By utilizing the data observed at Dunhuang during August and September 2000 in the 'Field Experiment on Interaction between Land and Atmosphere in the Arid Region of Northwest China (FEILARNC)', the characteri...By utilizing the data observed at Dunhuang during August and September 2000 in the 'Field Experiment on Interaction between Land and Atmosphere in the Arid Region of Northwest China (FEILARNC)', the characteristics of the soil moisture, temperature, and atmospheric humidity are analyzed. It is found that the thickness of the soil temperature active layer is about 5 cm and much thinner than is typical, that not only the atmospheric humidity gradient is often inverted but also the soil moisture gradient in the shallow layer in the Gobi near oasis, that the diurnal variation of soil moisture can be divided into the four stages that are called the wet stage, the losing-water stage, the dry stage, and the attaining-water stage. It is shown that in soil moisture profiles, the depth of the soil moisture active layer is about 10 cm and soil moisture inversion is the main feature in the shallow layer during the wet stage. Such a feature as soil moisture inversion indicates that soil in the shallow layer can inhale moisture from the air through condensation in the nighttime and exhale moisture to the air through evaporation in the daytime. The condensation and evaporation constitute together the full respiration process of moisture on the ground. The formation of soil moisture inversion is related with the state of soil temperature and moisture, the intensity of atmospheric humidity inversion, and the atmospheric thermodynamic stability.展开更多
The reliability of the model-based decomposition result,which is seldom investigated,is a key factor in determining whether decomposition parameters can be effectively applied to polarimetric synthetic aperture radar(...The reliability of the model-based decomposition result,which is seldom investigated,is a key factor in determining whether decomposition parameters can be effectively applied to polarimetric synthetic aperture radar(PolSAR)applications.In this paper,a type of polarimetric parameter for evaluating the reliability of model-based decomposition result is proposed.It originates from the degree of correlation between the scattering models.The main idea is whether the measured power can be assigned to the corresponding scattering model.The more the measured power that can be allocated to the corresponding scattering model,the more reliable the decomposition result.The C-band Radarsat-2,L-band UAVSAR,X-band TerraSAR-X,and L-band E-SAR PolSAR data are selected for experiments.The results show that the type of polarimetric parameter can effectively represent the reliability of the decomposition result.The reliabilities of surface and double-bounce scattering are high in the ocean and orthogonal buildings,respectively.For oriented buildings,the reliability of the decomposition result is lower owing to the overestimation of volume scattering.For forested areas,reliability is generally higher if volume scattering is not overestimated.Furthermore,the results show that the reliability of soil moisture retrieval is positively correlated with surface scattering reliability.展开更多
基金the National Nat-ural Science Foundation of China(No.40175004)and theNational Key Program for Developing Basic Sciences ofChina(No.G1998040904-2).
文摘By utilizing the data observed at Dunhuang during August and September 2000 in the 'Field Experiment on Interaction between Land and Atmosphere in the Arid Region of Northwest China (FEILARNC)', the characteristics of the soil moisture, temperature, and atmospheric humidity are analyzed. It is found that the thickness of the soil temperature active layer is about 5 cm and much thinner than is typical, that not only the atmospheric humidity gradient is often inverted but also the soil moisture gradient in the shallow layer in the Gobi near oasis, that the diurnal variation of soil moisture can be divided into the four stages that are called the wet stage, the losing-water stage, the dry stage, and the attaining-water stage. It is shown that in soil moisture profiles, the depth of the soil moisture active layer is about 10 cm and soil moisture inversion is the main feature in the shallow layer during the wet stage. Such a feature as soil moisture inversion indicates that soil in the shallow layer can inhale moisture from the air through condensation in the nighttime and exhale moisture to the air through evaporation in the daytime. The condensation and evaporation constitute together the full respiration process of moisture on the ground. The formation of soil moisture inversion is related with the state of soil temperature and moisture, the intensity of atmospheric humidity inversion, and the atmospheric thermodynamic stability.
基金funded in part by the National Natural Science Foundation of China[grant numbers 41820104005,41904004,42030112,42171387,and 41804004]in part by the Fundamental Research Funds for the Central University of Central South University[grant number 2021zzts0262].
文摘The reliability of the model-based decomposition result,which is seldom investigated,is a key factor in determining whether decomposition parameters can be effectively applied to polarimetric synthetic aperture radar(PolSAR)applications.In this paper,a type of polarimetric parameter for evaluating the reliability of model-based decomposition result is proposed.It originates from the degree of correlation between the scattering models.The main idea is whether the measured power can be assigned to the corresponding scattering model.The more the measured power that can be allocated to the corresponding scattering model,the more reliable the decomposition result.The C-band Radarsat-2,L-band UAVSAR,X-band TerraSAR-X,and L-band E-SAR PolSAR data are selected for experiments.The results show that the type of polarimetric parameter can effectively represent the reliability of the decomposition result.The reliabilities of surface and double-bounce scattering are high in the ocean and orthogonal buildings,respectively.For oriented buildings,the reliability of the decomposition result is lower owing to the overestimation of volume scattering.For forested areas,reliability is generally higher if volume scattering is not overestimated.Furthermore,the results show that the reliability of soil moisture retrieval is positively correlated with surface scattering reliability.
