An investigation was carried out at the Jagaramogara basin in Tendo, Yamagata from 1996 to 1997. Obtained results are as follows:
(1) There are wind caves or holes with changeable wind direction, blowing out cool air from the holes in summer half year of May to October and drawing in cold air in winter half year of November to April at the basin bottoms of Ohjigoku and Shimojigoku in Jagaramogara. The author found that the entrances of wind in summer and exits of wind in winter are the stone holes from the region below the cliff of Amayobari west slope to the region fallen down on upper Murakumonoike, and also found that the same regions mentioned above are the entrance in summer and the exit in winter including with the upper holes of the sloped area at Shimojigoku basin.
(2) The hole air temperature was observed 0°C at the end of May, 2 to 3°C with relative humidity of 100% and wind speed of 1.5m/s from July to August, maximum of 5.3°C in the middle ten days of October and minimum of -5.4°C in the last ten days of January. There are ices in the wind cave at least until June. The air temperature of blowing wind from the hole in summer is low based on the conduction heat contacted from the ice to air and by cooling of sublimation, fusion and evaporation heats.
(3) Inversion of air temperature frequently appeared at night from autumn to spring and is fairly even at the daytime in summer. Strong cooling continued for a long period by adding to the cold air lake with temperature inversion and to cold air blowing out from the holes of basin bottom under a proper condition.
(4) The cold air current being relatively dry and warm is observed and typical wind speed is fairly strong of 2.0 to 2.5m/s. The air current starts to blow from the elevation 760m on Amayobari Mt., slides down on the slope and joins in the basin. The cold air lake is developed by radiation cooling. The thermal belt appeared at the elevation of 560 to 570m.
(5) The plant profile indicates the reverse distribution to elevation which the semi-alpine plants of dwarfing with cold-drought resistance are found near the lower part of basin. There are many plant species, but the number of holes were decreased recently.
View full abstract