Cold springs in permafrost on Earth and Mars

occur in a region with a mean annual air temperature of 15C and flow through continuous permafrost 600 m thick. The spring water is a low-temperature (up to 6C) brine that maintains constant discharge temperatures and flow rates throughout the year. Here we report on observations of temperature and...

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Bibliographic Details
Main Authors: Dale T. Andersen, Wayne H. Pollard, Christopher P. Mckay, Jennifer Heldmann
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2002
Subjects:
hydrology
KEYWORDS
Arctic
permafrost
springs
astrobiology
Mars
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.486.5866
http://daleandersen.seti.org/Dale_Andersen/Science_articles_files/Andersen et al. 2002.pdf
Description
Summary:occur in a region with a mean annual air temperature of 15C and flow through continuous permafrost 600 m thick. The spring water is a low-temperature (up to 6C) brine that maintains constant discharge temperatures and flow rates throughout the year. Here we report on observations of temperature and discharge rate of these springs and develop a combined flow and thermal model of the subsurface flow using the measured geothermal gradient. We also consider the implications these springs have for the search for similar environments, past or present, on Mars. INDEX

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