HR: 0800h
AN: C21A-0062    [Abstracts]
TI: Micrometeorological conditions under different soil frost depths
AU: * Nemoto, M
EM: nemo@affrc.go.jp
AF: National Agricultural Research Center for Hokkaido Region, Hitsujigaoka, Toyohira-ku, Sapporo, 062-8555, Japan
AU: Hirota, T
EM: hirota@affrc.go.jp
AF: National Agricultural Research Center for Hokkaido Region, Hitsujigaoka, Toyohira-ku, Sapporo, 062-8555, Japan
AU: Iwata, Y
EM: iwatayuk@affrc.go.jp
AF: National Agricultural Research Center for Hokkaido Region, Shinsei, Memuro, 082-0071, Japan
AU: Suzuki, S
EM: s4suzuki@nodai.ac.jp
AF: Faculty of Regional Environment Science, Tokyo University of Agriculture, Setagaya-ku, Tokyo, 150-8502, Japan
AU: Hasegawa, S
EM: hasegawa@env.agr.hokudai.ac.jp
AF: Field Science Center for Northern Biosphere, Hokkaido University, Kita-ku, Sapporo, 060- 0811, Japan
AB: Eastern Hokkaido, where is one of the largest agricultural production regions in Japan, is characterized by low air temperature and relatively thin snow covers resulting in soil frost over the winter. However, the soil frost depth has been significantly decreasing since late 1980's due to an insulation from the cold air by a thick snow cover developing in early winter. In the current study, soil water movement, soil temperature, and surface heat balance under different soil frost conditions were monitored to obtain a knowledge of changes in micrometeorological condition of the agricultural production systems in the Eastern Hokkaido associated with the decreasing soil frost depth in the region. A paired soil plot experiment was conducted from Nov. 2005 to May 2006, where the frost depth was artificially enhanced by removing snow for 24 days in the retreatment plot and the natural condition was maintained in the control plot. The soil in the experimental field was classified as Andisol with much porosity and high drainability. In each plot, water content and soil temperature were measured by TDR and thermocouple, respectively. The maximum soil-frost depth in the treatment and control plots resulted in 43.8 and 13.6\.cm, respectively. Changes in snow water equivalent volume SWE) and snow depth were manually recorded. The difference of SWE just before melting snow was same. The day of snow disappearing was 18th April 2006 for both plots. The control plot with a thin frozen layer allowed infiltration of snow melt water, and water content at the lower subsoil increased accordance in snowmelting, whereas a thick frozen layer in the treatment plot impeded the infiltration resulting in waterlogging being observed on the soil surface. These differences in profile of water content and in developing soil frost depth results in more delay in increasing soil temperature at the deeper depth. At the surface, however, the difference in soil temperature was quickly disappeared, and the differences in elements of heat balance in each plot were small. Consequently, the result suggests that the recent decreasing soil frost depth in the Eastern Hokkaido changes hydraulic and thermal soil conditions extensively below the surface, but has no feedback effect to the atmosphere after snow disappearing.
DE: 0704 Seasonally frozen ground
DE: 0740 Snowmelt
DE: 0764 Energy balance
DE: 1838 Infiltration
DE: 1866 Soil moisture
SC: Cryosphere [C]
MN: 2007 Fall Meeting