| Model ID: | M00028 | ||||||
| Model Name: | DMRT-AIEM-MD | ||||||
| Encoders: |
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| Key words: | snow, DMRT, MD | ||||||
| Model Type: | theoretic model | ||||||
| Latest Modified: | 2014/7/27 0:00:00 | ||||||
| Submission Date: | 2005/9/13 0:00:00 | ||||||
| Abstract: | The matrix doubling approach is used to include multiple-scattering and combines the Dense Media Radiative | ||||||
| Equation: |
| 1 |
Name: incident angle
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Parameter type: double
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Physic Entity: incident angle
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| 2 |
Name: observing frequency
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Parameter type: double
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Physic Entity: observing frequency
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| 3 |
Name: snow depth
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Parameter type: double
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Physic Entity: snow depth
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| 4 |
Name: snow density
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Parameter type: double
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Physic Entity: snow density
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| 5 |
Name: radius
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Parameter type: double
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Physic Entity: radius of an assumed spherical particle
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| 6 |
Name: snow wetness
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Parameter type: double
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Physic Entity: Liquid water volume content in snow
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| 7 |
Name: surface root mean square height
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Parameter type: double
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Physic Entity: root mean square height of soil surface
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| 8 |
Name: surface correlation length
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Parameter type: double
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Physic Entity: correlation length of soil surface
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| 9 |
Name: soil moisture
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Parameter type: double
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Physic Entity: Liquid water volume content in soil
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| 10 |
Name: snow temperature
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Parameter type: double
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Physic Entity: ean temperature in one snow layer
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| 11 |
Name: temperature at snow-soil boundary
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Parameter type: double
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Physic Entity: temperature at snow-soil boundary
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| 12 |
Name: soil temperature
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Parameter type: double
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Physic Entity: near surface soil temperature
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| Title: | PASSIVE MICROWAVE REMOTE SENSINGOF SNOW WATER EQUIVALENCE STUDY | ||||||||||||
| Authors: |
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| Cited by: | |||||||||||||
| Abstract: | Snow is a key element in the meteorological and hydrological studies. Theamount of regional snow plays an important role in the climate change and alsoaffects greatly the development of agriculture and farming industries in arid/semi-aridareas. Seasonal snow cover and glacier are important components of global watercycling. Thus, it is necessary to monitor the seasonal snow cover, the depositing andmelting of the glacier. It will help us to acquire a more accurate understanding ofglobal water cycling. |
Equation