应用NOAA／AVHRR资料动态监测洪涝灾害的研究

以ＮＯＡＡ卫星为主要监测手段,对洪水、植被、土壤的光谱特征进行分析研究,提出了同时突出水体和植被的光谱分析思路。并根据客观分析需要,建立了洪涝灾情图像处理软件系统,对ＮＯＡＡ／ＡＶＨＲＲ图像资料进行投影、截取、放大、配准等一系列预处理。同时采用模糊非监督分类、比值、归一化植被指数方法对洪涝信息进行分析处理,确定受灾范围,量算受灾面积,划分受灾等级,提供灾情分布图,为防汛抗洪部门提供有力的科学依据。     

基于NOAA／AVHRR数据的景观格局分析——以塔里木河干流区域为例

在对NOAA／AVHRR数据进行灰度拉伸,直方图均衡化,多通道合成等方法处理后,应用IDRISI软件的空间分析功能,对塔里木河流域进行了景观格局的宏观分析,结果表明在塔里木河干流区城景观类型相对简单,各景观自身破碎度低,连通性较好,景观间的均匀度差,是一种典型的脆弱的干旱区陆河流域生态环境景观。     

NOAA/AVHRR观测角影响纠正的一种方法

利用ＬａｎｄｓａｔＴＭ６热红外遥感数据定量反演了干旱地区的地表温度,研究结果表明,区典型地表覆盖类型的地表亮温比地表起初温度低０．４－１Ｋ,遥感反演的地面真实温度与当地３月下旬的实测温度误差在０．８Ｋ以下,这说明用ＬａｎｄｓａｔＴＭ６定量反演干旱区的地表温度是可行的。研究结果表明,地下水富集带地表温度具有异常现象,其地表温度比地表水体高５Ｋ左右,而比其它地表类型低７Ｋ以上,据此,可以利用热红外遥感     

基于NOAA/AVHRR热红外数据的城市热岛强度年内变化特征

采用ENVI/IDL编程技术,实现NOAA/AVHRR数据的校准、几何纠正、云污染识别与剔除、影像特征统计与输出等过程的批处理自动化操作。并以济南市中心城区为例,通过2005~2006年间获取的白天NOAA/AVHRR影像热红外波段调查了济南市区城市热岛强度的年内变化规律与过程。研究结果表明：① 济南市区全年大部分时间存在热岛现象,4~9月份城市热岛效应较为明显,尤以5、7、8月为甚。② 全年城市热岛平均强度2.77℃,最强的热岛效应出现于7月下旬至8月中旬间。③ 从季节分布来看,济南市区夏季热岛效应最明显,春季次之,秋、冬两季较弱。④ 城市热岛强度与城、郊地表温度存在正相关关系,但相关程度较差。     

太湖地区NOAA—AVHRR资料估算水稻种植面积的有效性探讨

运用NOAA-AVHRR资料估算水稻种植面积,是遥感应用领域中一个新的研究方向,结合国家“八五”攻关项目“太湖地区遥感话产”的要求,在太湖地区进行了初步的尝试:(1)根据估产精度要求和NOAA一AVHRR资料校正精度,探讨了运用NOAA一AVHRR资料估产所需的最小区域范围。(2)针对太湖地区的具休地理环境设计了提取水稻种植曲积的技术方案,并在试验区取得了初步成果。     

多时机NOAA—AVHRR数据主成分分析的生物学意义

利用多时上NOAA－AVHRR的中国归一化植被指数NDVI数据进行主成分分析,并与从NDVI派生的4个生物不数作相关分析,结果表明：主成分变换既压缩了信息,将21个月的信息主要压缩到前4个主分量,又提取了关键的变化信息,第一主分量反映基本植被覆信息,第二、第三和第四主分量反映植被季相变化信息,正是由于一年12个月的NDVI曲线反映了植被季相变化特征,使得主成分变换得到的各主分量具有一定的生物学意义,而且17种中国典型植被在这4个主分量图像上存在一定的差异性,使其具有进行较高精度土地覆盖分类的潜力。     

林火卫星遥感监测及早期报警技术研究

以我国林火发生率较高、卫星监测林火难度较大的西南林区为试验区,为大幅度提高林火报准率,开展了微机图像处理技术、地理信息系统（ＧＩＳ）、森林火灾的分布规律、ＡＶＨＲＲ林火信息提取技术和专家系统应用等研究。介绍了该项目的研究方法,叙述了研究成果的技术原理,展望了今后研究的主攻方向。     

吉林省西部区域蒸散时空变化分析

基于地表能量平衡理论,利用NOAA/AVHRR数据,采用SEBS模型,计算了研究区15年地表蒸散量,从年、季度和月等三个时间尺度对其进行时空变化分析。结果显示:(1)各年平均蒸散量相差较大,最大的是1988年,最小的是1996年;月平均蒸散量最大值出现在5月,最小值出现在12月,形成一单峰型曲线;第二季度平均蒸散量最大,第四季度最小,其分布曲线也为单峰型。(2)多年平均蒸散量的空间分布东半部明显大于西半部,最大的是扶余县,最小的是通榆县;各市县的月平均蒸散量分布仍为单峰型曲线,在5月达到最大值,12月最小,与全区的月平均蒸散量分布曲线一致;各市县第一季度和第四季度平均蒸散量相差不大,第二和第三季度相差较大,但总体分布趋势与全区一致,仍为单峰型曲线。以上结果表明:研究区区域蒸散时空分布极不均匀,强烈的蒸散作用为研究区生态环境恶化提供了有利条件。     

AVHRR数据小火点自动识别方法的研究

利用NOAA-AVHRR数据,采用多因子分析方法,通过建立小火点自动识别模型来提取小火点燃烧信息。经实验验证,该方法能较好地减少云体、裸地对火点判断的干扰,从而在一定程度上提高了对小火点的监测精度。     

森林过火面积的遥感测算方法

根据对近年来多次特大森林火灾和相应的气象卫星资料的分析,提出利用NOAA/AVHRR数据测算森林大火的过火面积的四种方法,即灰度修正像元法、植被修正像元法、坐标法和蔓延法。在GIS地面信息数据库支持下,利用这4种方法能准确、快速地计算出过火面积。经今春应急评估试运行验证,森林大火过火面积测算精度达90%。     

Atmospheric conditions for monitoring the long-term vegetation dynamics in the Amazon using normalized difference vegetation index

This study examined the effect of biomass-burning aerosols and clouds on the temporal dynamics of the normalized difference vegetation index (NDVI) exhibited by two widely used, time-series NDVI data products: the Pathfinder AVHRR land (PAL) dataset and the NASA Global Inventory Monitoring and Modeling Studies (GIMMS) dataset. The PAL data are 10-day maximum-value NDVI composites from 1982 to 1999 with corrections for Rayleigh scattering and ozone absorption. The GIMMS data are 15-day maximum-value NDVI composites from 1982 to 1999. In our analysis, monthly maximum-value NDVI was extracted from these datasets. The effects were quantified by comparing time-series of NDVI from PAL and GIMMS with observations from the SPOT/VEGETATION sensor and aerosol index data from the Total Ozone Mapping Spectrometer (TOMS), and results from radiative transfer simulation. Our analysis suggests that the substantial large-scale NDVI seasonality observed in the south and east Amazon forest region with PAL and GIMMS is primarily caused by variations in atmospheric conditions associated with biomass-burning aerosols and cloudiness. Reliable NDVI data can be typically acquired from April to July when such effects are relatively low, whereas there is a few effective NDVI data from September to December. In the central Amazon forest region, where aerosol loads are relatively low throughout the year, large-scale NDVI seasonality results primarily from seasonal variations in cloud cover. Careful treatment of these aerosol and cloud effects is required when using NDVI from PAL and GIMMS (or other source) to determine large-scale seasonal and interannual dynamics of vegetation greenness and ecosystem-atmosphere CO₂ exchange in the Amazon region.     

Landsat TM热红外遥感数据定量反演地下水富集带的温度信息——以甘肃河西地区石羊河流域为例

利用ＬａｎｄｓａｔＴＭ６热红外遥感数据定量反演了干旱地区的地表温度,研究结果表明,研究区典型地表覆盖类型的地表亮温比地表真实温度低０．４～１Ｋ,遥感反演的地面真实温度与当地３月下旬的实测温度误差在０．８Ｋ以下,这说明用ＬａｎｄｓａｔＴＭ６定量反演干旱区的地表温度是可行的。研究结果还表明,地下水富集带地表温度具有异常现象,其地表温度比地表水体高５Ｋ左右,而比其它地表类型低７Ｋ以上,据此,可以利用热红外遥感技术有效地探测干旱区地下水富集带的信息。     

Estimating evapotranspiration of European forests from NOAA-imagery at satellite overpass time: Towards an operational processing chain for integrated optical and thermal sensor data products

Evapotranspiration (ET) using the Integral NOAA-imagery processing Chain (iNOAA-Chain) is quantified by implementing visible and thermal satellite information on a regional scale. ET is calculated based on the energy balance closure principle. The combination of evaporative fraction (EF), soil heat flux and instantaneous net radiation, results in an instantaneous spatial distribution of ET values. Surface broadband albedo and land surface temperature (LST) serve to determine EF. EF is derived using four methods based on NOAA/AVHRR satellite imagery. Instantaneous evapotranspiration, i.e. at time of satellite overpass, on European continental scale with emphasis on forest stands is estimated using the iNOAA-Chain. Finally, the estimated net radiation (R_n), soil heat fluxes (G₀) and evaporative fraction and evapotranspiration at time of satellite overpass are validated against EUROFLUX site data for the growing season of 1997 (March-October). The regression line for the pooled R_n (iNOAA-Chain versus EUROFLUX) has a slope, intercept, Pearson product moment correlation coefficient (R²) and relative root mean square error (RRMSE) of respectively 0.943, 17.120, 0.926 and 5.5%. The soil heat fluxes, calculated with two approaches are not-well modelled with slopes smaller than − 3.000 and a R² in the order of zero. We observe a slight underestimation of the iNOAA Chain estimated EF. The regression line for pooled EF data for the best performing method (SPLIT-method) has a slope of 0.935, an intercept of 0.041 and the R² is 0.847. A pooled RRMSE EF value of 12.3% is found. The pooled slope, intercept, R² and RRMSE for EF derived with SORT-method 1 are respectively 0.449, 0.251, 0.043 and 65.1%, with SORT-method 2, 0.567, 0.203, 0.174 and 39.1%, and with SORT-method 3, 0.568, 0.254, 0.288, and 32.8%. Also instantaneous evapotranspiration is underestimated with a pooled RRMSE on ET of 23.4%. The regression curve of pooled ET data for the best performing method has a slope of 0.889 an intercept of 15.880 and a Pearson product moment correlation coefficient of 0.771. The other method gives a slope of 0.781, an intercept of 17.541 and a R² of 0.776. Error propagation analysis reveals that the relative error on evapotranspiration at satellite overpass time is at least 27%.