File Download
There are no files associated with this item.
Links for fulltext
(May Require Subscription)
- Publisher Website: 10.1016/S0034-4257(96)00179-4
- Scopus: eid_2-s2.0-0031148946
- Find via
Supplementary
-
Citations:
- Scopus: 0
- Appears in Collections:
Article: Calculations of the soil hot-spot effect using the coherent backscattering theory
| Title | Calculations of the soil hot-spot effect using the coherent backscattering theory |
|---|---|
| Authors | |
| Issue Date | 1997 |
| Citation | Remote Sensing of Environment, 1997, v. 60, n. 2, p. 163-173 How to Cite? |
| Abstract | The shadowing theory has been widely used to account for the hot-spot effect for the canopy and soil. However, it is not valid for soils that are composed of fine particles and do not have well-defined shadows. The coherent backscattering is used in this study to calculate both the magnitude and the angular width of the hot-spot peak for clay and silt soils. The soil hot-spot magnitude is calculated by solving the vector radiative transfer equation. The dense nature of the soil medium is taken into account in the calculations of the hot-spot angular width. The results are also linked with the Hapke hot-spot empirical function. The effects of the wavelength dependence and of particle size and shape also are examined. |
| Persistent Identifier | http://hdl.handle.net/10722/321242 |
| ISSN | 2023 Impact Factor: 11.1 2023 SCImago Journal Rankings: 4.310 |
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Liang, Shunlin | - |
| dc.contributor.author | Mishchenko, Michael I. | - |
| dc.date.accessioned | 2022-11-03T02:17:36Z | - |
| dc.date.available | 2022-11-03T02:17:36Z | - |
| dc.date.issued | 1997 | - |
| dc.identifier.citation | Remote Sensing of Environment, 1997, v. 60, n. 2, p. 163-173 | - |
| dc.identifier.issn | 0034-4257 | - |
| dc.identifier.uri | http://hdl.handle.net/10722/321242 | - |
| dc.description.abstract | The shadowing theory has been widely used to account for the hot-spot effect for the canopy and soil. However, it is not valid for soils that are composed of fine particles and do not have well-defined shadows. The coherent backscattering is used in this study to calculate both the magnitude and the angular width of the hot-spot peak for clay and silt soils. The soil hot-spot magnitude is calculated by solving the vector radiative transfer equation. The dense nature of the soil medium is taken into account in the calculations of the hot-spot angular width. The results are also linked with the Hapke hot-spot empirical function. The effects of the wavelength dependence and of particle size and shape also are examined. | - |
| dc.language | eng | - |
| dc.relation.ispartof | Remote Sensing of Environment | - |
| dc.title | Calculations of the soil hot-spot effect using the coherent backscattering theory | - |
| dc.type | Article | - |
| dc.description.nature | link_to_subscribed_fulltext | - |
| dc.identifier.doi | 10.1016/S0034-4257(96)00179-4 | - |
| dc.identifier.scopus | eid_2-s2.0-0031148946 | - |
| dc.identifier.volume | 60 | - |
| dc.identifier.issue | 2 | - |
| dc.identifier.spage | 163 | - |
| dc.identifier.epage | 173 | - |