气候与环境研究
氣候與環境研究
기후여배경연구
CLIMATIC AND ENVIRONMENTAL RESEARCH
2014年
3期
351-361
,共11页
区域气候模式%土地利用/覆盖变化%东北区域%气候变化%数值模拟
區域氣候模式%土地利用/覆蓋變化%東北區域%氣候變化%數值模擬
구역기후모식%토지이용/복개변화%동북구역%기후변화%수치모의
Regional climate model%Land-use and land-cover change%Northeast China%Climate change%Numerical simulation
基于1990、2005年两期不同土地利用/覆盖资料,利用区域环境集成模拟系统(RIEMS2.0)分别进行2次连续15年数值模拟,探讨东北土地利用/覆盖变化对气候的影响,分析集中于气温和降水等要素变化上,并对结果进行统计显著性检验。结果表明:(1)东北农田扩张后,东北夏季和冬季平均气温降低,降水减少,并且农田面积扩张的范围越大,气温变化幅度也越大。在夏季,黑河西部、呼伦贝尔南部部分地区降温超过0.5°C,并通过显著性检验(P<0.05),大兴安岭南部、黑河西部等地区夏季降水减少20%左右,其中产生减少的大部分区域通过显著性检验(P<0.05)。(2)东北农田扩张通过影响潜热通量的变化和净吸收辐射通量的变化来影响气温的变化,其中东北南部土地利用/覆盖类型变化主要表现为短草类型转变为农田类型,这使得夏季蒸散发增加,潜热通量增加,气温降低。(3)东北农田扩张也影响大气环流场的变化,并与降水的变化有密切的关系。辽宁西部和东北北部部分地区夏季蒸散发增加,大气中水汽增加,但是由于大气环流场变化,降水在这两个地区并未增加。
基于1990、2005年兩期不同土地利用/覆蓋資料,利用區域環境集成模擬繫統(RIEMS2.0)分彆進行2次連續15年數值模擬,探討東北土地利用/覆蓋變化對氣候的影響,分析集中于氣溫和降水等要素變化上,併對結果進行統計顯著性檢驗。結果錶明:(1)東北農田擴張後,東北夏季和鼕季平均氣溫降低,降水減少,併且農田麵積擴張的範圍越大,氣溫變化幅度也越大。在夏季,黑河西部、呼倫貝爾南部部分地區降溫超過0.5°C,併通過顯著性檢驗(P<0.05),大興安嶺南部、黑河西部等地區夏季降水減少20%左右,其中產生減少的大部分區域通過顯著性檢驗(P<0.05)。(2)東北農田擴張通過影響潛熱通量的變化和淨吸收輻射通量的變化來影響氣溫的變化,其中東北南部土地利用/覆蓋類型變化主要錶現為短草類型轉變為農田類型,這使得夏季蒸散髮增加,潛熱通量增加,氣溫降低。(3)東北農田擴張也影響大氣環流場的變化,併與降水的變化有密切的關繫。遼寧西部和東北北部部分地區夏季蒸散髮增加,大氣中水汽增加,但是由于大氣環流場變化,降水在這兩箇地區併未增加。
기우1990、2005년량기불동토지이용/복개자료,이용구역배경집성모의계통(RIEMS2.0)분별진행2차련속15년수치모의,탐토동북토지이용/복개변화대기후적영향,분석집중우기온화강수등요소변화상,병대결과진행통계현저성검험。결과표명:(1)동북농전확장후,동북하계화동계평균기온강저,강수감소,병차농전면적확장적범위월대,기온변화폭도야월대。재하계,흑하서부、호륜패이남부부분지구강온초과0.5°C,병통과현저성검험(P<0.05),대흥안령남부、흑하서부등지구하계강수감소20%좌우,기중산생감소적대부분구역통과현저성검험(P<0.05)。(2)동북농전확장통과영향잠열통량적변화화정흡수복사통량적변화래영향기온적변화,기중동북남부토지이용/복개류형변화주요표현위단초류형전변위농전류형,저사득하계증산발증가,잠열통량증가,기온강저。(3)동북농전확장야영향대기배류장적변화,병여강수적변화유밀절적관계。료녕서부화동북북부부분지구하계증산발증가,대기중수기증가,단시유우대기배류장변화,강수재저량개지구병미증가。
Two simulations in 1990 and 2005 of land-use and land-cover in Northeast China were used to investigate the impact of land-use and land-cover change (LUCC) on climate. Using a regional environmental system integration model (RIEMS2.0) the authors simulated two consecutive 15-year periods to explore effects of the Northeast China LUCC on climate, focusing on temperature and precipitation changes, and testing their statistical significance. Results show that the expansion of northeast farmland had the following impacts on climate:(1) Mean temperatures in summer and winter in Northeast China were reduced, and precipitation decreased. The expansion of farmland areas also brought about increased changes in amplitude. Temperature changes of more than 0.5 °C is statistically significant (P<0.05) in summer in the west of Heihe and in the southern cooling areas of Hulun Buir. In summer in the south of Da Hinggan Ling and west of Heihe precipitation decreased by 20%, the greatest decrease of the regions that showed statistically significant changes (P<0.05). (2) The expansion of farmland has an influence on mean temperature through changes in the latent heat flux and the net absorption of the radiation flux. In the south of Northeast China, in which land cover type converted from mainly short grass to farmland, total summer evapotranspiration increased, the latent heat flux increased, and the temperature decreased. (3) Farmland expansion in Northeast China also results in changes in atmospheric circulation, and precipitation changes are closely related to the circulation changes. In the west of Liaoning and the northern part of Northeast China, summer water vapor in the atmosphere increased, but atmospheric circulation change at these areas did not result in an increase in precipitation in these two areas.