Table 2-2. Optimal SAR Parameters for Land Surface Applications

APPLICATION AREA


PARAMETER

 

RADAR FREQUENCY

POLARIZATION

INCIDENCE

ANGLE

RESOLUTION

SAMPLING

FREQUENCY

Vegetation Mapping

best results achieved if multiple frequencies are available; as a minumum, need two frequencies, one high and one low, e.g., L and C-band

important parameter in classification especially for single frequency systems

both low (20š to 40š) and high (40š to 60š) are desired

high resolutions are desirable for mapping smaller sampling units

higher sampling frequencies (greater than once every 2 weeks) not required for mapping purposes when multiple-channels are available, may improve classification for single-channel systems

Crop Monitoring

multiple frequencies are not always required, especially if multi-date data are used in classification

important parameter in classification especially for single frequency systems, not always necessary

lower angles (20š to 40š) are desired

higher resolutions are required for discrimination of small fields

higher sampling frequencies (greater than once per week) important for monitoring crop phenology and status and for improving classification accuracies

Biomass Estimation

L- or P-band are required but multiple frequencies are needed to develop best algorithms; as a minimum, L- and C-band are required

cross polarization data have most sensitivity to biomass variations; multi-polarization systems improve biomass algorithms

lower angles (20š to 35š) are required

for studying biomass dynamics in small forest stands, finer resolutions are required; for large area study, coarser resolutions can be used

high sampling frequencies are not required; sampling at proper phenologic stage and under optimum weather conditions is important

Monitoring Flooded Forests

L- and P-band are optimum, but some sensitivity at C-band if few leaves are present and HH polarization used

polarization very important for community discrimination; HH polarization most sensitive, HV and VV polarization can be important

lower angles (20š to 40š) are needed for maximum sensitivity to flooding

higher resolutions may not be as important as a high sampling frequency, but are important for mapping narrow features

high sampling frequencies usually important

 

 

 

Table 2-2 cont'd pg 2-15

Table 2-2 (continued). Optimal SAR Parameters for Land Surface Applications (continued)

APPLICATION AREA


PARAMETER

 

RADAR FREQUENCY

POLARIZATION

INCIDENCE

ANGLE

RESOLUTION

SAMPLING

FREQUENCY

Monitoring Coastal/ Low Stature Wetlands

X and C-band are required

for discrimination of different vegetation types, multiple polarizations are required; use HH or VV for monitoring inundation

intermediate angles (30š to 40š) are desired

high resolution is required in some cases

higher sampling frequencies are required for monitoring flooding dynamics; multi-temporal data can improve classification accuracy

Monitoring Tundra Inundation

X and C-band are required

for discrimination of different vegetation types, multiple polarizations are required; use HH or VV for monitoring inundation

lower angles (20š to 40š) are desired

high resolution is required in some cases

higher sampling frequencies required for monitoring flooding dynamics; multi-temporal data improves classification accuracy

Monitoring Fire-Disturbed

Boreal Forests

X and C-band are optimum, multiple frequencies improve monitoring of burn severity

polarization not important for relative soil moisture monitoring, but very important in moisture estimation and monitoring severity of burns

lower angles desired (20š to 40š) but may not be necessary

high resolution is not required

high sampling frequencies required for monitoring seasonal variations in soil moisture

Detection of Frozen/Thawed Vegetation

can be detected at both low and high radar frequencies; L-band data may be more effective; multiple-frequencies may be required to differentiate vegetation thawing from variations in surface moisture

polarization may be important to differentiate vegetation thawing from variations in surface moisture

incidence angle not a critical parameter

high resolution is not required if high resolution vegetation map available

high sampling frequencies required