaska. Elevations within the watershed range from 210 to 826 m, and approximately 28% of its area is underlain by permafrost. Climatic differences between the watershed and Fairbanks are primarily due to the higher elevation of the watershed. Generally the watershed climatic sites are warmer in winter and cooler in summer than Fairbanks. Within the watershed the greatest temperature contrasts exist in winter, when the valley-bottom sites are beneath the regional air temperature inversion, and the higher sites are above it. From May through September the total precipitation averages 270 mm, 1.47 times that received at Fairbanks. The annual precipitation is about 1.7 times that of Fairbanks. The historical precipitation record at Fairbanks indicates that summer precipitation was below the long-term normal in eight of the eleven years of watershed measurements (1969-1980); no climatic extremes occurred during this period. An analysis of annual streamflow data showed an inconsistency of baseflow recessions from year to year. The runoff-rainfall ratio for individual summer storms averaged 0.35 for Caribou Creek. Comparisons of spot discharge measurements of predominantly permafrost and non-permafrost subwatersheds showed that permafrost-dominated watersheds have a much flashier response to precipitation than non-permafrost watersheds. A comparison of the annual flow distribution of the watershed indicated that Caribou Creek has lower summer and higher winter discharges per unit area than the Chena or Salcha Rivers.
Type of Medium:
Series available for loan
Pages:
42 Seiten
,
Illustrationen
Series Statement:
CRREL Report 82-26
URL:
https://apps.dtic.mil/docs/citations/ADA122402
URL:
https://hdl.handle.net/11681/9369
Language:
English
Note:
CONTENTS
Abstract
Preface
Introduction
Setting
Geology and soils
Vegetation
Climate
Air temperature
Precipitation
Hydrology
Annual and monthly runoff
Individual storms
Baseflow recessions
Spatial flow variability
Temporal flow variability
Summary and conclusions
Literature cited
Appendix A: Station histories
Location:
AWI Archive
Branch Library:
AWI Library
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