CAJ | 학술논문

基于石羊河流域区1961—2010年气温、最高气温、最低气温、相对湿度、降水量、风速和日照百分率等气候要素资料,应用修订的Penman-Monteith(P-M)模型计算了最大潜在蒸散量和地表湿润指数,分析其空间分布、年际和年代际变化特征及其主要气象因子的影响.结果表明:1961—2010年间,研究区年降水量呈增加趋势,降水量变化曲线线性拟合倾向率为2.128~10.061 mm·(10a)-1,春夏季增幅较大;最大潜在蒸散量呈增加趋势,年最大潜在蒸散量变化曲线线性拟合倾向率在1.598~12.892 mm·(10a)-1,春夏季增幅最大;地表湿润指数变化也呈增加趋势,年地表湿润指数变化曲线线性拟合倾向率0.001~0.059(10a)-1,冬季增幅最大,在20 a周期附近,出现了2~4个干湿交替期,2002年之后为偏湿期,在高频区,2004—2005年有偏干振荡;影响石羊河流域区陆地表层湿润指数的主要因子是降水量、相对湿度.
기우석양하류역구1961—2010년기온、최고기온、최저기온、상대습도、강수량、풍속화일조백분솔등기후요소자료,응용수정적Penman-Monteith(P-M)모형계산료최대잠재증산량화지표습윤지수,분석기공간분포、년제화년대제변화특정급기주요기상인자적영향.결과표명:1961—2010년간,연구구년강수량정증가추세,강수량변화곡선선성의합경향솔위2.128~10.061 mm·(10a)-1,춘하계증폭교대;최대잠재증산량정증가추세,년최대잠재증산량변화곡선선성의합경향솔재1.598~12.892 mm·(10a)-1,춘하계증폭최대;지표습윤지수변화야정증가추세,년지표습윤지수변화곡선선성의합경향솔0.001~0.059(10a)-1,동계증폭최대,재20 a주기부근,출현료2~4개간습교체기,2002년지후위편습기,재고빈구,2004—2005년유편간진탕;영향석양하류역구륙지표층습윤지수적주요인자시강수량、상대습도.
Based on climatic observational data of temperature, maximum temperature, minimum temperature, relative humidity, precipitation, wind speed and sunshine duration in the Shiyang River basin during the year 1961-2010, the data of maximum potential evapotranspiration (ET0) and terrestrial surface humid index was computed by revised Penman-Monteith Model. The distribution, inter-annual change and the seasonal difference of ET0 and surface humid index were analyzed, and the climatic impact factors for the change trend of surface humid index were discussed. The main results were as follows: In 1961-2010, the annual precipitation in this region had an increased trend, the annual precipitation change curves’ linear fitting rate is 2.128-10.061 mm·(10a)-1, and the increasing rate mostly appeared bigger in spring and summer. The annual ET0 displayed an ascending trend as well, and the linear fitting rate of the annual ET0 change curves is 1.598-12.892 mm·(10a)-1, the biggest increasing rate appeared mostly in spring and summer. The surface humid index displayed an ascending trend,with the linear fitting rate of its change curves being 0.001-0.059 (10a)-1, the biggest increasing rate appeared mostly in winter. The climatic 2-4 periods of dry and wet alternation happened about every 20 a period of time and frequency, which was the light wet stages since 2002, while the light dry stages appeared at a higher frequency in 2004-2005. The main factors which could influence the surface humid index were the precipitation and the relative humidity.