Remote Sensing and Spectral Characteristics of Desert Sand from Qatar Peninsula, Arabian/Persian Gulf

Remote sensing data can provide valuable information about the surface expression of regional geomorphologic and geological features of arid regions. In the present study, several processing techniques were applied to reveal such in the Qatar Peninsula. Those included preprocessing for radiometric a...

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Main Authors: Fares Howari, Abdulali Sadiq
Format: Article
Language:English
Published: MDPI AG 2009-11-01
Series:Remote Sensing
Subjects:
Online Access:http://www.mdpi.com/2072-4292/1/4/915/
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spelling doaj-3d13751adcf14893ae79271c25483ab92020-11-24T22:21:36ZengMDPI AGRemote Sensing2072-42922009-11-011491593310.3390/rs1040915Remote Sensing and Spectral Characteristics of Desert Sand from Qatar Peninsula, Arabian/Persian GulfFares HowariAbdulali SadiqRemote sensing data can provide valuable information about the surface expression of regional geomorphologic and geological features of arid regions. In the present study, several processing techniques were applied to reveal such in the Qatar Peninsula. Those included preprocessing for radiometric and geometric correction, various enhancement methods, classification, accuracy assessment, contrast stretching, color composition, and principal component analyses. Those were coupled with field groundtruthing and lab analyses. Field groundtruthing included one hundred and forty measurements of spectral reflectance for various sediment exposures representing main sand types in the four studied parts in Qatar. Lab investigations included grain size analysis, X-ray diffraction and laboratory measurements of spectral reflectance. During the course of this study three sand types have been identified: (i) sabkha-derived salt-rich, quartz sand, and (ii) beach-derived calcareous sand and (iii) aeolian dune quartz. Those areas are spectrally distinct in the VNIR, suggesting that VNIR spectral data can be used to discriminate them. The study found that the main limitation of the ground spectral reflectance study is the difficulty of covering large areas. The study also found that ground and laboratory spectral radiance are generally higher in reflectance than those of Landsat TM. This is due to several factors such as atmospheric conditions, the low altitude or different scales. Whereas for areas with huge size of dune sand, the Landsat TM spectral has higher reflectance than those from field and laboratory. The study observed that there is a good correspondence or correlation of the wavelengths maximum sensitivity between the three spectral measurements i.e lab, field and space-borne measurements. http://www.mdpi.com/2072-4292/1/4/915/QatarLandsatsand dunesspectral reflectancequaternary geology
collection DOAJ
language English
format Article
sources DOAJ
author Fares Howari
Abdulali Sadiq
spellingShingle Fares Howari
Abdulali Sadiq
Remote Sensing and Spectral Characteristics of Desert Sand from Qatar Peninsula, Arabian/Persian Gulf
Remote Sensing
Qatar
Landsat
sand dunes
spectral reflectance
quaternary geology
author_facet Fares Howari
Abdulali Sadiq
author_sort Fares Howari
title Remote Sensing and Spectral Characteristics of Desert Sand from Qatar Peninsula, Arabian/Persian Gulf
title_short Remote Sensing and Spectral Characteristics of Desert Sand from Qatar Peninsula, Arabian/Persian Gulf
title_full Remote Sensing and Spectral Characteristics of Desert Sand from Qatar Peninsula, Arabian/Persian Gulf
title_fullStr Remote Sensing and Spectral Characteristics of Desert Sand from Qatar Peninsula, Arabian/Persian Gulf
title_full_unstemmed Remote Sensing and Spectral Characteristics of Desert Sand from Qatar Peninsula, Arabian/Persian Gulf
title_sort remote sensing and spectral characteristics of desert sand from qatar peninsula, arabian/persian gulf
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2009-11-01
description Remote sensing data can provide valuable information about the surface expression of regional geomorphologic and geological features of arid regions. In the present study, several processing techniques were applied to reveal such in the Qatar Peninsula. Those included preprocessing for radiometric and geometric correction, various enhancement methods, classification, accuracy assessment, contrast stretching, color composition, and principal component analyses. Those were coupled with field groundtruthing and lab analyses. Field groundtruthing included one hundred and forty measurements of spectral reflectance for various sediment exposures representing main sand types in the four studied parts in Qatar. Lab investigations included grain size analysis, X-ray diffraction and laboratory measurements of spectral reflectance. During the course of this study three sand types have been identified: (i) sabkha-derived salt-rich, quartz sand, and (ii) beach-derived calcareous sand and (iii) aeolian dune quartz. Those areas are spectrally distinct in the VNIR, suggesting that VNIR spectral data can be used to discriminate them. The study found that the main limitation of the ground spectral reflectance study is the difficulty of covering large areas. The study also found that ground and laboratory spectral radiance are generally higher in reflectance than those of Landsat TM. This is due to several factors such as atmospheric conditions, the low altitude or different scales. Whereas for areas with huge size of dune sand, the Landsat TM spectral has higher reflectance than those from field and laboratory. The study observed that there is a good correspondence or correlation of the wavelengths maximum sensitivity between the three spectral measurements i.e lab, field and space-borne measurements.
topic Qatar
Landsat
sand dunes
spectral reflectance
quaternary geology
url http://www.mdpi.com/2072-4292/1/4/915/
work_keys_str_mv AT fareshowari remotesensingandspectralcharacteristicsofdesertsandfromqatarpeninsulaarabianpersiangulf
AT abdulalisadiq remotesensingandspectralcharacteristicsofdesertsandfromqatarpeninsulaarabianpersiangulf
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