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K. Finkele J.J. Katzfey E.A. Kowalczyk J.L. McGregor L. Zhang M.R. Raupach 《Boundary-Layer Meteorology》2003,107(1):49-79
Two land surface schemes, SCAM and CSIRO9, were used to model the measured energy fluxes during the OASIS (Observations At Several Interacting Scales) field program. The measurements were taken at six sites along a 100 km rainfall gradient. Two types of simulations were conducted: (1) offline simulations forced with measured atmospheric input data at each of the six sites, and (2) regional simulations with the two land surface schemes coupled to the regional climate model DARLAM.The two land surface schemes employ two different canopy modelling concepts: in SCAM the vegetation is conceptually above the ground surface, while CSIRO9 employs the more commonly used `horizontally tiled' approach in which the vegetation cover is modelled by conceptually placing it beside bare ground. Both schemes utilize the same below-ground components (soil hydrological and thermal models) to reduce the comparison to canopy processes only. However, the ground heat flux, soil evaporation and evapotranspiration are parameterised by the two canopy treatments somewhat differently.Both canopy concepts reproduce the measured energy fluxes. SCAM has a slightly higher root-mean standard error in the model-measurement comparison for the ground heat flux. The mean surface radiative temperature simulated by SCAM is approximately 1K lower than in the CSIRO9 simulations. However, the soil and vegetation temperatures (which contribute to the radiative temperature) varied more in the CSIRO9 simulations. These larger variations are due to the absence of a representation of the aerodynamic interactions between vegetation and ground. 相似文献
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Spatial and Quantitative Comparison of Satellite-Derived Land Cover Products over China 总被引：1，自引：0，他引：1 
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下载免费PDF全文 Because land cover plays an important role in global climate change studies, assessing the agreement among different land cover products is critical. Significant discrepancies have been reported among ... 相似文献
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以我国长江中下游的南京及其周边15个市(县)为例,采用野外测定、室内分析与遥感反演相结合的方法,开展了土壤电阻率估算研究.选用影响土壤电阻率的土壤水分、土壤温度、土壤可溶盐总量与土壤阳离子交换量等4个主要因子,遥感反演土壤水分和温度空间分布,以获取估算土壤电阻率所需要的主要参数;采用偏最小二乘二次多项式(PLSQM)模型对不同地表覆盖类型下的土壤电阻率进行估算,PLSQM估算模型的估算值与实测值的相关系数达到0.85,平均相对误差(MRE)为19.02%,均方根误差(RMSE)为7.79.结果表明,草地、农田、林地3种不同地表覆盖类型下土壤电阻率有明显差异,PLSQM模型实现了较高估算精度,具有较好的应用潜力. 相似文献
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全球植被与大气之间碳通量的模式估计(英文) 总被引：1，自引：0，他引：1
用大气植被相互作用模式（AVIM）模拟了全球陆地植被的净初级生产力（NPP）。AVIM由相互耦合的两部分组成：物理过程，包括陆地表面水分和能量在土壤、植被与大气之间的传输；以及生理生态过程，如：光合、呼吸、干物质分配、凋落和物候等。全球的植被分为13类，土壤按质地分为6类。用EMDI提供的全球1637个包括不同植被类型的NPP观测点数据对模型进行了检验。NPP模拟的结果表明：全球陆地植被的平均NPP为405.13gCm-2yr-1，不同植被类型的平均 NPP变化范围在99.58 g Cm-2yr-1（苔原）到996.2 g Cm-2yr-1（热带雨林）之间。全球年总NPP为60.72GtCyr-1，其中最大的部分为热带雨林，15.84GtCyr-1，占全球的26.09％。最大的碳汇是在北半球的温带。模式模拟的NPP在全球的空间和季节分布是合理的。 相似文献
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全球植被与大气之间碳通量的模式估计 总被引：15，自引：0，他引：15
用大气植被相互作用模式(AⅥM)模拟了全球陆地植被的净初级生产力(NPP)。AⅥM由相互耦合的两部分组成：物理过程，包括陆地表面水分和能量在土壤、植被与大气之间的传输；以及生理生态过程，如：光合、呼吸、干物质分配、凋落和物候等。全球的植被分为13类，土壤按质地分为6类。用EMDI提供的全球1637个包括不同植被类型的NPP观测点数据对模型进行了检验。NPP模拟的结果表明：全球陆地植被的平均NPP为405.13 g C m-2yr-1，不同植被类型的平均NPP变化范围在99.58 g C m-2yr-l(苔原)到996.2 g C m-2yr-l(热带雨林)之间。全球年总NPP为60.72 Gt C yr-l，其中最大的部分为热带雨林，15.84 Gt C yr-1，占全球的26.09％。最大的碳汇是在北半球的温带。模式模拟的NPP在全球的空间和季节分布是合理的。 相似文献
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Summary The Oklahoma Atmospheric Surface-layer Instrumentation System (OASIS) is a recently-developed observational system that collects,
archives, and quality controls atmospheric, surface, and soil data in real-time from 90 stations across Oklahoma. Ten of the
90 sites, termed “super sites”, are equipped with additional sonic anemometry and four-component net radiometers to provide
complete observations of the surface energy balance. Oklahoma Mesonet and OASIS data are used in this study to validate the
sensitivity and accuracy of a land-surface scheme within a numerical prediction model.
The Advanced Regional Prediction System (ARPS) is a three-dimensional, nonhydrostatic mesoscale model developed by the Center
for Analysis and Prediction of Storms (CAPS) at the University of Oklahoma. The land-surface model (LSM) used within ARPS
is the Interactions Soil Biosphere Atmosphere (ISBA) scheme. Mesonet and OASIS data collected from the super site located
in Norman, Oklahoma, are used as verification for the ISBA.
Research presented in this study outlines the challenges in developing, maintaining, and using in-situ data for model validation.
Such problems as instrument error, surface heterogeneity, and non-closure of the surface energy budget limit data accuracy.
Preliminary results of model validation focus on the sensitivity of the soil physics within the ISBA scheme. Model sensitivity
to vegetation cover, surface roughness, and soil type are investigated. Furthermore, several recent improvements to ISBA are
evaluated and compared to observations. This study concludes that the sensitivity of the ISBA to a priori soil and vegetation
type is detrimental for this scheme to be used in a mesoscale model without improved treatment of surface heterogeneity.
Received November 18, 2001 Revised December 28, 2001 相似文献
8.
Sensitivity study and validation of a land surface parameterization using the HAPEX-MOBILHY data set 总被引：6，自引：0，他引：6
A simple parameterization of land surface processes, amenable to the structure of a two-layer soil model, including a representation of the vegetation, has been designed for use in meteorological models. Prior to implementation in a mesoscale model, it is necessary to check the components and to verify the good working order of the parameterization as a whole. The aims of this paper then are: (i) evaluation and a sensitivity study of the various components of the model, specifying the needed accuracy for the parameters; (ii) micrometeorological validation of the model against the HAPEX-MOBILHY data set.First, we present the basic scheme. The focus is on the parameterization of surface resistance, and especially on its relationship with soil moisture.A sensitivity study is then performed through a set of one-dimensional simulations which allow a full interaction between the ground and the atmosphere. Above bare ground, it is shown that both soil texture and initial moisture greatly influence the outcome of the simulation. Latent heat flux ranges from that associated with potential evaporation through a switch-like behavior to that of dry soil. Next, the effects of transpiring vegetation canopies on the physical processes involved and the surface energy balance are examined. The sensitivity of the latent heat flux to changes in the soil and canopy parameters is emphazised; the major influence of the initial mean soil moisture and of the vegetation cover is pointed out. Finally, the evolution of the boundary layer in response to various surface conditions is studied.A validation of the land surface scheme is conducted through daily cycles during cloudless days. Simulated turbulent fluxes are successfully compared to micrometeorological measurements over a maize field at different growth stages. Over a pine forest, the correct simulation of the turbulent fluxes is obtained with an adequate parameterization of the surface resistance accounting for the atmospheric moisture deficit. 相似文献
9.
The impact of logging on precipitation in the Amazon region is investigated based on numerical experiments using the community atmosphere model version 3 coupled with the community land surface model version 3 (CAM3–CLM3). Three different representations of logging are examined, ranging from selective logging, to partial deforestation, to clear cut. Precipitation increases in response to modest selective logging, and decreases as the severity of logging progresses to partial deforestation and clear cut. Further experiments indicate that the increase of precipitation is mostly due to the decrease of surface albedo following selective logging, resulting from a low contrast between bare soil albedo and vegetation optical properties (i.e., leaf reflectance) in CLM3. This study demonstrates the complexity of representing land cover changes in climate models, and underlines the importance of accuracy in albedo measurement from satellite remote sensing. 相似文献
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Development of the IAP Dynamic Global Vegetation Model 总被引：1，自引：0，他引：1
ABSTRACT The lAP Dynamic Global Vegetation Model （IAP-DGVM） has been developed to simulate the distribution and structure of global vegetation within the framework of Earth System Models. It incorporates our group＇s recent developments of major model components such as the shrub sub-model, establishment and competition parameterization schemes, and a process-based fire parameterization of intermediate complexity. The model has 12 plant functional types, including seven tree, two shrub, and three grass types, plus bare soil. Different PFTs are allowed to coexist within a grid cell, and their state variables are updated by various governing equations describing vegetation processes from fine-scale biogeophysics and biogeochemistry, to individual and population dynamics, to large-scale biogeography. Environmental disturbance due to fire not only affects regional vegetation competition, but also influences atmospheric chemistry and aerosol emissions. Simulations under observed atmospheric conditions showed that the model can correctly reproduce the global distribution of trees, shrubs, grasses, and bare soil. The simulated global dominant vegetation types reproduce the transition from forest to grassland （savanna） in the tropical region, and from forest to shrubland in the boreal region, but overestimate the region of temperate forest. 相似文献
11.
天气雷达天线馈源的精确定位关系到雷达数据的精确使用和天气雷达全网拼图的使用效果.目前,国内新一代天气雷达天线馈源坐标基本都是使用GNSS(GLobal Navigation Satellite System)系统中的美国GPS(Global Position System)系统接收机,在雷达塔楼楼顶单点瞬时定位测量得到的,误差一般大于30 m.为了提高定位精度,将GPS精确定位技术与全站仪测量相对高度结合起来,提出了一种测量天气雷达的馈源坐标的方法,可使天线馈源的海拔高度测量精度达到10 m以内.使用这种方法对北京市气象局S波段新一代天气雷达天线馈源坐标进行了实地测量,精度达到设计要求. 相似文献
12.
金塔绿洲地表特征参数遥感反演研究 总被引：16，自引：9，他引：7
TM影像是陆地资源卫星（Landsat）携带的专题绘图仪（Thematic Mapper,TM）扫描计获取的遥感图像,近年来,该数据得到了广泛的应用。本文使用Landsat-5TM数据推算了金塔地区的地表参数,包括标准化差值植被指数NDVI、修正的土壤调整植被指数MSAVI、植被覆盖度、地表反射率及地表温度。并将地表反射率、地表温度的反演值与观测值进行对比,结果表明：地表温度反演结果的相对误差在9％以内,地表反射率反演结果的相对误差在8％以内。 相似文献
13.
Xia Zhang 《Asia-Pacific Journal of Atmospheric Sciences》2012,48(1):97-105
A soil-atmosphere-transfer model (SATM) was evaluated using observational data from the Tongyu Cropland Station and Audubon Research Ranch in semiarid areas, where the land cover was nearly bare soil during the simulation period. Simulations by the SATM at both sites were conducted using the new and original surface thermal roughness length parameterization schemes, respectively. Comparisons of simulations and observations have demonstrated that using the new surface thermal roughness length scheme in this model made sound improvements in the simulation of soil surface temperatures, sensible heat fluxes and net radiation fluxes in the daytime at both sites, compared to the original scheme, because the new scheme produced a larger aerodynamic resistance for turbulent heat transfer in the daytime. With respect to latent heat fluxes, the improvement was not as obvious as that attained for soil surface temperature since the soil water content in the surface layer in a semiarid area is a more important factor than surface soil temperature in controlling evaporation rate. Accordingly, it can be concluded that the new surface thermal roughness length parameterization scheme could improve the ability of the SATM to simulate bare soil surface energy budget with latent heat flux component being innegligible in semiarid areas. 相似文献
14.
Theoretical determination of the surface energy balance and thermal regimes of bare soils 总被引：1，自引：0，他引：1
An analytical theory that determines the thermal regimes in the soil and the thermal and moisture regimes in the atmosphere for bare surfaces is derived. Both soil and atmospheric thermal properties are assumed to be power functions of depth and height, respectively. Evaporation is determined using a surface resistance to vapour flow. Fourier superposition is used to represent nonsinusoidal variations in time due to effects such as variable cloud cover. The theory is in acceptable agreement with micrometeorological measurements made at two bare soil sites of contrasting surface bulk density. It is concluded that the surface resistance model for evaporation is applicable to bare soils which remain wet at depth, particularly if their surface is loosened. The theory is used to predict the diurnal thermal regimes of saturated and dry sand, loam, and peat soils. 相似文献
15.
E. L. Muzylev A. B. Uspenskii Z. P. Startseva E. V. Volkova A. V. Kukharskii 《Russian Meteorology and Hydrology》2010,35(3):225-235
The method of the AVHRR-3 (NOAA) radiometer measurement data subject processing is produced for the retrieval of underlying
surface temperature and several vegetation characteristics under cloud-free conditions. A technology for deriving the values
of these parameters from the MODIS (EOS/Terra and Aqua) radiometer data is developed. The estimation of the temperature and
vegetation characteristics is carried out for the Seim River basin (Kursk region) with the catchment area of 7460 km2 for 2003–2005 vegetation seasons. Practical coincidence of estimations of AVHRR- and MODIS-derived temperatures, as well
as the coincidence with ground observation results, is revealed. Statistics of these estimation errors is analyzed. Satellite-derived
estimations of land surface temperature (LST) and vegetation characteristics are used for the calibration and verification
of the developed model of the vertical heat and water transfer in the soil-vegetation-atmosphere system (SVAT). The model
is intended for calculations of evapotranspiration, soil water and heat content, latent and sensible heat fluxes, and other
water and heat balance components. The abilities to compute these parameters using the satellite estimations of the leaf area
index and projective vegetation cover fraction as the model parameters and LST satellite estimations as the model input variable
are investigated. 相似文献
16.
内蒙古植被NDVI变化特征分析 总被引：2，自引：0，他引：2
对植被状况和植被覆盖的研究可以反映植被受环境条件影响产生的时空变化。文章根据GIMMS-NDVI数据集1982—2006年影像数据,分析内蒙古农田、森林、草原三种植被类型NDVI年内、年际的变化趋势以及植被覆盖变化特征的空间差异。各植被类型变化曲线都呈现4—7月NDVI激增,8—10月NDVI猛降,冬季农田、草原植被覆盖接近裸土的特点。农田夏季NDVI平均值的历年线性变化趋势通过显著性检验,森林夏季NDVI平均值呈现下降的趋势,草原夏季NDVI平均值呈现上升的趋势,但都不显著。 相似文献
17.
Evaluating the Dependence of Vegetation on Climate in an Improved Dynamic Global Vegetation Model 总被引：2，自引：0，他引：2
ZENG Xiaodong 《大气科学进展》2010,27(5):977-991
The capability of an improved Dynamic Global Vegetation Model (DGVM) in reproducing the impact of climate on the terrestrial ecosystem is evaluated. The new model incorporates the Community Land ModelDGVM (CLM3.0-DGVM) with a submodel for temperate and boreal shrubs, as well as other revisions such as the two-leaf scheme for photosynthesis and the definition of fractional coverage of plant functional types (PFTs). Results show that the revised model may correctly reproduce the global distribution of tempera... 相似文献
18.
Summary A network of ground-based Global Positioning System (GPS) receivers is used to continuously obtain information on variations
in the integrated water vapor (IWV) in the atmosphere. We use GPS data from 1996–1998 to compare the IWV estimates with radiosonde
data. The spatial correlation of estimation errors is important when the GPS results are to be used in assimilation models.
We study and model this effect by comparing the horizontal correlations of the IWV time series derived from the radiosonde
network and the GPS data analysis. Under ideal conditions this method separates the IWV features from the underlying correlation
function for the estimation errors in the GPS data. A sparse radiosonde network limits the quality of the obtained results.
We foresee continued studies including more data and simulations of the errors associated with the GPS technique.
Received November 21, 2000 Revised April 2, 2001 相似文献
19.
The role of vegetation feedbacks for the process of ice-sheet evolution could potentially be important in realistically modeling the past and future evolution of the Greenland ice-sheet. We use a fully coupled atmosphere–ocean model to assess the response of the climate when the Greenland ice-sheet is replaced with a number of fixed vegetation types (bare soil, broadleaf and needleleaf trees, C3 and C4 grasses and shrubs) in conjunction with loaded and unloaded bedrock orography. These sensitivity experiments show that albedo changes dominate the climate response during the summer months while temperature changes during winter are attributed to altitude change and changes in atmospheric circulation over Greenland. Snow-free summers occur for all fixed vegetation types, except for high altitude eastern regions for bare soil. We perform further simulations with dynamic vegetation resulting in dominant shrub coverage over central and southern Greenland with grasses supported in the north. Ice-sheet modeling shows significant regrowth of the Greenland ice-sheet can occur for a bare soil surface type, dependent on ice-sheet model parameters, while Greenland remains almost ice-free for needleleaf tree coverage. Furthermore, a realistically vegetated Greenland can only support a small amount of ice-sheet regrowth implying multi-stability of the Greenland ice-sheet under a preindustrial climate. This study highlights the importance of considering vegetation climate ice-sheet interactions, and uncertainty in ice-sheet model parameters. 相似文献