林业研究(英文版)
林業研究(英文版)
임업연구(영문판)
JOURNAL OF FORESTRY RESEARCH
2007年
2期
114-118
,共5页
姜纪峰%延晓冬%黄耀%郭维栋%刘辉志
薑紀峰%延曉鼕%黃耀%郭維棟%劉輝誌
강기봉%연효동%황요%곽유동%류휘지
集成生物圈模型%二氧化碳通量%感热通量%潜热通量%农田生态系统%草地生态系统
集成生物圈模型%二氧化碳通量%感熱通量%潛熱通量%農田生態繫統%草地生態繫統
집성생물권모형%이양화탄통량%감열통량%잠열통량%농전생태계통%초지생태계통
Integrated biosphere simulator (IBIS)%CO2 flux%Sensible flux%Latent heat flux%Cropland ecosystem%Grassland ecosystem
集成生物圈模型(IBIS)是目前最复杂的基于动态植被模型的陆面生物物理模型之一.应用该模型对国际CEOP计划半干旱区基准站之一的吉林通榆观测站(44°25'N , 122°52'E)草地和农田生态系统2003年全年的CO2和水、热通量变化进行模拟,并将结果与涡度相关法测定的观测值进行了对比分析,以检验IBIS模型在半干旱区的模拟能力.对比结果表明:除CO2通量模拟结果不够理想外,IBIS模型较好地模拟了通榆观测站的感热通量和潜热通量.总体上看,该模型对农田生态系统模拟的偏差小于对退化草地的模拟.
集成生物圈模型(IBIS)是目前最複雜的基于動態植被模型的陸麵生物物理模型之一.應用該模型對國際CEOP計劃半榦旱區基準站之一的吉林通榆觀測站(44°25'N , 122°52'E)草地和農田生態繫統2003年全年的CO2和水、熱通量變化進行模擬,併將結果與渦度相關法測定的觀測值進行瞭對比分析,以檢驗IBIS模型在半榦旱區的模擬能力.對比結果錶明:除CO2通量模擬結果不夠理想外,IBIS模型較好地模擬瞭通榆觀測站的感熱通量和潛熱通量.總體上看,該模型對農田生態繫統模擬的偏差小于對退化草地的模擬.
집성생물권모형(IBIS)시목전최복잡적기우동태식피모형적륙면생물물리모형지일.응용해모형대국제CEOP계화반간한구기준참지일적길림통유관측참(44°25'N , 122°52'E)초지화농전생태계통2003년전년적CO2화수、열통량변화진행모의,병장결과여와도상관법측정적관측치진행료대비분석,이검험IBIS모형재반간한구적모의능력.대비결과표명:제CO2통량모의결과불구이상외,IBIS모형교호지모의료통유관측참적감열통량화잠열통량.총체상간,해모형대농전생태계통모의적편차소우대퇴화초지적모의.
A comparison between simulated land surface fluxes and observed eddy covariance (EC) measurements was conducted to validate Integrated Biosphere Simulator (IBIS) at Tongyu field observation station (44°25'N, 122°52'E) in Jilin Province, China. Results showed that the IBIS model could reproduce net ecosystem CO2 exchange (NEE), sensible and latent heat fluxes reasonably, as indicated by correlation coefficients exceeding the significant level of 0.05. It was also evident that the NEE and sensible heat fluxes were characterized by diurnal and seasonal variation both in the grassland and the cropland ecosystems, while the latent heat fluxes correlated with evapotranspiration, only took on the diurnal variation during the growing season. Moreover, both sensible heat fluxes and the latent heat fluxes were larger in the cropland ecosystem than that in the degraded grassland ecosystem. This different characteristic was possibly correlated with vegetation growing situation in the two kinds of ecosystems. A close agreement between observation and simulation on NEE, sensible heat fluxes and latent heat flux was obtained both in the degraded grassland and the cropland ecosystems. In addition, the annual NEE in the model was overestimated by 23.21% at the grassland and 27.43% at the cropland, sensible heat flux with corresponding 9.90% and 11.98%, respectively, and the annual latent heat flux was underestimated by 4.63% and 3.48%, respectively.