Fifth recent advances in quantitative remote sensingJosé Antonio Sobrino Rodríguez Universitat de València, 14 déc. 2018 - 481 pages
The Fifth International Symposium on Recent Advances in Quantitative Remote Sensing was held in Torrent, Spain from 18 to 22 September 2018. It was sponsored and organized by the Global Change Unit (GCU) from the Image Processing Laboratory (IPL), University of Valencia (UVEG), Spain. This Symposium addressed the scientific advances in quantitative remote sensing in connection with real applications. Its main goal was to assess the state of the art of both theory and applications in the analysis of remote sensing data, as well as to provide a forum for researcher in this subject area to exchange views and report their latest results. In this book 89 of the 262 contributions presented in both plenary and poster sessions are arranged according to the scientific topics selected. The papers are ranked in the same order as the final programme. |
À l'intérieur du livre
Résultats 1-5 sur 81
Page 10
... Average penetration depth for most of currently operated systems are in the range of 30 meters, LADS (Laser Airborne Depth Sounder) developed by Tenix LADS Corporation is an exception where penetration depth reaches 70 meters. Also ...
... Average penetration depth for most of currently operated systems are in the range of 30 meters, LADS (Laser Airborne Depth Sounder) developed by Tenix LADS Corporation is an exception where penetration depth reaches 70 meters. Also ...
Page 12
... average depth of only 11 meters and containing about 90 million cubic meters of water. The lake is surrounded by industrial workshops for shipyards, domestic areas, recreational beaches and agricultural lands. The Suez Canal pathway is ...
... average depth of only 11 meters and containing about 90 million cubic meters of water. The lake is surrounded by industrial workshops for shipyards, domestic areas, recreational beaches and agricultural lands. The Suez Canal pathway is ...
Page 14
... average solar Zenith angle S The traditional NDVI ratio will be used to generate a mask to separate the water body of the study area , as in Figure 4. C / RE , C / Y , B / Y , C / G , B / G and G / Y ratios will be used to derive ...
... average solar Zenith angle S The traditional NDVI ratio will be used to generate a mask to separate the water body of the study area , as in Figure 4. C / RE , C / Y , B / Y , C / G , B / G and G / Y ratios will be used to derive ...
Page 21
... average of 5% of uncertainty were gathered. For SWIR region both sources, environmental and instrumental rise to 12% of uncertainty. 1 INTRODUCTION In optical Earth Observation satellites, ground truth data acquired by field ...
... average of 5% of uncertainty were gathered. For SWIR region both sources, environmental and instrumental rise to 12% of uncertainty. 1 INTRODUCTION In optical Earth Observation satellites, ground truth data acquired by field ...
Page 25
... average of 5% of uncertainty were gathered. For SWIR region both sources, environmental and instrumental, reach to 12%. Only a small correlation were found between standard deviation of reference panel radiance measurement and solar ...
... average of 5% of uncertainty were gathered. For SWIR region both sources, environmental and instrumental, reach to 12%. Only a small correlation were found between standard deviation of reference panel radiance measurement and solar ...
Table des matières
RARQS2017p339 | 243 |
RARQS2017p341 | 248 |
RARQS2017p342 | 254 |
RARQS2017s1004 | 260 |
RARQS2017s105 | 265 |
RARQS2017s121 | 270 |
RARQS2017p404 | 276 |
RARQS2017p405 | 282 |
| 47 | |
| 51 | |
| 56 | |
| 61 | |
| 67 | |
| 73 | |
| 77 | |
| 82 | |
| 90 | |
RARQS2017p212 | 95 |
RARQS2017p217 | 104 |
RARQS2017p225 | 107 |
RARQS2017p226 | 112 |
RARQS2017p231 | 118 |
RARQS2017p234 | 123 |
RARQS2017p235 | 128 |
RARQS2017p241 | 138 |
RARQS2017s604 | 144 |
RARQS2017p304 | 151 |
RARQS2017p307 | 157 |
RARQS2017p308 | 162 |
RARQS2017p309 | 168 |
RARQS2017p311 | 174 |
RARQS2017p315 | 180 |
RARQS2017p318 | 186 |
RARQS2017p319 | 191 |
RARQS2017p322 | 197 |
RARQS2017p323 | 202 |
RARQS2017p324 | 206 |
RARQS2017p327 | 211 |
RARQS2017p330 | 217 |
RARQS2017p331 | 223 |
RARQS2017p332 | 227 |
RARQS2017p335 | 232 |
RARQS2017p337 | 238 |
RARQS2017p406 | 287 |
RARQS2017p407 | 292 |
RARQS2017p408 | 296 |
RARQS2017p412 | 303 |
RARQS2017p417 | 312 |
RARQS2017p420 | 318 |
RARQS2017p424 | 323 |
RARQS2017p427 | 327 |
RARQS2017p428 | 332 |
RARQS2017p434 | 337 |
RARQS2017p437 | 342 |
RARQS2017p440 | 346 |
RARQS2017p441 | 351 |
RARQS2017p501 | 356 |
RARQS2017p503 | 362 |
RARQS2017p504 | 368 |
RARQS2017p506 | 374 |
RARQS2017p508 | 379 |
RARQS2017p509 | 384 |
RARQS2017p510 | 387 |
RARQS2017p511 | 391 |
RARQS2017p512 | 396 |
RARQS2017p514 | 402 |
RARQS2017p519 | 407 |
RARQS2017p524 | 412 |
RARQS2017p525 | 418 |
RARQS2017p527 | 425 |
RARQS2017p528 | 430 |
RARQS2017p532 | 436 |
RARQS2017p535 | 443 |
RARQS2017p538 | 449 |
RARQS2017p539 | 454 |
RARQS2017p540 | 460 |
RARQS2017 | 464 |
Expressions et termes fréquents
accuracy Agricultural albedo algorithm analysis angle applications atmospheric average backscatter band Beijing brightness temperature C-band calculated calibration China classification climate coefficient comparison computed correlation crop datasets derived detection emissivity error estimation evaluate evapotranspiration FAPAR field Figure FPGA Geoscience and Remote global GNSS grass production grassland greenup date Guangxi hyperspectral IEEE imagery images infrared interpolation inversion Journal land surface temperature Landsat landslide leaf area index linear Livingston Island MAIAC mapping maximum measurements meteorological method MODIS monitoring multispectral NDVI obtained optimized parameters pixels polarization precipitation processing radar radiance radiation reflectance region Remote Sensing remote sensing data Research retrieval rice RMSE sampling satellite data scale Sciences Sensing of Environment sensor shows signal simulated soil moisture solar spatial resolution spectral study area temporal thermal infrared Tibetan Plateau trend TWSA uncertainty validation values variables variation vegetation index Zhang