CAJ | 학술논문

利用在念青唐古拉山脉西段南坡沿海拔架设的10个翻斗式自记雨量计2006年至2008年的夏季风降水记录,分析了不同海拔降水的年际年内和日变化特征.结果表明该地区夏季降水的海拔梯度效应明显,高海拔降水日过程和低海拔差异显著,最大降水高度位于山坡上部的5 100 m附近.
이용재념청당고랍산맥서단남파연해발가설적10개번두식자기우량계2006년지2008년적하계풍강수기록,분석료불동해발강수적년제년내화일변화특정.결과표명해지구하계강수적해발제도효응명현,고해발강수일과정화저해발차이현저,최대강수고도위우산파상부적5 100 m부근.
The summer monsoon precipitation measurements during 2006 to 2008 were analyzed from 10 tipping-bucket rain gauges set up along an altitudinal transect on the southern slope of the west Nyainqentanglha Mountains. The results indicated that the altitude effects for the distribution of summer monsoon precipitation was significant. The diurnal variations of the summer precipitation at the higher altitudes shown different patterns from those at the lower altitudes. The maximum precipitation height was found at the upslope of about 5110 m a.s.l.