Caitlyn Florentine, Ph.D.
I research the cryosphere (frozen Earth) using an approach that integrates in situ data collected in the field, remotely-sensed data, and simple numerical models. My main research interest is in quantitative glaciology, especially regarding the physics of glacier flow and glacier-climate relationships.
Research Interests
The snow and ice systems I study are intimately linked to the lithosphere, biosphere, and hydrosphere. My research therefore often overlaps with avalanche science, geology, geomorphology, ecology, and hydrology in alpine and Arctic settings. Currently I work with the U.S. Geological Survey Glaciers and Climate Project and the Climate Change in Mountain Ecosystems group.
Education and Certifications
Ph.D. Geosciences. 2018. University of Montana, Missoula, Montana
M.S. Earth Sciences. 2011. Montana State University, Bozeman, Montana
B.A. Geology. 2007. Colorado College, Colorado Springs, Colorado
Science and Products
Wolverine Glacier
Mass Balance Summary
Mass Balance Methods - Measuring Glacier Change
Glaciers—Understanding Climate Drivers
Assessing the Vulnerability of Alaska’s Glaciers in a Changing Climate
Time Series of Glacier Retreat
Raw Ground Penetrating Radar Data on North American Glaciers
Glaciers and ice caps outside Greenland
Observing glacier elevation changes from spaceborne optical and radar sensors – an inter-comparison experiment using ASTER and TanDEM-X data
Brief communication: Recent estimates of glacier mass loss for western North America from laser altimetry
How to handle glacier area change in geodetic mass balance
Historical Structure from Motion (HSfM): Automated processing of historical aerial photographs for long-term topographic change analysis
Uncertainty of ICESat-2 ATL06- and ATL08-derived snow depths for glacierized and vegetated mountain regions
Non-USGS Publications**
reflects the present-day internal flow field in the ablation zone of western
Greenland Ice Sheet. Frontiers in Earth Science 6, 1-11. https://doi.org/10.3389/feart.2018.00044
and internal deformation at Lone Peak rock glacier, Big Sky, Montana, USA.
Journal of Glaciology 60, 453-462. https://doi.org/10.3189/2014JoG13J160
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
Wolverine Glacier
Mass Balance Summary
Mass Balance Methods - Measuring Glacier Change
Glaciers—Understanding Climate Drivers
Assessing the Vulnerability of Alaska’s Glaciers in a Changing Climate
Time Series of Glacier Retreat
Raw Ground Penetrating Radar Data on North American Glaciers
Glaciers and ice caps outside Greenland
Observing glacier elevation changes from spaceborne optical and radar sensors – an inter-comparison experiment using ASTER and TanDEM-X data
Brief communication: Recent estimates of glacier mass loss for western North America from laser altimetry
How to handle glacier area change in geodetic mass balance
Historical Structure from Motion (HSfM): Automated processing of historical aerial photographs for long-term topographic change analysis
Uncertainty of ICESat-2 ATL06- and ATL08-derived snow depths for glacierized and vegetated mountain regions
Non-USGS Publications**
reflects the present-day internal flow field in the ablation zone of western
Greenland Ice Sheet. Frontiers in Earth Science 6, 1-11. https://doi.org/10.3389/feart.2018.00044
and internal deformation at Lone Peak rock glacier, Big Sky, Montana, USA.
Journal of Glaciology 60, 453-462. https://doi.org/10.3189/2014JoG13J160
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.