Quisition program within the towers are shown in Table 1. Height in the Ground (m) Equipment Description VariableFMI BPE Table 1. Description of the gear usedNE, USA incident solar radiation (Rgi), reflected solar to measure Rgi/Rgr LI200X, LI-COR, Lincoln, 5 20 radiation (Rgi), net radiation (Rn), soil heat flux (G), air temperature (Ta), relative humidity (RH), Rn NRLITE, Kipp Zonen, Delft, The Netherlands 5 20 wind speed HFP01, Hukseflux BV, Delft, The Netherlands the Fazenda Miranda (FMI) and Ba das (u), datalogger, and their respective heights in G -0.05 -0.05 Ta/RH Pedras (BPE) flux towers. Vaisala Inc., Woburn, USA HMP-45AC, 58 221 u 014A, Met One particular, Grants Pass, USA 5 22 Installation Height Datalogger CR1000, Campbell Scientific, Inc., Logan, USAfrom the Ground (m) FMI BPE The SEBFs and ET in the two flux towers have been calculated working with the Bowen ratio energy Rgi/Rgr balance (BREB) strategy using the sensor listed in Table 1.5This method has been extensively LI200X, LI-COR, Lincoln, NE, USA 20 Rn applied and has the benefit of requiring few micrometeorological20 NRLITE, Kipp Zonen, Delft, Netherlands five parameters though G havingHFP01,physical basis [1,39]. Furthermore, comparisons between estimates obtained Hukseflux BV, Delft, Netherlands -0.05 -0.05 a firm Ta/RH by the BREB and also the extra directWoburn, USA HMP-45AC, Vaisala Inc., eddy covariance approach provide221 information, which 58 comparable u 014A, Met One particular, Grants Pass, environmental research in remote and logistically five 22 tends to make the MRB a fantastic process forUSA difficult Campbell as the Cerrado-Pantanal Datalogger CR1000,locations, suchScientific, Inc., Logan, USAecotone [1,39]. The calculation with the SEBFs and ET is described in detail in [1]. The SEBFs and ET in the two flux towers have been calculated using the Bowen ratio power balance (BREB) approach applying the sensor listed in Table 1. This method has been extensively applied and has the benefit of requiring few micrometeorological parameters Variable Equipment DescriptionSensors 2021, 21,5 of2.three. Remote Sensing Information The study was carried out with information and pictures obtained amongst 2013 and 2016 making use of 27 pictures of surface reflectance and brightness temperature in the Operational Land Imager (OLI) plus the Thermal Infrared Sensor (TIRS) sensors, respectively, from Landsat eight in path 226 and row 71, and 10 photos of surface reflectance on the MOD09A1 item in the MODIS sensor around the TERRA satellite had been downloaded from the EROS Science Processing Architecture (ESPA) [espa.cr.usgs.gov accessed on 25 April 2020] of the US Geological Survey (USGS). The OLI sensor photos are composed of 9 bands, with spatial resolutions of 30 m for bands 1 and 9, and 15 m for band eight (panchromatic). The photos in the TIRS sensor are composed of bands ten and 11, with spatial resolution of 90 m. The temporal resolution with the Landsat 8 satellite is 16 days along with the radiometric resolution is 16 bits [42]. The photos in the surface reflectance without having the impact of the atmosphere had been processed by the Landsat Ecosystem Disturbance Adaptive Processing Technique (LEDAPS) hosted on the ESPA platform. LEDAPS is usually a complex algorithm that integrates GYKI 52466 Autophagy internal sensor information (metadata) with external information (NCEP, NOAA, and NASA) to (i) GNE-371 Biological Activity transform the digital quantity to prime of atmosphere (TOA) reflectance; (ii) detect pixels with clouds from TOA reflectance and; and (iii) calculate the corrected surface reflectance in the TOA reflectance [43]. The atmospheric correction of your surfac.
