CO 2 in Arctic snow cover: landscape form, in‐pack gas concentration gradients, and the implications for the estimation of gaseous fluxes-Reference-Cited by-同舟云学术

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CO 2 in Arctic snow cover: landscape form, in‐pack gas concentration gradients, and the implications for the estimation of gaseous fluxes

Published:1999-12-15 Issue:18 Volume:13 Page:2977-2989
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Jones H. G.¹,Pomeroy J. W.²,Davies T. D.³,Tranter M.⁴,Marsh P.²

Affiliation:

1. INRS‐Eau, Ste‐Foy, Quebec, G1V 4C7, Canada

2. National Hydrology Research Centre, Saskatoon, Saskatchewan, S7N 3H5, Canada

3. School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, United Kingdom

4. School of Geographical Sciences, University of Bristol, Bristol, BS8 1SS, United Kingdom

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/%28SICI%291099-1085%2819991230%2913%3A18%3C2977%3A%3AAID-HYP12%3E3.0.CO%3B2-%23

Reference44 articles.

1. Firn Properties Affecting Gas Exchange at Summit, Greenland: Ventilation Possibilities

2. Structure and wind transport of seasonal snow on the Arctic slope of Alaska

3. Solar-heating rates and temperature profiles in Antarctic snow and ice

4. A three-dimensional theory of wind pumping

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4. The Spatial–Spectral–Environmental Extraction Endmember Algorithm and Application in the MODIS Fractional Snow Cover Retrieval;Remote Sensing;2020-11-11

5. Organic bromine compounds produced in sea ice in Antarctic winter;Nature Communications;2018-12

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