Mapping wetland areas on forested landsacpes using Radarasat-2 and Landsat-5 TM data

Wetlands are an important ecosystem for many vital functions such as groundwater recharge, flood control, water quality improvement, and to mitigate erosion. Monitoring and mapping wetlands on a large scale is becoming increasingly more important, and satellite remote sensing provides a practical approach. This study examines the potential for using multi-beam Radarsat-2 C-band polarimetric SAR, Landsat-5 TM, and DEM data for classifying wetland and non-wetland classes in a forested watershed in Ontario, Canada. It investigates the influence of incidence angle, leaf presence and moisture conditions in the classification of SAR images. The images were classified using two classification methods: the Maximum Likelihood Classifier and Random Forests classifier. Lastly, SAR polarimetric variables and decompositions were investigated for their usefulness in classification. Fourteen Radarsat-2 Fine Quad (FQ) SAR images were acquired from October 2010 to November 2011 at different incidence angles but with the same orbit-descending pass (west-looking direction). The images were paired according to the beam mode (FQ4 and FQ22/27), leaf presence (off and on) and moisture (wet/dry) conditions. The FQ image pair which gave the best classification overall accuracy (76.3%) using the Maximum Likelihood classification was those from the two FQ22/27 images acquired under leaf-off and dry conditions. When the FQ images were classified together with five optical bands of a Landsat image, the classification accuracy was higher for all classes as well as for the overall accuracy (94.4%). When the FQ images were combined with the Landsat image and slope, overall accuracy improved only slightly from the FQ and Landsat combination (95.4%). With the Random Forests classification, the best overall accuracy was obtained with the combination of the FQ 22/27 image pair acquired under leaf-off and dry image conditions, Landsat and slope (98.7%), followed closely by the FQ pair and Landsat combination (98.6%). When all FQ images were used as input to the Random Forests classification, this also produced high cross-validation overall accuracies (98.3%), indicating that while Landsat does add accuracy FQ images can give comparable accuracies if the right dates and conditions are chosen. A benefit of using Random Forests is the ability to rank band importance in image classification. From this it was determined that using multiple FQ images with leaf-off conditions were preferred. As for the other conditions, a mix of incidence angles, moisture conditions, and polarizations were important for classification. The incoherent target decompositions were the most important polarimetric variable in the classification, while the only other parameter indicated as important from both classifications was the orientation angle for the maximum of the completely polarized component. In future studies, it may be of interest to test the combination of multi-date polarimetric variables and decompositions parameters together with all polarizations (HH, HV, VH, and VV). So far, we classified only two types of wetlands (closed and open). Further studies are needed to test the Random Forests classifier for classifying the wetlands into more detailed classes (bog, fen, marsh, swamp, etc.). Lastly, future studies should test the results found here using independent evaluation data to assess the accuracy

Influence of Incidence Angle in the Correlation of C-band Polarimetric Parameters with Biophysical Variables of Rain-fed Crops

A multi-temporal field experiment was conducted within the Soil Measurement Stations Network of the University of Salamanca (REMEDHUS) in Spain in order to retrieve useful crop information. The objective of this research was to evaluate the potential of polarimetric observations for crop monitoring by exploiting a time series of 20 quad-pol RADARSAT-2 images at different incidence angles (i.e. 25°, 31°, and 36°) during an entire growing season of rain-fed crops, from February to July 2015. The time evolution of 6 crop biophysical variables was gathered from the field measurements, whereas 10 polarimetric parameters were derived from the images. Thus, a subsequent correlation analysis between both datasets was performed. The study demonstrates that the backscattering ratios (HH/VV and HV/VV), the normalized correlation between HH and VV (γHHVV), and the dominant alpha angle (α1), showed significant and relevant correlations with several biophysical variables such as biomass, height, or leaf area index (LAI) at incidence angles of 31° or 36°. The joint use of data acquired with different beams could be exploited effectively to increase the refresh rate of information about crop condition with respect to a single incidence acquisition scheme.This study was supported by the Spanish Ministry of Economy and Competitiveness and the Spanish Ministry of Science, Innovation and Universities, [Projects ESP2015-67549-C3-3, ESP2017-89463-C3-3-R, and TEC2017-85244-C2-1-P] and the European Regional Development Fund (FEDER)

Analyse des signaux radars polarimétriques en bandes C et L pour le suivi de l'humidité du sol de sites forestiers

Résumé : Dans les couverts forestiers, le suivi de l’humidité du sol permet de prévenir plusieurs désastres tels que la paludification, les incendies et les inondations. Comme ce paramètre est très dynamique dans l’espace et dans le temps, son estimation à grande échelle présente un grand défi, d’où le recours à la télédétection radar. Le capteur radar à synthèse d’ouverture (RSO) est couramment utilisé grâce à sa vaste couverture et sa résolution spatiale élevée. Contrairement aux sols nus et aux zones agricoles, le suivi de l’humidité du sol en zone forestière est très peu étudié à cause de la complexité des processus de diffusion dans ce type de milieu. En effet, la forte atténuation de la contribution du sol par la végétation et la forte contribution de volume issue de la végétation réduisent énormément la sensibilité du signal radar à l’humidité du sol. Des études portées sur des couverts forestiers ont montré que le signal radar en bande C provient principalement de la couche supérieure et sature vite avec la densité de la végétation. Cependant, très peu d’études ont exploré le potentiel des paramètres polarimétriques, dérivés d’un capteur polarimétrique comme RADARSAT-2, pour suivre l’humidité du sol sur les couverts forestiers. L’effet du couvert végétal est moins important avec la bande L en raison de son importante profondeur de pénétration qui permet de mieux informer sur l’humidité du sol. L’objectif principal de ce projet est de suivre l’humidité du sol à partir de données radar entièrement polarimétriques en bandes C et L sur des sites forestiers. Les données utilisées sont celles de la campagne terrain Soil Moisture Active Passive Validation EXperiment 2012 (SMAPVEX12) tenue du 6 juin au 17 juillet 2012 au Manitoba (Canada). Quatre sites forestiers de feuillus ont été échantillonnés. L’espèce majoritaire présente est le peuplier faux-tremble. Les données utilisées incluent des mesures de l’humidité du sol, de la rugosité de surface du sol, des caractéristiques des sites forestiers (arbres, sous-bois, litières…) et des données radar entièrement polarimétriques aéroportées et satellitaires acquises respectivement, en bande L (UAVSAR) à 30˚ et 40˚ et en bande C (RADARSAT-2) entre 20˚ et 30˚. Plusieurs paramètres polarimétriques ont été dérivés des données UAVSAR et RADARSAT-2 : les coefficients de corrélation (ρHHVV, φHHVV, etc); la hauteur du socle; l’entropie (H), l’anisotropie (A) et l’angle alpha extraits de la décomposition de Cloude-Pottier; les puissances de diffusion de surface (Ps), de double bond (Pd) extraites de la décomposition de Freeman-Durden, etc. Des relations entre les données radar (coefficients de rétrodiffusion multifréquences et multipolarisations (linéaires et circulaires) et les paramètres polarimétriques) et l’humidité du sol ont été développées et analysées. Les résultats ont montré que 1) En bande L, plusieurs paramètres optimaux permettent le suivi de l’humidité du sol en zone forestière avec un coefficient de corrélation significatif (p-value < 0,05): σ[indice supérieur 0] linéaire et σ[indice supérieur 0] circulaire (le coefficient de corrélation, r, varie entre 0,60 et 0,96), Ps (r entre 0,59 et 0,84), Pd (r entre 0,6 et 0,82), ρHHHV_30˚, ρVVHV_30˚, φHHHV_30˚ and φHHVV_30˚ (r entre 0,56 et 0,81) alors qu’en bande C, ils sont réduits à φHHHV, φVVHV et φHHVV (r est autour de 0,90). 2) En bande L, les paramètres polarimétriques n’ont pas montré de valeur ajoutée par rapport aux signaux conventionnels multipolarisés d’amplitude, pour le suivi de l’humidité du sol sur les sites forestiers. En revanche, en bande C, certains paramètres polarimétriques ont montré de meilleures relations significatives avec l’humidité du sol que les signaux conventionnels multipolarisés d’amplitude.Abstract : Over forest canopies, soil moisture monitoring allows to prevent many disasters such as paludification, fires and floods. As this parameter is very dynamic in space and time, its large-scale estimation is a great challenge, hence the use of radar remote sensing. Synthetic aperture radar (SAR) sensor is commonly used due to its wide spatial coverage and its high spatial resolution. Unlike bare soils and agricultural areas, only few investigations focused on the monitoring of soil moisture over forested areas due to the complexity of the scattering processes in this kind of medium. Indeed, the high attenuation of soil contribution by the vegetation and the high vegetation volume contribution significantly reduce the sensitivity of the radar signal to soil moisture. Studies conducted at C-band have shown that the radar signal mainly comes from the upper layer and it quickly saturates with the vegetation density. However, very few studies have explored the potential of polarimetric parameters derived from a fully polarimetric sensor such as RADARSAT-2, to monitor soil moisture over forest canopies. With its large penetration’s depth, vegetation cover effect is less important at L-band, allowing thus to better inform on soil moisture. The main objective of this project is to monitor soil moisture from fully polarime tric L and C bands radar data acquired over forested sites. The data used were collected during the field campaign of Soil Moisture Active Passive Validation EXperiment 2012 (SMAPVEX12) which took place from June 6 to July 17, 2012 in Manitoba (Canada). Four deciduous forested sites were sampled. The main species is the trembling aspen. The data used included measurements of soil moisture, soil surface roughness, characteristics of the forested sites (trees, undergrowth, litter, etc.) and fully polarimetric airborne and satellite radar data respectively acquired at L-band (UAVSAR) with 30 ̊ and at 40 ̊ incidence angles and at C-band (RADARSAT -2) between 20 ̊ and 30 ̊. Several polarimetric parameters were derived from UAVSAR and RADARSAT-2 data: the correlation c oefficients (ρHHVV, φHHVV, etc); the pedestal height; entropy (H), anisotropy (A) and alpha angle extracted from Cloude-Pottier decomposition; surface (Ps) and double bounce (Pd) scattering powers extracted from Freeman-Durden decomposition, etc. Relationships between radar backscattering data (multifrequency and multipolarisation (linear/circular) backscattering coefficients and polarimetric parameters) and soil moisture were developed and analyzed. The results showed that 1) at L-band, several optimal parameters allow soil moisture monitoring over forested sites with a significant correlation coefficient (p-value < 0.05): linear and circular σ[superscript 0] (the correlation coefficient, r, varies between 0.60 and 0.96), Ps (r varies between 0.59 and 0.84), Pd (r varies between 0.60 and 0.82), ρHHHV_30 ̊, ρVVHV_30 ̊, φHHHV_30 ̊ and φHHVV_30 ̊ (r varies between 0.56 and 0.81). However, at C-band, there are only few optimal parameters φHHHV, φVVHV and φHHVV (r is around 0.90) . 2) at L-band, polarimetric parameters did not show any added values for soil moisture monitoring over forested sites compared to multipolarised σ[superscript 0]. Nevertheless, at C-band some polarimetric parameters show better significant relationships with the soil moisture than the conventional multipolarised backscattering amplitudes

TerraSAR-X and Wetlands: A Review

Since its launch in 2007, TerraSAR-X observations have been widely used in a broad range of scientific applications. Particularly in wetland research, TerraSAR-X\u27s shortwave X-band synthetic aperture radar (SAR) possesses unique capabilities, such as high spatial and temporal resolution, for delineating and characterizing the inherent spatially and temporally complex and heterogeneous structure of wetland ecosystems and their dynamics. As transitional areas, wetlands comprise characteristics of both terrestrial and aquatic features, forming a large diversity of wetland types. This study reviews all published articles incorporating TerraSAR-X information into wetland research to provide a comprehensive study of how this sensor has been used with regard to polarization, and the function of the data, time-series analyses, or the assessment of specific wetland ecosystem types. What is evident throughout this literature review is the synergistic fusion of multi-frequency and multi-polarization SAR sensors, sometimes optical sensors, in almost all investigated studies to attain improved wetland classification results. Due to the short revisiting time of the TerraSAR-X sensor, it is possible to compute dense SAR time-series, allowing for a more precise observation of the seasonality in dynamic wetland areas as demonstrated in many of the reviewed studies