农业科学与技术(英文版)
農業科學與技術(英文版)
농업과학여기술(영문판)
AGRICULTURAL SCIENCE & TECHNOLOGY
2009年
5期
30-33
,共4页
谢今范%曾丽红%宋开山%张柏
謝今範%曾麗紅%宋開山%張柏
사금범%증려홍%송개산%장백
澳大利亚%参考作物蒸散量%Penman-Monteith方程%时空变化
澳大利亞%參攷作物蒸散量%Penman-Monteith方程%時空變化
오대리아%삼고작물증산량%Penman-Monteith방정%시공변화
Australia%Reference evapotranspiration%Penman-Monteith equation%Spatiotemporal change
[目的] 探讨参考作物蒸散量在全球气候变化环境中的区域响应形式及其影响因素.[方法] 利用Penman-Monteith方程计算澳大利亚1998~2007年的参考作物蒸散量(ET0),通过GIS方法分析ET0的时空变化特征并探讨了ET0与主要气候因子的关系.[结果] ①澳大利亚多年平均ET0呈半环状分布,自东、南两面向西北部和内陆逐渐增加,与气候带分布具有较高的空间一致性;②全区平均ET0约1 750 mm,2000年取得最小值(1 647.97 mm),2002年取得最大值(1 851.45 mm);③ ET0按夏、春、秋、冬的顺序递减,1月、12月ET0最高,分别为200.42 mm、201.24 mm,6月最低,为79.55 mm;④ ET0与平均气温、太阳辐射量正相关,确定性系数分别为0.83、0.94,与平均相对湿度呈负相关关系,与降水量没有明显的相关性.[结论] 该研究为澳大利亚的作物需水量研究及灌溉措施的制定提供了参考.
[目的] 探討參攷作物蒸散量在全毬氣候變化環境中的區域響應形式及其影響因素.[方法] 利用Penman-Monteith方程計算澳大利亞1998~2007年的參攷作物蒸散量(ET0),通過GIS方法分析ET0的時空變化特徵併探討瞭ET0與主要氣候因子的關繫.[結果] ①澳大利亞多年平均ET0呈半環狀分佈,自東、南兩麵嚮西北部和內陸逐漸增加,與氣候帶分佈具有較高的空間一緻性;②全區平均ET0約1 750 mm,2000年取得最小值(1 647.97 mm),2002年取得最大值(1 851.45 mm);③ ET0按夏、春、鞦、鼕的順序遞減,1月、12月ET0最高,分彆為200.42 mm、201.24 mm,6月最低,為79.55 mm;④ ET0與平均氣溫、太暘輻射量正相關,確定性繫數分彆為0.83、0.94,與平均相對濕度呈負相關關繫,與降水量沒有明顯的相關性.[結論] 該研究為澳大利亞的作物需水量研究及灌溉措施的製定提供瞭參攷.
[목적] 탐토삼고작물증산량재전구기후변화배경중적구역향응형식급기영향인소.[방법] 이용Penman-Monteith방정계산오대리아1998~2007년적삼고작물증산량(ET0),통과GIS방법분석ET0적시공변화특정병탐토료ET0여주요기후인자적관계.[결과] ①오대리아다년평균ET0정반배상분포,자동、남량면향서북부화내륙축점증가,여기후대분포구유교고적공간일치성;②전구평균ET0약1 750 mm,2000년취득최소치(1 647.97 mm),2002년취득최대치(1 851.45 mm);③ ET0안하、춘、추、동적순서체감,1월、12월ET0최고,분별위200.42 mm、201.24 mm,6월최저,위79.55 mm;④ ET0여평균기온、태양복사량정상관,학정성계수분별위0.83、0.94,여평균상대습도정부상관관계,여강수량몰유명현적상관성.[결론] 해연구위오대리아적작물수수량연구급관개조시적제정제공료삼고.
[Objective] To discuss regional response of reference evapotranspiration (ET0) to global climate change and its influencing factors. [Method] Penman-Monteith equation was adopted to calculate ET0 in Australia from 1998 to 2007. Spatiotemporal change characteristics were analyzed by using GIS spatial analysis tools and relationships between ET0 and main climate factors were also analyzed. [Results] The results showed that multi-year average ET0 increased from the east and south part to the northwest part and inland, and its distribution was consistent with climate zones. Multi-year average ET0 of the whole region was 1 750 mm, obtaining minimum and maximum values in 2000 and 2002 respectively. Regional ET0 decreased in the order of summer, spring, autumn and winter; January and December got the highest monthly ET0, while June got the lowest value 79.55 mm. ET0 positively correlated with mean temperature and solar radiation, R2 for each were 0.83 and 0.94, while the relationship between ET0 and average relative humidity was negative, and precipitation had no significant relationship with ET0. [Conclusion] This research could provide important reference for crop water requirement study and making irrigation method for Australia.