INCREASED SURFACE ALBEDO IN NORTHERN HEMISPHERE

[11] KENNETT J P, 1972, Quaternary Research (Orlando), V2, P384, DOI 10.1016/0033-5894(72)90062-2

[12] Koch L., 1945, MEDDELELSER GRONLAND, V130, P1

[13] Kukla G. J., 1972, Quaternary Research, V2, P412, DOI 10.1016/0033-5894(72)90067-1

[14] KUKLA J, 1969, GEOL MIJNBOUW, V48, P307

[15] Kung E. C., 1964, MONTHLY WEATHER REVI, V92, P543, DOI DOI 10.1175/1520-0493(1964)092<0543:SOACSA>2.3.CO

[16] 2

[17] 2-WAY RELATIONSHIP BETWEEN THE SNOW OR ICE LIMIT AND 1,000-500 MB THICKNESSES IN THE OVERLYING ATMOSPHERE [J]. QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1955, 81 (348) : 172 - 189

[18] Langleben M. P., 1972, J GLACIOL, V11, P337

[19] MARSHUNOVA MS, 1961, T ARKT ANTARKT NAUCH, V229, P5

[20] MCCLAIN EP, 1969, NESC12 NAT ENV SAT C

[11] KENNETT J P, 1972, Quaternary Research (Orlando), V2, P384, DOI 10.1016/0033-5894(72)90062-2

[12] Koch L., 1945, MEDDELELSER GRONLAND, V130, P1

[13] Kukla G. J., 1972, Quaternary Research, V2, P412, DOI 10.1016/0033-5894(72)90067-1

[14] KUKLA J, 1969, GEOL MIJNBOUW, V48, P307

[15] Kung E. C., 1964, MONTHLY WEATHER REVI, V92, P543, DOI DOI 10.1175/1520-0493(1964)092<0543:SOACSA>2.3.CO

[16] 2

[17] 2-WAY RELATIONSHIP BETWEEN THE SNOW OR ICE LIMIT AND 1,000-500 MB THICKNESSES IN THE OVERLYING ATMOSPHERE [J]. QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1955, 81 (348) : 172 - 189

[18] Langleben M. P., 1972, J GLACIOL, V11, P337

[19] MARSHUNOVA MS, 1961, T ARKT ANTARKT NAUCH, V229, P5

[20] MCCLAIN EP, 1969, NESC12 NAT ENV SAT C