Lemon Creek Glacier is located in the high-latitude maritime region of Alaska, at the southernmost tip of the Juneau Icefield. Glacier observations began at this site in 1953.
Return to Glaciers and Climate Project
Lemon Creek Glacier is located at the southernmost tip of the Juneau Icefield in Southeast Alaska, USA, approximately 6.5 km northeast of the city of Juneau. It is a subarctic alpine glacier in a maritime climate. The glacier flows northward from its accumulation zone and spans 900 m of elevation, from approximately 600 to 1500 m. Lemon Creek Glacier is in a 31.9 km2 basin and had an area of 9.7 km2 in 2018 (O'Neel et al, 2019).
In 1957/58, Lemon Creek Glacier was chosen as a representative glacier for the 1957/58 International Geophysical Year and it continues to serve as a reference glacier of the World Glacier Monitoring Service.
Lemon Creek Glacier is geographically situated between glaciers in the contiguous USA and those in mainland Alaska. This strategic location and existing long term data set prompted the USGS to align protocols and mass balance analysis with the other four USGS Benchmark Glaciers in 2013.
Research
Glacier mass balance
Mass balance measurements began at Lemon Creek Glacier in 1953, under the direction of the Juneau Icefield Research Program (JIRP). These data represent the second longest continuous annual record of mass balance in North America, consisting mostly of annual late-season accumulation observations. Around 1970 a network of four standard measurement sites were established across an elevation gradient and standard methods of mass balance measurement were implemented at snow pits and along ablation transects (Pelto and others, 2013). In 2013, additional measurements were added to complement the USGS Benchmark Glacier research protocol which includes two field visits per year to capture the range of mass balance (O’Neel, and others, 2019). These visits to measure and maintain stakes at the index sites are made each spring, at the onset of the melt season, and again in early autumn, near its completion. Density of the material gained or lost is measured with a snow-pit or core. By collecting data near the balance maxima and minima, direct measurements closely reflect maximum winter accumulation and the annual balances at each location.
Direct field measurements are combined with weather data and imagery analyses to calculate the seasonal and annual mass balance of each glacier. Access all the data here.
Meteorologic
Measurements of air temperature data have been collected at many permanent camp facilities and along the margins of Lemon Creek Glacier for use in mass balance calculations for the period of record 1990-2018. These data are available through the Alaska Science Center Data Repository for the following parameters:
- Temperature, air (1998 - present)
Gaps in data and challenges with instrumentation over the decades have also required the use of nonlocal meteorological data from the nearby Juneau Airport (ncdc.noaa.gov, Station ID: USW00025309) for mass balance calculations. The airport is located at sea-level, 13 km from the glacier. The data from the Juneau airport were used in the 2019 reanalysis and are available here.
Hydrologic
The Lemon Creek near Juneau stream gaging station, USGS station 15052000, is part of the USGS network of nearly 100 stations in Alaska. Data collection and analysis are conducted by standard techniques developed by the USGS. Daily values of discharge are available online and published annually in the USGS Water-Data report series. Water data back to 1948 exists of the USGS Lemon Creek Gaging Station web page.
Lemon Creek Gaging Station Data (USGS 15052000):
- Temperature, air (available 2019-08-18 to current)
- Temperature, water (available 2017-11-09 to current)
- Stream Discharge (available 2002-05-08 to current)
- Gage Height (available 2007-10-18 to current)
Location: Latitude: 58°23'30"N, Longitude: 134°25'15 NAD27, City And Borough Of Juneau, Alaska, Hydrologic Unit 19010301, Datum of gage: 204 m above NAVD88.
Drainage Area: 32 km2
Period of Record: August 1951 to current year (discharge data), Field/lab water quality data Oct 1948 to current year.
Previous Work
Because of its ease of access and its designation as a one of nine representative glaciers for the 1957/58 International Geophysical Year, Lemon Creek Glacier has been extensively studied over the decades. The data are reported to the World Glacier Monitoring Service (WGMS) annually. Field observations were initiated in 1953, under the direction of the Juneau Icefield Research Program (JIRP). Seasonal measurements and a consistent network of snowpit sites were added to the protocol in 2016 to align methodology with the other benchmark glaciers. Reanalysis of the five USGS Benchmark Glaciers (including Lemon Creek) was published by O’Neil et al (2019) and underscored the importance of using geodetic calibration to evaluate mass-balance trends based on the direct glacier measurements.
Glaciers and Climate Project
Additional Research Glaciers
Wolverine Glacier
Sperry Glacier
South Cascade Glacier
Gulkana Glacier
Mass Balance Summary
Mass Balance Methods - Measuring Glacier Change
Specialized meltwater biodiversity persists despite widespread deglaciation
Parsing complex terrain controls on mountain glacier response to climate forcing
Explaining mass balance and retreat dichotomies at Taku and Lemon Creek Glaciers, Alaska
Glacier retreat in Glacier National Park, Montana
Reanalysis of the U.S. Geological Survey Benchmark Glaciers: Long-term insight into climate forcing of glacier mass balance
Glacier recession since the Little Ice Age: Implications for water storage in a Rocky Mountain landscape
Interannual snow accumulation variability on glaciers derived from repeat spatially extensive ground-penetrating radar surveys
Local topography increasingly influences the mass balance of a retreating cirque glacier
Glacierized headwater streams as aquifer recharge corridors, subarctic Alaska
Snow and ice
Geometry, mass balance and thinning at Eklutna Glacier, Alaska: an altitude-mass-balance feedback with implications for water resources
Hypsometric control on glacier mass balance sensitivity in Alaska and northwest Canada
- Overview
Lemon Creek Glacier is located in the high-latitude maritime region of Alaska, at the southernmost tip of the Juneau Icefield. Glacier observations began at this site in 1953.
Return to Glaciers and Climate Project
Lemon Creek Glacier area change, 1948 - 2018 Lemon Creek Glacier is located at the southernmost tip of the Juneau Icefield in Southeast Alaska, USA, approximately 6.5 km northeast of the city of Juneau. It is a subarctic alpine glacier in a maritime climate. The glacier flows northward from its accumulation zone and spans 900 m of elevation, from approximately 600 to 1500 m. Lemon Creek Glacier is in a 31.9 km2 basin and had an area of 9.7 km2 in 2018 (O'Neel et al, 2019).
In 1957/58, Lemon Creek Glacier was chosen as a representative glacier for the 1957/58 International Geophysical Year and it continues to serve as a reference glacier of the World Glacier Monitoring Service.
Lemon Creek Glacier is geographically situated between glaciers in the contiguous USA and those in mainland Alaska. This strategic location and existing long term data set prompted the USGS to align protocols and mass balance analysis with the other four USGS Benchmark Glaciers in 2013.
Research
Glacier mass balance
Mass balance measurements began at Lemon Creek Glacier in 1953, under the direction of the Juneau Icefield Research Program (JIRP). These data represent the second longest continuous annual record of mass balance in North America, consisting mostly of annual late-season accumulation observations. Around 1970 a network of four standard measurement sites were established across an elevation gradient and standard methods of mass balance measurement were implemented at snow pits and along ablation transects (Pelto and others, 2013). In 2013, additional measurements were added to complement the USGS Benchmark Glacier research protocol which includes two field visits per year to capture the range of mass balance (O’Neel, and others, 2019). These visits to measure and maintain stakes at the index sites are made each spring, at the onset of the melt season, and again in early autumn, near its completion. Density of the material gained or lost is measured with a snow-pit or core. By collecting data near the balance maxima and minima, direct measurements closely reflect maximum winter accumulation and the annual balances at each location.
Direct field measurements are combined with weather data and imagery analyses to calculate the seasonal and annual mass balance of each glacier. Access all the data here.
Meteorologic
Researchers walk amid the glacial ice and crevasses left bare by summer melt on Lemon Creek Glacier, AK. Measurements of air temperature data have been collected at many permanent camp facilities and along the margins of Lemon Creek Glacier for use in mass balance calculations for the period of record 1990-2018. These data are available through the Alaska Science Center Data Repository for the following parameters:
- Temperature, air (1998 - present)
Gaps in data and challenges with instrumentation over the decades have also required the use of nonlocal meteorological data from the nearby Juneau Airport (ncdc.noaa.gov, Station ID: USW00025309) for mass balance calculations. The airport is located at sea-level, 13 km from the glacier. The data from the Juneau airport were used in the 2019 reanalysis and are available here.
Hydrologic
The Lemon Creek near Juneau stream gaging station, USGS station 15052000, is part of the USGS network of nearly 100 stations in Alaska. Data collection and analysis are conducted by standard techniques developed by the USGS. Daily values of discharge are available online and published annually in the USGS Water-Data report series. Water data back to 1948 exists of the USGS Lemon Creek Gaging Station web page.
Lemon Creek Gaging Station Data (USGS 15052000):
- Temperature, air (available 2019-08-18 to current)
- Temperature, water (available 2017-11-09 to current)
- Stream Discharge (available 2002-05-08 to current)
- Gage Height (available 2007-10-18 to current)
Location: Latitude: 58°23'30"N, Longitude: 134°25'15 NAD27, City And Borough Of Juneau, Alaska, Hydrologic Unit 19010301, Datum of gage: 204 m above NAVD88.
Drainage Area: 32 km2
Period of Record: August 1951 to current year (discharge data), Field/lab water quality data Oct 1948 to current year.
Lemon Creek Glacier in the spring. Previous Work
Because of its ease of access and its designation as a one of nine representative glaciers for the 1957/58 International Geophysical Year, Lemon Creek Glacier has been extensively studied over the decades. The data are reported to the World Glacier Monitoring Service (WGMS) annually. Field observations were initiated in 1953, under the direction of the Juneau Icefield Research Program (JIRP). Seasonal measurements and a consistent network of snowpit sites were added to the protocol in 2016 to align methodology with the other benchmark glaciers. Reanalysis of the five USGS Benchmark Glaciers (including Lemon Creek) was published by O’Neil et al (2019) and underscored the importance of using geodetic calibration to evaluate mass-balance trends based on the direct glacier measurements.
- Science
Glaciers and Climate Project
Mountain glaciers are dynamic reservoirs of frozen water closely coupled to ecosystems and climate. Glacier change in North America has major socioeconomic impacts, including global sea level change, tourism disruption, natural hazard risk, fishery effects, and water resource alteration. Understanding and quantifying precise connections between glaciers and climate is critical to decision makers...Additional Research Glaciers
Black Rapids, Columbia and Hubbard glaciers are also researched by the USGS.Wolverine Glacier
Wolverine Glacier is located in the high-latitude maritime climate regime of Alaska’s Kenai Mountains. Glacier observations began at this site in 1966.Sperry Glacier
Sperry Glacier is located along the Continental Divide within Glacier National Park, Montana. It represents the midlatitude continental or transitional climate. Glacier observations began at this site in 2005.South Cascade Glacier
South Cascade Glacier is located in the midlatitude maritime climate of the North Cascade Mountains of Washington State. Glacier observations began at this site in 1958.Gulkana Glacier
Gulkana Glacier is located in the high-latitude continental climate regime of Alaska’s Delta Mountains. Glacier observations began at this site in 1966.Mass Balance Summary
The USGS Benchmark Glacier Project measures changes in mass balance at five benchmark glaciers: Gulkana (AK), Wolverine (AK), Lemon Creek (AK), South Cascade (WA), and Sperry (MT).Mass Balance Methods - Measuring Glacier Change
Nearly all Earth's alpine glaciers are losing ice, usually expressed as loss of mass. Rates of mass loss for North American glaciers are among the highest on Earth (Gardner, 2013) and shrinking glaciers are often the most visible indicators of mountain ecosystems responding to climate change. - Multimedia
- Publications
Filter Total Items: 35
Specialized meltwater biodiversity persists despite widespread deglaciation
Glaciers are important drivers of environmental heterogeneity and biological diversity across mountain landscapes. Worldwide, glaciers are receding rapidly due to climate change, with important consequences for biodiversity in mountain ecosystems. However, the effects of glacier loss on biodiversity have never been quantified across a mountainous region, primarily due to a lack of adequate data atAuthorsClint C. Muhlfeld, Timothy Joseph Cline, J. Joseph Giersch, Erich Peitzsch, Caitlyn Florentine, Dean Jacobsen, Scott HotalingParsing complex terrain controls on mountain glacier response to climate forcing
Glaciers are a key indicator of changing climate in the high mountain landscape. Glacier variations across a mountain range are ultimately driven by regional climate forcing. However, changes also reflect local, topographically driven processes such as snow avalanching, snow wind-drifting, and radiation shading as well as the initial glacier conditions such as hypsometry and ice thickness. Here weAuthorsCaitlyn Elizabeth Florentine, Joel T. Harper, Daniel B. FagreExplaining mass balance and retreat dichotomies at Taku and Lemon Creek Glaciers, Alaska
We reanalyzed mass balance records at Taku and Lemon Creek Glaciers to better understand the relative roles of hypsometry, local climate and dynamics as mass balance drivers. Over the 1946–2018 period, the cumulative mass balances diverged. Tidewater Taku Glacier advanced and gained mass at an average rate of +0.25±0.28 m w.e. a–1, contrasting with retreat and mass loss of –0.60±0.15 m w.e. a-1 atAuthorsChristopher J. McNeil, Shad O'Neel, Michael Loso, Mauri Pelto, Louis C. Sass, Emily Baker, Seth CampbellGlacier retreat in Glacier National Park, Montana
Currently, the volume of land ice on Earth is decreasing, driving consequential changes to global sea level and local stream habitat. Glacier retreat in Glacier National Park, Montana, U.S.A., is one example of land ice loss and glacier change. The U.S. Geological Survey Benchmark Glacier Project conducts glaciological research and collects field measurements across select North American glaciers,AuthorsCaitlyn FlorentineReanalysis of the U.S. Geological Survey Benchmark Glaciers: Long-term insight into climate forcing of glacier mass balance
Mountain glaciers integrate climate processes to provide an unmatched signal of regional climate forcing. However, extracting the climate signal via intercomparison of regional glacier mass balance records can be problematic when methods for extrapolating and calibrating direct glaciological measurements are mixed or inconsistent. To address this problem, we reanalyzed and compared long-term massAuthorsShad O'Neel, Christopher J. McNeil, Louis C. Sass, Caitlyn Florentine, Emily Baker, Erich Peitzsch, Daniel J McGrath, Andrew G. Fountain, Daniel B. FagreGlacier recession since the Little Ice Age: Implications for water storage in a Rocky Mountain landscape
Glacial ice is a significant influence on local climate, hydrology, vegetation, and wildlife. We mapped a complete set of glacier areas from the Little Ice Age (LIA) using very high-resolution satellite imagery (30-cm) within Glacier National Park, a region that encompasses over 400,000 hectares. We measured glacier change across the park using LIA glacier area as a baseline and used this to estimAuthorsChelsea Mikle, Daniel B. FagreInterannual snow accumulation variability on glaciers derived from repeat spatially extensive ground-penetrating radar surveys
There is significant uncertainty regarding the spatiotemporal distribution of seasonal snow on glaciers, despite being a fundamental component of glacier mass balance. To address this knowledge gap, we collected repeat, spatially extensive high-frequency ground-penetrating radar (GPR) observations on two glaciers in Alaska for five consecutive years. GPR measurements showed steep snow water equivaAuthorsDaniel J McGrath, Louis Sass, Shad O'Neel, Christopher J. McNeil, Salvatore G Candela, Emily Baker, Hans P. MarshallLocal topography increasingly influences the mass balance of a retreating cirque glacier
Local topographically driven processes – such as wind drifting, avalanching, and shading – are known to alter the relationship between the mass balance of small cirque glaciers and regional climate. Yet partitioning such local effects from regional climate influence has proven difficult, creating uncertainty in the climate representativeness of some glaciers. We address this problem for Sperry GlaAuthorsCaitlyn Florentine, Joel T. Harper, Daniel B. Fagre, Johnnie Moore, Erich H. PeitzschGlacierized headwater streams as aquifer recharge corridors, subarctic Alaska
Arctic river discharge has increased in recent decades although sources and mechanisms remain debated. Abundant literature documents permafrost thaw and mountain glacier shrinkage over the past decades. Here we link glacier runoff to aquifer recharge via a losing headwater stream in subarctic Interior Alaska. Field measurements in Jarvis Creek (634 km2), a subbasin of the Tanana and Yukon Rivers,AuthorsAnna K. Lilledahl, Anne Gadeke, Shad O'Neel, T. A. Gatesman, T. A. DouglasSnow and ice
Temperature and precipitation are key determinants of snowpack levels. Therefore, climate change is likely to affect the role of snow and ice in the landscapes and hydrology of the Chugach National Forest region.Downscaled climate projections developed by Scenarios Network for Alaska and Arctic Planning (SNAP) are useful for examining projected changes in snow at relatively fine resolution using aAuthorsJeremy S. Littell, Stephanie A. McAfee, Shad O'Neel, Louis C. Sass, Evan Burgess, Steve Colt, Paul ClarkGeometry, mass balance and thinning at Eklutna Glacier, Alaska: an altitude-mass-balance feedback with implications for water resources
We analyzed glacier surface elevations (1957, 2010 and 2015) and surface mass-balance measurements (2008–2015) on the 30 km2 Eklutna Glacier, in the Chugach Mountains of southcentral Alaska. The geodetic mass balances from 1957 to 2010 and 2010 to 2015 are −0.52 ± 0.46 and −0.74 ± 0.10 m w.e. a−1, respectively. The glaciological mass balance of −0.73 m w.e. a−1 from 2010 to 2015 is indistinguishabAuthorsLouis C. Sass, Michael G. Loso, Jason Geck, Evan Thoms, Daniel McgrathHypsometric control on glacier mass balance sensitivity in Alaska and northwest Canada
Glacier hypsometry provides a first‐order approach for assessing a glacier's response to climate forcings. We couple the Randolph Glacier Inventory to a suite of in situ observations and climate model output to examine potential change for the ∼27,000 glaciers in Alaska and northwest Canada through the end of the 21st century. By 2100, based on Representative Concentration Pathways (RCPs) 4.5–8.5AuthorsDaniel Mcgrath, Louis C. Sass, Shad O'Neel, Anthony A. Arendt, C. Kienholz