Add to ORKGMeteorological observations were carried out in the period from August to December 1994,in order to make clear the characteristics of mountain winds which develop in the upper and middle course of the Obitsu River. The results of this study are summarized as follows 1) Mountain winds developed twice in August and once in December during the 5-month observation period from August to December, 1994. 2) When mountain winds blew, a thermal belt was formed near Lake Kameyama. 3) Mountain winds, which were observed in August, developed only in the upper course of the Obitsu River. 4) Mountain winds were observed in the upper and middle course of the Obitsu River in December. The winds developed more strongly in the middle course than in the upper...
The objective of this paper is to clarify the cooling effect of going-up sea breeze along the canal ...
Observational data collected in the Lake Tekapo hydro catchment of the Southern Alps in New Zealand ...
Wind and vertical distribution of the temperature have been continuously observed fromApril 1976 usi...
Meteorological observations were carried out in the period from August to December 1994,in order to ...
Meteorological observations were carried out in the period from January to July 1995. In order to ma...
To clarify the characteristics of mountain winds around a valley mouth, the local climate in Oume Ci...
To clarify the effects of mountain winds on urban temperatures, meteorological observations were con...
The purpose of this paper is to show differences between some height fields in unusually hot summer ...
Making local meteorological observations on the southeastern slope of Mt. Shiouji in Dazaifu on a ca...
In this paper the author sought to clarify the interaction between the nocturnal heat island phenome...
The lapse rates of air temperature were found to be 0. 7℃/100m in the austral summer and 1. 1～1. 2℃/...
The Yamase is a cold, humid, northeasterly wind blowing toward the coast on the Pacific side of the ...
Meteorological data collected at mountain sites during the period 2006?2010 were archived under the ...
The purpose of this study is to investigate the thermal environment in Kumamoto and to develop the t...
Field observation was carried out around the Turumi river and in the Tama river to estimate their co...
The objective of this paper is to clarify the cooling effect of going-up sea breeze along the canal ...
Observational data collected in the Lake Tekapo hydro catchment of the Southern Alps in New Zealand ...
Wind and vertical distribution of the temperature have been continuously observed fromApril 1976 usi...
Meteorological observations were carried out in the period from August to December 1994,in order to ...
Meteorological observations were carried out in the period from January to July 1995. In order to ma...
To clarify the characteristics of mountain winds around a valley mouth, the local climate in Oume Ci...
To clarify the effects of mountain winds on urban temperatures, meteorological observations were con...
The purpose of this paper is to show differences between some height fields in unusually hot summer ...
Making local meteorological observations on the southeastern slope of Mt. Shiouji in Dazaifu on a ca...
In this paper the author sought to clarify the interaction between the nocturnal heat island phenome...
The lapse rates of air temperature were found to be 0. 7℃/100m in the austral summer and 1. 1～1. 2℃/...
The Yamase is a cold, humid, northeasterly wind blowing toward the coast on the Pacific side of the ...
Meteorological data collected at mountain sites during the period 2006?2010 were archived under the ...
The purpose of this study is to investigate the thermal environment in Kumamoto and to develop the t...
Field observation was carried out around the Turumi river and in the Tama river to estimate their co...
The objective of this paper is to clarify the cooling effect of going-up sea breeze along the canal ...
Observational data collected in the Lake Tekapo hydro catchment of the Southern Alps in New Zealand ...
Wind and vertical distribution of the temperature have been continuously observed fromApril 1976 usi...