Dibb, J E; Jaffrezo, J L; Bales, Roger C (1999): GISP2 Concentration of H2O2 in surface snow. PANGAEA, https://doi.org/10.1594/PANGAEA.56099
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Bales, Roger C; Losleben, M V; McConnell, Joseph R (1995): H2O2 in snow, air and open pore space in firn at Summit, Greenland. Geophysical Research Letters, 22(10), 1261-1264, https://doi.org/10.1029/95GL01110
Bales, Roger C; McConnell, Joseph R; Losleben, M V; Conklin, M H; Fuhrer, Katrin; Neftel, A; Dibb, J E; Kahl, J D W; Stearns, C R (1995): Diel variations of H2O2 in Greenland: A discussion of the cause and effect relationship. Journal of Geophysical Research: Atmospheres, 100(D9), 18661-18668, https://doi.org/10.1029/95JD01841
Dibb, J E; Jaffrezo, J L (1997): Air-snow exchange investigations at Summit, Greenland: An overview. Journal of Geophysical Research: Oceans, 102(C12), 26795-26808, https://doi.org/10.1029/96JC02303
GRIP/GISP (1997): The Greenland Summit Ice Cores CD-ROM GISP2/GRIP. National Snow and Ice Data Center, University of Colorado at Boulder, and World Data Center for Paleoclimatology, National Geophysical Data Center, Boulder Colorado, CD-ROM, grip-gisp.iso
Latitude: 72.970000 * Longitude: -38.800000
Date/Time Start: 1993-05-27T09:29:00 * Date/Time End: 1993-07-20T16:09:00
Minimum Elevation: 3208.0 m * Maximum Elevation: 3208.0 m
GISP2 * Latitude: 72.970000 * Longitude: -38.800000 * Date/Time: 1990-01-01T00:39:00 * Elevation: 3208.0 m * Recovery: 3053 m * Campaign: GISP * Basis: Sampling/drilling ice * Method/Device: Drilling/drill rig (DRILL) * Comment: GISP2 is a combination of the shallow B and the deeper D core; about 200 ka
Samples were collected from the top few millimeters of snow from a 10 x 10 cm area. Samples were generally melted and analyzed within 1 to 3 hours after collection. Analysis was by the peroxidase method of Sigg et al. (1992).
|#||Name||Short Name||Unit||Principal Investigator||Method/Device||Comment|
|2||Day of the year||DOY||day||Dibb, J E|
|3||Hydrogen peroxide, water||H2O2||µmol/l||Bales, Roger C||Peroxidase||Concentration data for H2O2 in surface snow for the 1993 summer season. Samples were collected from the top few millimeters of snow from a 10 x 10 cm area. Samples were generally melted and analyzed within 1 to 3 hours after collection. Analysis was by the peroxidase method of Sigg et al. (1992). See Bales et al. (1995) for more details.|
162 data points