Gulkana Glacier area change, from 1957 - 2021. Gulkana Glacier is located along the south flank of the eastern Alaska Range.
Christopher McNeil
My research focuses on understanding the ways glaciers change in area, volume, and mass at basin-to-regional spatial scales, and how those changes impact local ecosystems and global sea level.
My projects synthesize both in-situ and remotely sensed data of glacier change ranging from Alaska to the Contiguous United States. Research includes reanalyzing the longest in-situ records of glacier change in North America to homogenize the U.S. Geological Survey’s traditional glacier monitoring network. Additionally, my research extends to understanding the factors (hypsometry, snow accumulation patterns, energy balances, dynamic processes) that drive variable glacier change rates at the mountain range scale. This work leverages historical aerial imagery, high resolution commercial satellite imagery, open-source computing platforms, geospatial analyses, and high-performance computing.
Science and Products
Glaciers and Climate Project
Firn Density and Stratigraphy Observations from USGS Benchmark Glaciers
USGS Benchmark Glacier Mass Balance and Project Data
Point Raw Glaciological Data: Ablation Stake, Snow Pit, and Probed Snow Depth Data on USGS Benchmark Glaciers
Geodetic Data for USGS Benchmark Glaciers: Orthophotos, Digital Elevation Models, Glacier Boundaries and Surveyed Positions
Glacier-Wide Mass Balance and Compiled Data Inputs: USGS Benchmark Glaciers
Glacier-Wide Mass Balance and Compiled Data Inputs: Juneau Icefield Glaciers
Raw Ground Penetrating Radar Data on North American Glaciers
Geodetic Data for Juneau Icefield Glaciers: Orthophotos, Digital Elevation Models, and Glacier Boundaries
Weather Station Data on the Juneau Icefield
Raw Ground Penetrating Radar Data, Valdez Glacier, Alaska; 2013
Raw Ground Penetrating Radar Data,Taku Glacier, Alaska; 2013
Raw Ground Penetrating Radar Data, Scott Glacier, Alaska; 2013
Gulkana Glacier area change, from 1957 - 2021. Gulkana Glacier is located along the south flank of the eastern Alaska Range.
2019 Juneau Icefield Research Program (JIRP) students during a four day and 83 kilometers ski traverse across Taku Glacier, carrying all their food, water, clothing, tents, and science gear as they help measure the mass balance along the way.
2019 Juneau Icefield Research Program (JIRP) students during a four day and 83 kilometers ski traverse across Taku Glacier, carrying all their food, water, clothing, tents, and science gear as they help measure the mass balance along the way.
Students Stacey Edmonsond (left) and Audrey Erickson (right) of the Juneau Icefield Research Program, measuring glacier mass balance at the flow divide of Taku and Mendenhall glaciers during the summer of 2019
Students Stacey Edmonsond (left) and Audrey Erickson (right) of the Juneau Icefield Research Program, measuring glacier mass balance at the flow divide of Taku and Mendenhall glaciers during the summer of 2019
Image of the Taku towers, among the Taku Range at Taku Glacier during the summer of 2019
Image of the Taku towers, among the Taku Range at Taku Glacier during the summer of 2019
Satellite image of Taku Glacier in October 1, 2018. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image. Citation: McNeil, C. J., and Baker, E.
Satellite image of Taku Glacier in October 1, 2018. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image. Citation: McNeil, C. J., and Baker, E.
Satellite image of Taku Glacier in October 1, 2018. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image.
Satellite image of Taku Glacier in October 1, 2018. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image.
Aerial image of Taku Glacier in 1948. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image. Citation: McNeil, C. J., and Baker, E. H., 2019, Geodetic data for Juneau Icefield Glaciers: orthophotos, digital elevation models, and glacier boundaries (ver 1.0, August, 2019): U.S.
Aerial image of Taku Glacier in 1948. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image. Citation: McNeil, C. J., and Baker, E. H., 2019, Geodetic data for Juneau Icefield Glaciers: orthophotos, digital elevation models, and glacier boundaries (ver 1.0, August, 2019): U.S.
GNSS reflectometry from low-cost sensors for continuous in situ contemporaneous glacier mass balance and flux divergence
Direct measurements of firn-density evolution from 2016 to 2022 at Wolverine Glacier, Alaska
Accelerating glacier volume loss on Juneau Icefield driven by hypsometry and melt-accelerating feedbacks
How to handle glacier area change in geodetic mass balance
Inventory of glaciers and perennial snowfields of the conterminous USA
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
Beyond glacier-wide mass balances: Parsing seasonal elevation change into spatially resolved patterns of accumulation and ablation at Wolverine Glacier, Alaska
Topographic controls on ice flow and recession for Juneau Icefield (Alaska/British Columbia)
The imminent calving retreat of Taku Glacier
Explaining mass balance and retreat dichotomies at Taku and Lemon Creek Glaciers, Alaska
Reanalysis of the U.S. Geological Survey Benchmark Glaciers: Long-term insight into climate forcing of glacier mass balance
Non-USGS Publications**
**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
Glaciers and Climate Project
Firn Density and Stratigraphy Observations from USGS Benchmark Glaciers
USGS Benchmark Glacier Mass Balance and Project Data
Point Raw Glaciological Data: Ablation Stake, Snow Pit, and Probed Snow Depth Data on USGS Benchmark Glaciers
Geodetic Data for USGS Benchmark Glaciers: Orthophotos, Digital Elevation Models, Glacier Boundaries and Surveyed Positions
Glacier-Wide Mass Balance and Compiled Data Inputs: USGS Benchmark Glaciers
Glacier-Wide Mass Balance and Compiled Data Inputs: Juneau Icefield Glaciers
Raw Ground Penetrating Radar Data on North American Glaciers
Geodetic Data for Juneau Icefield Glaciers: Orthophotos, Digital Elevation Models, and Glacier Boundaries
Weather Station Data on the Juneau Icefield
Raw Ground Penetrating Radar Data, Valdez Glacier, Alaska; 2013
Raw Ground Penetrating Radar Data,Taku Glacier, Alaska; 2013
Raw Ground Penetrating Radar Data, Scott Glacier, Alaska; 2013
Gulkana Glacier area change, from 1957 - 2021. Gulkana Glacier is located along the south flank of the eastern Alaska Range.
Gulkana Glacier area change, from 1957 - 2021. Gulkana Glacier is located along the south flank of the eastern Alaska Range.
2019 Juneau Icefield Research Program (JIRP) students during a four day and 83 kilometers ski traverse across Taku Glacier, carrying all their food, water, clothing, tents, and science gear as they help measure the mass balance along the way.
2019 Juneau Icefield Research Program (JIRP) students during a four day and 83 kilometers ski traverse across Taku Glacier, carrying all their food, water, clothing, tents, and science gear as they help measure the mass balance along the way.
Students Stacey Edmonsond (left) and Audrey Erickson (right) of the Juneau Icefield Research Program, measuring glacier mass balance at the flow divide of Taku and Mendenhall glaciers during the summer of 2019
Students Stacey Edmonsond (left) and Audrey Erickson (right) of the Juneau Icefield Research Program, measuring glacier mass balance at the flow divide of Taku and Mendenhall glaciers during the summer of 2019
Image of the Taku towers, among the Taku Range at Taku Glacier during the summer of 2019
Image of the Taku towers, among the Taku Range at Taku Glacier during the summer of 2019
Satellite image of Taku Glacier in October 1, 2018. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image. Citation: McNeil, C. J., and Baker, E.
Satellite image of Taku Glacier in October 1, 2018. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image. Citation: McNeil, C. J., and Baker, E.
Satellite image of Taku Glacier in October 1, 2018. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image.
Satellite image of Taku Glacier in October 1, 2018. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image.
Aerial image of Taku Glacier in 1948. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image. Citation: McNeil, C. J., and Baker, E. H., 2019, Geodetic data for Juneau Icefield Glaciers: orthophotos, digital elevation models, and glacier boundaries (ver 1.0, August, 2019): U.S.
Aerial image of Taku Glacier in 1948. The Norris Glacier can be seen on the lower left hand corner and the Hole-in-the-Wall Glacier in the upper center portion of the image. Citation: McNeil, C. J., and Baker, E. H., 2019, Geodetic data for Juneau Icefield Glaciers: orthophotos, digital elevation models, and glacier boundaries (ver 1.0, August, 2019): U.S.
GNSS reflectometry from low-cost sensors for continuous in situ contemporaneous glacier mass balance and flux divergence
Direct measurements of firn-density evolution from 2016 to 2022 at Wolverine Glacier, Alaska
Accelerating glacier volume loss on Juneau Icefield driven by hypsometry and melt-accelerating feedbacks
How to handle glacier area change in geodetic mass balance
Inventory of glaciers and perennial snowfields of the conterminous USA
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
Beyond glacier-wide mass balances: Parsing seasonal elevation change into spatially resolved patterns of accumulation and ablation at Wolverine Glacier, Alaska
Topographic controls on ice flow and recession for Juneau Icefield (Alaska/British Columbia)
The imminent calving retreat of Taku Glacier
Explaining mass balance and retreat dichotomies at Taku and Lemon Creek Glaciers, Alaska
Reanalysis of the U.S. Geological Survey Benchmark Glaciers: Long-term insight into climate forcing of glacier mass balance
Non-USGS Publications**
**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.