Correspondence Among Mid‐Latitude Glacier Equilibrium Line Altitudes, Atmospheric Temperatures, and Westerly Wind Fields

Author:

Audet Alexander C.12ORCID,Putnam Aaron E.1,Russell Joellen L.3ORCID,Lorrey Andrew4ORCID,Mackintosh Andrew5,Anderson Brian6,Denton George H.1

Affiliation:

1. School of Earth and Climate Sciences and Climate Change Institute University of Maine ME Orono USA

2. Department of Geography College of Science University of Nevada Reno Reno NV USA

3. Department of Geosciences University of Arizona AZ Tucson USA

4. National Institute of Water & Atmospheric Research Ltd Auckland New Zealand

5. Securing Antarctica’s Environmental Future, School of Earth, Atmosphere and Environment Monash University VIC Clayton Australia

6. Antarctic Research Centre Victoria University of Wellington Wellington New Zealand

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference70 articles.

1. Temperature change is the major driver of late-glacial and Holocene glacier fluctuations in New Zealand

2. Climate sensitivity of a high-precipitation glacier in New Zealand

3. Arctic Oscillation. (2020).Arctic oscillation[Dataset].Climate Prediction Center. Retrieved fromhttps://www.cpc.ncep.noaa.gov/products/precip/CWlink/daily_ao_index/ao.shtml

4. Atlantic Multidecadal Oscillation. (2020).Atlantic multidecadal oscillation index (AMO)[Dataset].NOAA Physical Sciences Laboratory. Retrieved fromhttps://psl.noaa.gov/data/timeseries/AMO/

5. Audet A. Putnam A. E. Russell J. Lorrey A. &Denton G. H.(2022).Correlation of glacier ELA/snowlines & temperature station data with ERA5 temperature and wind speed 1979 to 2017[Dataset].PANGAEA.https://doi.org/10.1594/PANGAEA.948198

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