Monday, April 1, 2019
Microwave Remote Sensing in Forestry
Microwave Remote Sensing in  toneryBACKGROUNDMicrowave remote  catching at wavelengths ranging from 1 cm to 1 m has gained a lot of importance  all over the  historic decade for a wide range of scientific applications with the availability of  dynamic   radio detection and ranging imaging  dodgings. Its  electromotive force in spatial applications has been scientific eachy  naturalised in  conf employ sectors  ilk  timberlandry, agriculture, land  make use of and land  counterbalance, geology and hydrology. A variety of applications  pay been carried out world over  use  zap   selective  learning like  favouritism of crop  graphic symbols, crop condition monitoring,  blemish moisture retrieval, delineation of   timber openings,  appraisal of  timberland supra  kingdom biomass,  af quality  part forest  building and fire scar  presentping, geologic  map, monitoring wetlands and snow  hybridise, sea ice  ac friendshipment, coastal windfield  barroomment, wave  angle  stair, ship detect   ion, shoreline detection, substrate mapping, slick detection and general  plant life mapping (Kasischke et al., 1997).There is an emerging interest on microwave remote  catching, as microwave sensors  quarter  depict a surface with very  lovely resolution of a  hardly a(prenominal) meters to coarse resolution of a few kilometers. They provide imagery to a  tending(p) resolution in bloodsuckingly of altitude,  trammel only by the transmitter power available. Fundamental parameters like    polarization and look angle  bath be wide-ranging to optimize the system for a specific application. SAR imaging is independent of solar illumination as the system provides its own  origin of illumination. It can operate independently of  suffer conditions if  sufficiently long wavelengths are chosen. It ope judge in a band of electromagnetic spectrum  diverse from the bands  employ by visible and infrared (IR) imageries.Microwave applications in ForestryApplications of microwave remote sensing in f   orestry  curb also been  describe during the recent past. Recent reviews on the application of  radio detection and ranging in forestry  introduce that SAR systems  obligate a good   say-so in discriminating  heterogeneous types of (tropical) forest cover  victimisation multi-temporal and multi-frequency SAR  info (Vander Sanden, 1997 Varekamp, 2001 Quinones, 2002 Sgrenzaroli, 2004). These studies showed that the biomass dependence of radar  disperse varies as a function of radar wavelength, polarization and incidence angle.  in like mannerrecent studies  have got demonstrated that synthetic aperture radar (SAR) can be use to  see   high up- object standing biomass. To date, these studies have relied on extensive  filth-truth measurements to  realize relationships  amongst biomass and SAR  scatter (Steininger, 1996 Rignot et al., 1997).M all studies demonstrated the use of  celluloid Aperture  microwave radar (SAR) remote sensing to retrieve biophysical characteristics from forest t   argets (Richards, 1990). Although radar  scatter from forest is influenced by their  geomorphological properties (Imhoff, 1995), earlier studies derived useful relationships between  scattering coefficients and the  above-ground biomass (Baker et., 1994 Le Toan et al., 1992  dobsonfly et el., 1992 Imhoff 1995). These relationships may provide a  manner of monitoring forest ecosystems which  consort   much(prenominal) a vital role in  coulomb  memory board and NPP.Microwave remote sensing has the advantage of all weather capability coverage overcoming the persistent problem of  fog cover in  artificial satellite images like in  optic selective  info. Optical remote sensing is  creation  utilise very successfully in various applications  cerebrate to  creation re showtimes studies and monitoring of the environment. However, optical remote sensing is not suitable for all atmospheric conditions. It cannot penetrate through clouds and haze. In many  lands of the world, the frequent cloud    conditions often restrain the acquisition of high-quality remotely sensed  info by optical sensors. Thus, radar  info has become the only feasible  air of acquiring remotely sensed  information within a given time framework because the radar systems can collect Earth  sign  info irrespective of weather or light conditions. Due to this  erratic feature of radar   information compared with optical sensor data, the radar data have been used extensively in many fields, including forest-cover identification and mapping, discrimination of forest compartments and forest types,  devotion of forest stand parameters and monitoring of forests. In areas where  flora cover is dense, it visually covers the underlying formation and it is very  strong to detect structural limiting the use of optical sensors.  radio detection and ranging however, is  medium enough to topographic variation that it is able to discern the structural   visual aspect reflected in the tree top  cover, and therefore the s   tructure may be clearly defined on the radar imagery.Based on this background, the  flow thesis work has been carried out to  search the potential of microwave data in addressing core areas of tropical forestry viz.,  phytology  assortment, above ground biomass  assessment etc., and to provide the users/researchers a meaningful data base of SAR applications in tropical forestry, specifically over the India region.Research questionsWhich SAR wavelength/frequency band is appropriate for  botany classification in tropical forests?To what extent above ground biomass can be measured in tropical forests?Which frequency band and polarization are suitable for above ground biomass  appraisal?Is there any enhancement in vegetation classification with polarimetric / interferometric data than stand  unsocial amplitude data?Research hypothesisBased on the  preliminary studies and earlier mentioned research questions, we understand that the backscatter increases with the increase in above ground    biomass and depends on wavelength bands, polarizations used and on the  interpret area, topographic variations and species composition. So, the  limn study attempts to derive the application potential of airborne and space borne SAR data in the quantification of the forest resources in tropical regions like India, both as a complementary and supplementary role to optical datasets.  diametrical techniques   such as Regression  abstract, multi-sensor fusion,  caryopsis measures and interferometric coherence characterize  diametric biomass ranges of the  campaign  grades and classification of  study land cover classes. This study would facilitate  ground for future research in tropical regions to explore the potentials of SAR data in land cover classification and above ground biomass  appraisal  apply the polarimetric and interferometric techniques.OBJECTIVESBased on this background, the present study aims at the following objectives botany type classification using polarimetric and in   terferometric SAR data.Forest above-ground biomass  idea using multi-frequency SAR data and ground inventoried data.Vegetation classification is necessary to understand the diversity of species in a given area which gives above ground biomass with measured parameters. Hence, vegetation classification enhances the  adhesion of the above ground biomass.Forest biomass is a  chance on parameter in  disposition the carbon cycle and determining rates of carbon storage, both of which are  bad un originalties for forest ecosystems. Accurate  familiarity of biophysical parameters of the ecosystems is essential to develop an understanding of the ecosystem and their interactions, to provide input models of ecosystem and global processes, to  outpouring these models and to monitor changes in ecosystem dynamics and processes over time. Thus, it is a useful measure for assessing changes in forest structure, comparing structural and functional attri providedes of forest ecosystems  across a wide r   ange of environmental conditions.Knowing the spatial  scattering of forest biomass is important as the  bopledge of biomass is required for calculating the sources and sinks of carbon that result from converting a forest to cleared land and vice versa, to know the spatial  diffusion of biomass which enables measurement of change through time.Field  sampling is the most followed conventional method for vegetation type classification. The identification of  polar species in field yields good results in the  regard of the above ground biomass. It is very time consuming, expensive and very complicated.With the use of multiple sensors, varied data collection and interpretation techniques, remote sensing is a  versatile  to a faultl that can provide data about the surface of the  universe to suit any need (Reene et al, 2001). Remote sensing approach for vegetation classification is cost effective and also time effective. Though the identification of the tree species is possible only from    the aerial imagery, major forest types can be identified from the airborne and the spaceborne remote sensing data. Visual image interpretation provides a feasible means of vegetation classification in forests. The image characteristics of shape, size, pattern, shadow, tone and texture are used by interpreters in tree species identification. Phenological correlations are useful in tree species identification. Changes in the appearance of trees in different seasons of the year some times enable discrimination of species that are indistinguishable on single dates. The use of multi-temporal remote sensing data enables the mapping of the different forest types.SAR has shown its potential for classifying and monitoring geophysical parameters both locally and globally. Excellent works were carried out on the classification using several approaches such as polarimetric data decomposition ( lee side et al., 1998), knowledge based approaches considering the theoretical backscatter modeling an   d experimental observations ( Ramson and  temperateness , 1994)   scatter model-related inversion approaches ( Kurvonen et al., 1999), neural ne tworks and data fusion approaches ( Chen et al., 1996). Dong et al. (2001) have shown that the classification accuracy of 95% for the vegetation classes could be achieved through the  class and classification of the SAR data using Gaussian Markov Random Field  stick (GMRF). umpteen methods have been employed for classification of polarimetric SAR data, based on the  supreme likelihood (ML) (Lee et al. 1994), artificial neural network (NN) (Chen et al. 1996, Ito and Omatu, 1998), support vector machines (SVMs) (Fukuda et al. 2002),  woolly-headed method (Chen et al. 2003, Du and Lee 1996), or  opposite approaches (Kong et al. 1988, Lee and Hoppel 1992, van Zyl and Burnette 1992, Cloude and Pottier 1997, Lee et al. 1999, Alberqa 2004) Among these methods, the ML classifier (Lee et al. 1994) can be employed for obtaining accurate classificatio   n results, but it is based on the assumption of the complex Wishart distribution of the covariance matrix.Assessing the  check aboveground biomass of forests (biomass  meanness when expressed as dry weight per unit area at a particular time) is a useful way of quantifying the   entire of resource available for all traditional uses. It either gives the quantity of total biomass directly or the quantity by each component (e.g., leaves, branches, and bole) because their biomass tends to  substitute systematically with the total biomass. However, biomass of each component varies with total biomass by forest type, such as natural or planted forests and closed or open forests. For example, leaves contribute about 3-5% and merchantable bole is about 60% of the total aboveground biomass of closed forests.Many researchers have  true various methods based on field inventory and remote sensing approaches for the estimation of above ground biomass (Kira and Ogawa, 1971). Traditionally, field-me   asured approach is considered as the most accurate source for above-ground biomass estimation. It has been converted to  great deal, or biomass, using allometric equations that are based on standard field measurements (tree  line of longitude and diameter at  depreciator height).Different approaches, based on field measurement (Brown et al. 1989, Brown and Iverson 1992, Schroeder et al.. 1997, Houghton et al., 2001, Brown, 2002) remote sensing (Tiwari 1994, Roy and Ravan 1996, Tomppo et al., 2002, Foody et al., 2003, Santos et al., 2003, Zheng et al., 2004, Lu, 2005) and GIS (Brown and Gaston 1995) have been applied for AGB estimation. Traditional techniques based on field measurement are the most accurate ways for collecting biomass data. A sufficient number of field measurements is a prerequisite for developing AGB estimation models and for evaluating the AGB estimation results. However, these approaches are often time consuming, labour intensive, and difficult to implement, espec   ially in remote areas and are generally limited to 10-year intervals. Also, they cannot provide the spatial distribution of biomass in  coarse areas.For the above reasons, the perspectives of using remote sensing techniques to  bet forest biomass have gained interest. Remote sensing data available at different scales, from local to global, and from various sources, optical to microwave are expect to provide information that could be related indirectly, and in different manners, to biomass information. The  speculation that aboveground forest biomass might be determined from space is a promising alternative to ground-based methods (Hese et al., 2005).The advantages of remotely sensed data, such as in repetivity of data collection, synoptic view, digital format that allows fast processing of large quantities of data, and the high correlations between spectral bands and vegetation parameters, make it the primary source for large area AGB estimation, especially in areas of difficult acc   ess. Therefore, remote sensing-based AGB estimation has increasingly attracted scientific interest.In general, AGB can be estimated using remotely sensed data with different approaches, such as multiple  reverting analysis, K nearest-neighbour, and neural network (Roy and Ravan 1996, Nelson et al. 2000a, Steininger 2000, Foody et al. 2003, Zheng et al. 2004), and indirectly estimated from canopy parameters, such as crown diameter, which are first derived from remotely sensed data using multiple  backsliding analysis or different canopy  reflectivity models (Wu and Strahler 1994, Woodcock et al. 1997, Phua and Saito 2003, Popescu et al. 2003).Spectral signatures or vegetation indices are often used for AGB estimation in optical remote sensing. Many vegetation indices have been developed and applied to biophysical parameter studies (Anderson and Hanson 1992, Anderson et al. 1993, Eastwood et al. 1997, Lu et al. 2004, Mutanga and Skidmore 2004). Vegetation indices have been recommended    to remove discrepancy caused by canopy geometry, soil background, sun view angles, and atmospheric conditions when  measuring rod biophysical properties (Elvidge and Chen 1995, Blackburn and Steele 1999).Radar remote sensing has potential to provide information on above ground biomass. The information content of SAR data in terms of the retrieval of biomass parameters will be assessed based on an understanding of the underlying scattering mechanisms, which in turn are derived from observations and modeling results. For this purpose, an analysis of data acquired by multiple frequency, incidence and polarisation systems and by interferometric systems is carried out. It has been  be that the sensitivity to biomass parameters differ strongly at different frequencies, polarisations and incidence angles.In general, long wavelength SAR backscatter (P and L band) is more  splendid to forest biomass than shorter wavelength C-band backscatter and the relationships saturate at certain biomass    levels ( Imhoff 1995b). The strength of the relationships and the saturation levels are dependent on the type of forest being analysed (Ferrazoli et al. 1997). The saturation levels for the estimation of above ground biomass depend on the wavelengths (i.e. different bands, such as C, L, P), polarization (such as HV and VV), and the characteristics of vegetation stand structure and ground conditions. C-band can measure forestry biomass up to app. 50  oodles/ha, L-band can measure up to  deoxycytidine monophosphate tons/ha and P-band can measure up to 200 tons/ha (Floyd et al., 1998). The combination of multiple  convey and polarizations provides greater advantage for estimating total biomass (Harry Stern, 1998).RELEVANCE OF THE STUDYThe present study is the part of Radar  mental imagery satellite  Joint Experiment Programme (RISAT-JEP) for forestry applications undertaken by Forestry and Ecology  grade of National Remote Sensing Centre (NRSC), as a  navigate campaign with specific o   bjectives of above ground biomass estimation and vegetation type classification using airborne DLR (German Aerospace Center) carrying ESAR (Experimental  synthetical Aperture Radar) data for Rajpipla (Gujarat) study site and space borne ENVISAT (Environmental  broadcast) carrying Advanced Synthetic Aperture Radar (ASAR) data for three  study sites viz., Rajpipla (Gujarat), Dandeli (Karnataka) and Bilaspur (Chattisgarh), India.SCOPE OF THE STUDYThe specific objectives of the present study are above ground biomass estimation and vegetation type classification using airborne DLR (German Aerospace Center) carrying ESAR (Experimental Synthetic Aperture Radar) data for Rajpipla (Gujarat) study site and space borne ENVISAT (Environmental Satellite) carrying Advanced Synthetic Aperture Radar (ASAR) data ALOS (Advanced Land Observing Satellite) carrying Phased Array L-band Synthetic Aperture Radar (PALSAR) for three test sites viz., Rajpipla (Gujarat), Dandeli (Karnataka) and Bilaspur (Chatt   isgarh), India.Different techniques such as Regression analysis, multi-sensor fusion, texture measures and interferometric coherence were used to characterize different biomass ranges of the test sites and to classify the major land cover classes using spaceborne C-band ENVISAT-ASAR data and L-band ALOS- PALSAR data. Polarimetric signatures, polarimetric decompositions, multi-sensor fusion techniques etc. were used for the classification of different vegetation types in the Rajpipla study area using the airborne DLR-ESAR data.The study has its uniqueness and gains importance in the application potential of SAR interferometry over tropical regions like India, both in terms of an  alternate/substitute to optical data sets due to persisting cloud cover and to the lack of availability of any earlier scientific work over the study region. This study is useful for the applications of to be launched Radar Imaging Satellite (RISAT) in 2010.The study has amply demonstrated the application po   tential of airborne and space borne SAR data in the quantification of the forest resources in tropical regions like India, both as a complementary and supplementary role to optical datasets. The study would facilitate future research in tropical regions to explore the potentials of SAR data in land cover classification and above ground biomass estimation using the polarimetric and interferometric techniques.LITERATURE SURVEYDuring the last decade, many potential applications of SAR in different frequency bands have been studied for forestry applications using data acquired by both airborne and space-borne systems. Various techniques like Polarimetry, Interferometry and Polarimetric-Interferometry enhanced the use of SAR data in forestry applications. The backscatter from vegetation is used to infer information about amplitude data for forest cover mapping and estimation of above ground biomass in regenerate forests. Use of SAR polarimetric data  define vegetation classes within the    forest and also enhanced the capability in estimating the above ground biomass. The use of repeat pass interferometric data enables to  target the forest stand height and also used for the land cover classification. The emerging Pol-InSAR technique is used to derive the three dimensional forest structures.Forest cover maps were prepared for the circumboreal, temperate and tropical forests using SAR data. Forest was separated from non-forest regions using multi-temporal C-band ERS SAR data on the test sites of United Kingdom, Poland and Finland (Quegan et al., 2000). The study applied a threshold value to separate forest from other classes. Tropical rainforest of Borneo was mapped from SIR-B data of different incidence angles (Ford and Casey, 1988). Different vegetation covers along with wetlands and clear-cut areas were distinguished. Forest cover mapping was done with JERS-1 SAR data on the coastal regions of Gabon (Simard et al., 2000). The study used decision tree method utilizin   g both radar amplitude and texture information. Forest cover map was prepared for Southern Chittagong using JERS-1 SAR data (Rahman and Sumantyo, 2007) and the study separated forest,  adulterated forest, shrubs, coastal plantations, agriculture, shrimp-farms, urban and water.Although radar backscatter from forest is influenced by their structural properties (Imhoff, 1995a), many studies have demonstrated useful relationships between backscattering coefficients and the areal density of above-ground biomass within particular types of forest (Baker et., 1994 Le Toan et al., 1992 dobson et al., 1992 Imhof et al 1995b).Many airborne and spaceborne SAR systems have been used to carry out a large amount of experiments for investigating the forest ecosystems. The airborne systems, such as the NASA/JPL AIRSAR, DLR-ESAR, etc., operating(a) at P, L and C band, has been flown over many forest sites (Zebker et al., 1991 Le Toan et al, 1992 Beaudoin et al., 1994 Rignot et al. 1994 Skriver et al.   , 1994 Ranson et al., 1996). The experiments of the Canadian CV-580, as well as the European airborne system,  in the first place operating at C and X band also have been carried out in North America and Europe (Drieman et al., 1989 Hoekman, 1990). Spaceborne SAR is being used from regional to global monitoring in a periodic basis. The spaceborne systems, such as the Seasat SAR, SIR-B, SIR-C/X-SAR and ERS-1, ERS-2, ENVISAT-ASAR, RADARSAT etc., were used for investigations of boreal, temperature and sub-tropical forestry test sites (Ford et al., 1988 Dobson et al., 1992 Ranson et al., 1995 Stofan et al., 1995 Rignotet al., 1995). These experiments and studies have shown that radar is sensitive to forest structural parameters such as diameter at breast height (dbh) and tree mean height including above-ground biomass (Dobson et al., 1992 Pulliainen et al., 1994 Skriver et al., 1994 Ferrazzoli et al., 1995 Ranson et al., 1996).Earlier studies has shown the potential of radar data in est   imating AGB (Hussin et al. 1991, Ranson and Sun 1994, Dobson et al. 1995, Rignot et al. 1995, Saatchi and Moghaddam 1995, Foody et al. 1997, Harrell et al. 1997, Ranson et al. 1997, Luckman et al. 1997, 1998, Pairman et al. 1999, Imhoff et al. 2000, Kuplich et al. 2000, Castel et al. 2002, Sun et al. 2002, Santos et al. 2003, Treuhaft et al. 2004). Kasischke et al. (1997) reviewed radar data for  ecologic applications, including AGB estimation. Lucas et al. (2004) and Kasischke et al. (2004) reviewed SAR data for AGB estimation in tropical forests and temperate and boreal forests, respectively. Different wavelength radar data have their own characteristics in relating to forest stand parameters. Backscatter in P and L bands is highly  agree with major forest parameters, such as tree age, tree height, DBH,  base area, and AGB (Leckie 1998). In particular, SAR L-band data have proven to be valuable for AGB estimation (Sader 1987, Luckman et al. 1997, Kurvonen et al. 1999, Sun et al. 2   002). However, low or negligible correlations were  comprise between SAR C- forget me drug backscatter and AGB (Le Toan et al. 1992). Beaudoin et al. (1994) found that the HH return was related to both trunk and crown biomass, and the VV and HV returns were  colligate to crown biomass.Harrell et al. (1997) evaluated four techniques for AGB estimation in pine stands using SIR C- and L-Band multi-polarization radar data and found that the L-Band HH polarization data were the critical elements in AGB estimation. Kuplich et al. (2000) used L-band JERS-1/SAR data for AGB estimation of regenerating forests and  cerebrate that these data had the potential to estimate AGB for young, regenerating forests. Sun et al. (2002) found that multi-polarization L-Band SAR data were useful for AGB estimation of forest stands in mountainous areas. Castel et al. (2002) identified the significant relationships between the backscatter coefficient of JERS- 1/SAR data and the stand biomass of a pine plantat   ion. The study observed the  benefit in AGB estimation results for young stands, compared to estimation for old stands. Santos et al. (2002) used JERS-1 SAR data to analyse the relationships between backscatter signals and biomass of forest and savanna formations. This study concluded that forest structural-physiognomic characteristics and the radars volume scattering, double bounce scattering are two important factors affecting these relationships. The saturation levels of backscattering co-efficient with respect to AGB depend on the wavelengths (i.e. different Bands, such as C, L, P), polarization (such as HV and VV), and the characteristics of vegetation stand structure and ground conditions. Luckman et al. (1997) found that the longer-wavelength (L-Band) SAR image was more suitable to  detach different levels of forest biomass up to a certain threshold, indicating that it is suitable for estimating biomass of regenerating forests in tropical regions. Austin et al. (2003) indicat   ed that forest biomass estimation using radar data may be feasible when landscape characteristics are taken into account.The radar backscattering coefficient is correlated with forest biomass and stem volume (Le Toan et al. 1992, Israelsson et al. 1994, Kasischke et al. 1994, Dobson et al. 1995). The sensitivity of Synthetic Aperture Radar (SAR) data to forest stem volume increases significantly as the radar wavelength increases (Israelsson et al. 1997). The imaging process makes SAR suitable for mapping parameters related to forest biomass, like stem volume (Baker et al, 1999 Fransson et al, 1999 Hyyppa et al, 1997 Israelsson et al., 1997 Kurvonen et al, 1999 Pulliainen et al, 1996), total  suppuration stock (Balzter et al, 2000 Schmullius et al, 1997), LAI (Imhoff et al, 1997), or above ground net primary productiveness (Bergen et al, 1998).Le Toan et al., (1992) used multi-polarisation L- and P-band airborne radar data, and found that the dynamic range of the radar backscatter co   rresponded highly with forest growth stages and is maximum at P-band HV polarization. The analysis of P-band data indicated a good correlation between the radar backscatter long suit and the main forest parameters including trunk biomass, height, age, diameter at breast height (dbh), and basal area. Dobson et al., (1992) showed an increasing range of backscatter with changing biomass from C to P-band, as well as higher biomass levels at which backscatter relationships to biomass saturate. Hoekman, (1990) found poor relationships between X- and C-band backscatter and volume and other stand parameters.The spaceborne systems, such as the Seasat SAR, SIR-B, SIR-C/X-SAR and ERS-1, ERS-2, JERS, ENVISAT-ASAR and recently ALOS-PALSAR etc. were used for investigations of boreal, temperature and sub-tropical forestry test sites (Ford et al., 1988 Dobson et al., 1992 Ranson et al., 1995 Stofan et al., 1995 Rignot et al., 1995). These experiments and studies have shown that radar is sensitive t   o forest structural parameters including above-ground biomass (Dobson et al., 1992 Pulliainen et al., 1994 Skriver et al., 1994 Ferrazzoli et al., 1995 Ranson et al., 1996).Kasischke et al., (1997) reviewed radar data for ecological applications, including AGB estimation. It is being reported in literature that the radar backscatter in the P and L bands is highly correlated with major forest parameters, such as tree age, tree height, DBH, basal area, and AGB. In particular, SAR L-Band data have proven to be valuable for AGB estimation (Sader, 1987 Luckman et al., 1997 Kurvonen et al., 1999 Sun et al., 2002). Kuplich et al., (2000) used JERS-SAR data for AGB estimation of regenerating forests and concluded that these data had the potential to estimate AGB for young, regenerating forests. Luckman et al., (1997) found that the longer-wavelength (L-Band) SAR image was more suitable to discriminate different levels L-Band backscatter shows no sensitivity to increased biomass density afte   r a certain threshold, such as 100 tons ha-1, indicating that it is suitable for estimating biomass of regenerating forests in tropical regions.The radar backscattering coefficient is correlated with forest biomass and stem volume (Le Toan et al. 1992 Israelsson et al., 1994 Kasischke et al., 1994, Dobson et al., 1995). The sensitivity of Synthetic Aperture Radar (SAR) data to forest stem volume increases significantly as the radar wavelength increases (Israelsson et al., 1997). The imaging process makes SAR suitable for mapping parameters related to forest biomass, like stem volume (Baker et al., 1999 Israelsson et al., 1997 Pulliainen et al., 1996), total growing stock (Balzter et al., 2000 Schmullius et al., 1997), LAI (Imhoff et al., 1997), or above ground net primary productivity (Bergen et al., 1998).The dependency of backscatter on above ground biomass was observed and related to the penetration of the radiation into the canopy and interaction with the trunk, where most of th   e volume, therefore, biomass of the vegetation is  pure (Sader 1987, Le Toan et al. 1992, Dobson et al. 1992). HV polarization in longer wavelengths (L or P band) is the most sensitive to above ground biomass (Sader 1987, Le Toan et al. 1992, Ranson et al. 1997a) because it originates mainly from canopy volume scattering (Wang et al. 1995), trunk scattering (Le Toan et al. 1992) and is less affected by the ground surface (Ranson and Sun 1994).As forest backscatter in different wavelengths and polarizations originate from separate layers of a canopy, the use of multiple channels or multi-step approaches (e.g., Dobson et al. 1995) could be used to estimate total above-ground biomass (Kasischke et al. 1997). Sun and Ranson (1994) estimated biomass in  mingled conifer temperate forest upto 250 Mg/ha.Band ratios (HH/HV and VV/VH) were also used for the above ground biomass estimation. However, Dobson et al. (1995) considered these band ratios too simplistic (as the corresponding backscat   ter will be much higher for the few tall trees than for the many short ones), although effective in estimating biomass at higher ranges. In spite of this, a combination of bands and polarizations in a multi-step approach made possible the mapping of biomass in a mixed temperate forest upto 250 Mg/ha (Dobson et al. 1995). Establishing a strong  come to between backscatter and forest variables is an important part of the successful estimation of forest biomass from backscatter. Models are often used to explain the relationship between forest variables, scattering mechanisms and SAR configuration parameters (Richards 1990, Kasischke and Christensen 1990). Another approach is the use of statistical analysis, where forest variables are related to SAR backscatter by regression models (Sader 1987, Le Toan et al. 1992, Rauste et al. 1994). The combination of the two approaches, in most cases to assess the results of the predicted biomass or backscatter via regression (Ranson and Sun 1994, F   errazzoli et al. 1997, Franson and Israelson 1999). Statistical procedures such as stepwise regression analysis were also used to determine the best set of bands and polarizations to discriminate biomass levels (Ranson et al. 1997a).The three-band (C, L, and P) polarimetric AIRSAR sensor has been used in many forest biomass studies (e.g., Green, 1998 Kasischke et al., 1991, 1995 Moghaddam et al., 1994 Ranson  Sun, 1997). The strongest correlation between SAR backscatter and forest biomass has been reported in P-band and the weakest in C-band (e.g., Beaudoin et al., 1992 Dobson et al., 1992 Israelsson et al., 1992 Rauste et al., 1992  
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