DocumentCode :
1756657
Title :
Multitemporal Fluctuations in L-Band Backscatter From a Japanese Forest
Author :
Watanabe, Manabu ; Motohka, Takeshi ; Shiraishi, Tomohiro ; Thapa, Rajesh Bahadur ; Yonezawa, Chinatsu ; Nakamura, Kazuki ; Shimada, Masanobu
Author_Institution :
Japan Aerosp. Exploration Agency/Earth Obs. Res. Center, Ibaraki, Japan
Volume :
53
Issue :
11
fYear :
2015
fDate :
Nov. 2015
Firstpage :
5799
Lastpage :
5813
Abstract :
The temporal variations (diurnal and annual) in arboreal (εTree) and bare soil (εSoil) dielectric constants and their correlation with precipitation were examined for several trees in Japan. A significant (1 σ (standard deviation) and 2 σ) εTree increase is observed after rainfall at 89.8% and 90.5% probability. However, rainfall does not always induce significant εTree increases. Rainfall of more than 5 mm/day can induce 1 σ εTree Tree increase at a 59.6% probability. In order to examine whether the increase in εTree affects the L-band σ0 variation in a forest, the four-year temporal variation of the L-band backscattering coefficient (σ0) was estimated from observations by the Advanced Land Observing Satellite Phased Array type L-band Synthetic Aperture Radar. Observed maximum absolute deviations from the mean over the forest area were 1.0 and 1.2 dB for σHH0 and σHV0, respectively, and 4.0 and 3.0 dB over open land. σ0 and rainfall correlations show that εTree and σForest0 are proportional to precipitation integrated over seven or eight days; εSoil and σOpen land0 are proportional to precipitation integrated over three days. This finding indicates that εTree variations influence σForest areas0. A stronger correlation between σHV0 and precipitation is observed in several sites with low σHV0, where less biomass is expected, and several sites with high σHV0, where more biomass is expected. A weaker correlation between σHV0 and precipitation is observed for several - ites with high σHV0. These differences may be explained by the different contributions of double bounce scattering and potential transpiration, which is a measure of the ability of the atmosphere to remove water from the surface through the processes of transpiration. The two other results were as follows: 1) The functional relation between aboveground biomass and σ0 showed dependence on precipitation data, this being an effect connected with seasonal changes of the εTree. This experiment reinforces the fact that the dry season is preferable for retrieval of woody biomass from inversion of the functional dependence of SAR backscatter and for avoiding the influence of rainfall. 2) The complex dielectric constant for a tree trunk, which is measured between 0.2 and 6 GHz, indicates that free water is dominant in the measured tree.
Keywords :
remote sensing by radar; synthetic aperture radar; vegetation; vegetation mapping; Advanced Land Observing Satellite Phased Array type L-band SAR; Japanese forest; L-band backscattering coefficient; L-band sigma variation; Synthetic Aperture Radar; aboveground biomass; arboreal soil; bare soil; complex dielectric constant; dielectric constants; double bounce scattering; multitemporal fluctuations; potential transpiration; precipitation data; Biomass; Dielectric constant; Dielectric measurement; L-band; Probes; Soil measurements; Vegetation; Biomass; Phased Array type L-band Synthetic Aperture Radar (PALSAR); dielectric constant; forest; temporal variation;
fLanguage :
English
Journal_Title :
Geoscience and Remote Sensing, IEEE Transactions on
Publisher :
ieee
ISSN :
0196-2892
Type :
jour
DOI :
10.1109/TGRS.2015.2415832
Filename :
7118692
Link To Document :
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