Source: http://gtnpdatabase.org/activelayers/view/16
Timestamp: 2019-04-26 08:40:32+00:00

Document:
Happy Valley grid is located on the Unglaciated foothills. Landcover units include Tussock-graminoid, dwarf- shrub tundra and low-shrub tundra (moist acidic). U9a 1-ha grid located within U9B 1-km grid.
Walker, D. A., H. E. Epstein, W. A. Gould, A. Kade, A.M. Kelley, J. A. Knudson, W. B. Krantz, R. A. Peterson, G. Michaelson, R.A. Peterson, C. L. Ping, M. A. Raynolds, V. E. Romanovsky, Y. Shur, and M.D. Walker, Frost-boil ecosystems: complex interactions between landforms, soils, vegetation, and climate, Permafrost and Periglacial Processes, 15: 171-188, 2004.
Sturm, M., Schimel, J., Michelson, G., Welker, J., Oberbauer, S. F., Liston, G. E., Fahnestock, J., and V. E. Romanovsky, Are winter biological processes important in converting arctic tundra to shrubland?, BioScience, Vol. 55, No. 1: 17 26, 2005.
Shimel, J. P., Fahnstock, J., Michaelson, G. J., Mican, C., Ping, C., Romanovsky, V. E. and J. Welker, A microbial activity based model of winter CO2 fluxes in Arctic tundra communities, Arctic, Antarctic, and Alpine Research,Vol. 38, No. 2, 249-256, 2006.
Nicolsky, D. J., Romanovsky, V. E., Alexeev, V. A. and D. M. Lawrence, Improved modeling of permafrost dynamics in Alaska with CLM3, Geophysical Research Letters, VOL. 34, L08501, doi:10.1029/2007GL029525, 2007.
Nicolsky, D. J., Romanovsky, V.E., and G. S.Tipenko, Using in-situ temperature measurements to estimate saturated soil thermal properties by solving a sequence of optimization problems, The Cryosphere, 1, 41 58, 2007.
Brown, J. and V. E. Romanovsky, Report from the International Permafrost Association: State of Permafrost in the First Decade of the 21st Century, Permafrost and Periglacial Processes, 19: 255 260, 2008.
Kade, A., Romanovsky, V. E. and D. A. Walker, The N-factor of nonsorted circles along a climate gradient in Arctic Alaska, Permafrost and Periglacial Processes, 17: 279-289, 2006.

References: V. 
 V. 
 V. 
 V. 
 V. 
 V. 
 V.