中国农业气象
中國農業氣象
중국농업기상
AGRICULTURAL METEOROLOGY
2009年
4期
509-514
,共6页
龚宇%石志增%花家嘉%王爱军
龔宇%石誌增%花傢嘉%王愛軍
공우%석지증%화가가%왕애군
气温%蒸发%降水%降蒸差
氣溫%蒸髮%降水%降蒸差
기온%증발%강수%강증차
Temperature%Evaporation%Precipitation%Difference of precipitation to evaporation
地面蒸发量、气温和降水是估算水资源各分量的重要物理量.利用唐山地区7个站点1959-2006年的月平均气温及月降水资料,分析了唐山地区气温、降水的变化特征,用高桥浩一郎的陆面蒸发经验公式估算了蒸发量,并分析计算了相应的降蒸差及其演变特征.结果显示:(1)自1995年发生由冷到暖的突变以来,当地气温呈显著上升趋势,线性倾向值为0.3℃/10a.(2)降水量、蒸发量和降蒸差季节分布和逐月分布一致,1月最小,7月最大.夏季降水最为丰富,秋季次之,春季和冬季最少.(3)降水量和降蒸差的年际间变幅很大(降水距平值范围为-260.3~384.9mm),且呈减少趋势,蒸发量变幅没有降水量变幅大(蒸发距平值范围为-127.4~147.1mm),且年际间相对稳定.(4)未来本地区旱涝问题依然存在,水资源短缺的形势依然严峻.
地麵蒸髮量、氣溫和降水是估算水資源各分量的重要物理量.利用唐山地區7箇站點1959-2006年的月平均氣溫及月降水資料,分析瞭唐山地區氣溫、降水的變化特徵,用高橋浩一郎的陸麵蒸髮經驗公式估算瞭蒸髮量,併分析計算瞭相應的降蒸差及其縯變特徵.結果顯示:(1)自1995年髮生由冷到暖的突變以來,噹地氣溫呈顯著上升趨勢,線性傾嚮值為0.3℃/10a.(2)降水量、蒸髮量和降蒸差季節分佈和逐月分佈一緻,1月最小,7月最大.夏季降水最為豐富,鞦季次之,春季和鼕季最少.(3)降水量和降蒸差的年際間變幅很大(降水距平值範圍為-260.3~384.9mm),且呈減少趨勢,蒸髮量變幅沒有降水量變幅大(蒸髮距平值範圍為-127.4~147.1mm),且年際間相對穩定.(4)未來本地區旱澇問題依然存在,水資源短缺的形勢依然嚴峻.
지면증발량、기온화강수시고산수자원각분량적중요물리량.이용당산지구7개참점1959-2006년적월평균기온급월강수자료,분석료당산지구기온、강수적변화특정,용고교호일랑적륙면증발경험공식고산료증발량,병분석계산료상응적강증차급기연변특정.결과현시:(1)자1995년발생유랭도난적돌변이래,당지기온정현저상승추세,선성경향치위0.3℃/10a.(2)강수량、증발량화강증차계절분포화축월분포일치,1월최소,7월최대.하계강수최위봉부,추계차지,춘계화동계최소.(3)강수량화강증차적년제간변폭흔대(강수거평치범위위-260.3~384.9mm),차정감소추세,증발량변폭몰유강수량변폭대(증발거평치범위위-127.4~147.1mm),차년제간상대은정.(4)미래본지구한로문제의연존재,수자원단결적형세의연엄준.
The ground evaporation, temperature and precipitation are important parameters for estimating the water resources. By using the data of month mean temperature and month precipitation in 1959 -2006 from seven meteorological stations in Tangshan, the characteristics of atmospheric temperature and precipitation changes was analyzed. The land evaporation empirical equation of Takahashi's Equation was applied to estimate evaporation, water resources and other parameters related to water resources. The results showed that the temperature increased significantly in Tangshan since 1995. The linear trend of the increasing temperature was with 0.3℃ per decade. The seasonal distribution of precipitation, evaporation and available water resources was in accordance with the monthly distribution. The precipitation and water resources varied greatly in different year. The anomaly precipitation was between - 260. 3 mm and 384. 9 mm with a decreased trend. The evaporation did not change obviously with anomaly evaporation between - 127. 4mm and 47.1 mm, and its inter-annual value was rather steady. The risks of the future droughts and floods in the region still existed and water resources shortage was one of the faced challenges.