Retrieval of the surface reflectance is important in the remotely sensed data analysis to obtain the atmospheric reflectance or atmospheric correction. The relationship between visible and mid infrared reflectance over land was investigated and developed in this study. The surface reflectances of the two visible bands were measured using a handheld spectroradiometer collected around Penang Isla...

Tian et al., (2004a), Oleson et al., (2003), and Tian et al., (2004b) recently identified significant differences between the current land surface parameters of the Community Land Model (CLM) used with the Community Climate System Model (CCSM), and global land surface descriptions from Moderate Resolution Imaging Spectroradiometer (MODIS) satellite mapping. Specifically these investigations ide...

Based on surface energy balance and the assumption of fairly invariant evaporative fraction (EF) during daytime, this study proposes a new parameterization scheme of directly estimating daily EF. Daily EF is parameterized as a function of temporal variations in surface temperature, air temperature, and net radiation. The proposed EF parameterization scheme can well reproduce daily EF estimates ...

     Temperature is considered as the basic element of climate and also the environmental limiting factor in LutDesert. In this research, in order to identify the temperature of Lut Desert located in east of central Iran, using remote sensing data, six series of MODIS sensor images related to June 24th & December 23rd 2002, and also January 22nd, March 22nd, June 22nd & September 24th 2003 were...

In this study, the Visible Infrared Imager Radiometer Suite (VIIRS) Land Surface Temperature (LST) Environmental Data Record (EDR) was evaluated against snow surface (T-skin) and near-surface air temperature (T-air) ground observations recorded at the Cooperative Remote Sensing Science and Technology Center—Snow Analysis and Field Experiment (CREST-SAFE), located in Caribou, ME, USA during the ...

Under simplifying conditions catchment-scale vapor pressure at the drying land surface can be calculated as a function of its watershed-representative temperature () by the wet-surface equation (WSE, similar to the wet-bulb equation in meteorology for calculating the dry-bulb thermometer vapor pressure) of the Complementary Relationship of evaporation. The corresponding watershed ET rate, <...

1 Assessing species composition and its changes through time across broad 2 geographic regions are time consuming and difficult endeavors. The synoptic view 3 provided by imaging remote sensors offers an alternative. But while many studies have 4 developed procedures for assessing biodiversity using multiand hyper-spectral imagery, 5 they may only provide snapshots at particular months/seasons ...

The MODIS Rapid Response (RR) System was developed to meet the near real time needs of the applications community. Generally, its products are available online within hours of the satellite overpass. We recently adapted the standard MODIS land surface temperature (LST) splitwindow algorithm for use in the RR System. To minimize latency, we eliminated the algorithm's dependency on upstream MODIS...