| dc.contributor.author | Alavipanah, S. | en_US |
| dc.contributor.author | Shamsipour, A. | en_US |
| dc.contributor.author | Jafer Beglo, M. | en_US |
| dc.date.accessioned | 1399-07-09T11:01:04Z | fa_IR |
| dc.date.accessioned | 2020-09-30T11:01:04Z | |
| dc.date.available | 1399-07-09T11:01:04Z | fa_IR |
| dc.date.available | 2020-09-30T11:01:04Z | |
| dc.date.issued | 2005-12-01 | en_US |
| dc.date.issued | 1384-09-10 | fa_IR |
| dc.date.submitted | 2014-07-02 | en_US |
| dc.date.submitted | 1393-04-11 | fa_IR |
| dc.identifier.citation | Alavipanah, S., Shamsipour, A., Jafer Beglo, M.. (2005). DIURNAL BEHAVIOR OF LAND SURFACE TEMPERATURE IN LUT DESERT. Desert, 10(1), 19-28. doi: 10.22059/jdesert.2005.31878 | en_US |
| dc.identifier.issn | 2008-0875 | |
| dc.identifier.issn | 475-2345X | |
| dc.identifier.uri | https://dx.doi.org/10.22059/jdesert.2005.31878 | |
| dc.identifier.uri | https://jdesert.ut.ac.ir/article_31878.html | |
| dc.identifier.uri | https://iranjournals.nlai.ir/handle/123456789/393336 | |
| dc.description.abstract | analyses and thermal infrared channels 4 and 5 NOAA- AVHRR images. <br />This research was carried out in Lut Desert located in center of sub-tropical divergence dominant in' Iranian <br />plateau. The physical and thermal properties of the various desert surfaces have been determined using <br />correlation relationships between the desert variables including: dark sand, normal sand, marl, saline soil, soil <br />depth (10 cm), wet and dry bulb temperature in daytimes with the interval of two hours from 6 AM to 20 P.M <br />within 15 days. <br />The result shows that thermal conductivity, thermal capacity, physico-chemical properties of the studied <br />materials and other thermal properties, are the most important factors affecting correlation coefficients. The <br />highest correlation obtained around the sunrise (6 AM) and especially before and after the sunset (18, 20 <br />P.M). Minimum correlations were obtained around the noon at soil depth and the best fitted models are linear <br />for light sand and marl in 18, 20 P.M and non-linear for soil depth and marl in 18 P.M. Therefore it is generally <br />concluded that the study of diurnal behavior of land surface temperatures might be useful for thermal image <br />interpretation. | en_US |
| dc.format.extent | 701 | |
| dc.format.mimetype | application/pdf | |
| dc.language | English | |
| dc.language.iso | en_US | |
| dc.publisher | University of Tehran | en_US |
| dc.relation.ispartof | Desert | en_US |
| dc.relation.isversionof | https://dx.doi.org/10.22059/jdesert.2005.31878 | |
| dc.title | DIURNAL BEHAVIOR OF LAND SURFACE TEMPERATURE IN LUT DESERT | en_US |
| dc.type | Text | en_US |
| dc.contributor.department | Associate Prof,Faculty of Geography,University of Tehran | en_US |
| dc.contributor.department | Ph.D. Canditate,Faculty of Geography,University of Tehran | en_US |
| dc.contributor.department | Associate Prof,Faculty of Geography.University of Tehran | en_US |
| dc.citation.volume | 10 | |
| dc.citation.issue | 1 | |
| dc.citation.spage | 19 | |
| dc.citation.epage | 28 | |