A 30-Year Record of Surface Mass Balance (1966-95), and Motion and Surface Altitude (1975-95) at Wolverine Glacier, Alaska

• Main Authors: Mayo, Lawrence R., Trabant, Dennis C., March, Rod S.
• Other Authors: GEOLOGICAL SURVEY ANCHORAGE AK
• Format: Text
• Language: English
• Published: 2004
• Subjects: Snow; Ice and Permafrost; *MEASUREMENT; *ALASKA; *MOTION; *ALTITUDE; *GLACIERS; *SURFACES; MASS; SUMMER; ANCHORS(STRUCTURAL); ICE FORMATION; SNOW COVER; TABLES(DATA); GEODETIC SURVEYS; STAKES; GLACIER MASS BALANCE MEASUREMENTS; glacier; glaciers; Ice; permafrost; Alaska
• Online Access: http://www.dtic.mil/docs/citations/ADA440036; http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA440036

Scientific measurements at Wolverine Glacier, on the Kenai Peninsula in south-central Alaska, began in April 1966. At three long-term sites in the research basin, the measurements included snow depth, snow density, heights of the glacier surface and stratigraphic summer surfaces on stakes, and identification of the surface materials. Calculations of the mass balance of the surface strata - snow, new firn, superimposed ice, and old firn and ice mass at each site were based on these measurements. Calculations of fixed-date annual mass balances for each hydrologic year (October 1 to September 30), as well as net balances and the dates of minimum net balance measured between time-transgressive summer surfaces on the glacier, were made on the basis of the strata balances augmented by air temperature and precipitation recorded in the basin. From 1966 through 1995, the average annual balance at site A (590 meters altitude) was -4.06 meters water equivalent; at site B (1,070 meters altitude), was -0.90 meters water equivalent; and at site C (1,290 meters altitude), was +1.45 meters water equivalent. The original document contains color images.