Source: Applied GeoSolutions, LLC submitted to NRP
OPERATIONAL SAR FOREST STRUCTURE AND DISTURBANCE METRICS
Sponsoring Institution
National Institute of Food and Agriculture
Project Status
COMPLETE
Funding Source
Reporting Frequency
Annual
Accession No.
1002737
Grant No.
2014-33610-21910
Cumulative Award Amt.
$99,785.00
Proposal No.
2014-00038
Multistate No.
(N/A)
Project Start Date
Jun 1, 2014
Project End Date
Jan 31, 2016
Grant Year
2014
Program Code
[8.1]- Forests & Related Resources
Recipient Organization
Applied GeoSolutions, LLC
87 Packers Falls Road
Durham,NH 03824
Performing Department
(N/A)
Non Technical Summary
The goal of the SBIR is to "Operationalize multiscale Synthetic Aperture Radar (SAR) forest structure and disturbance metrics". The objectives are to develop 1.) operational forest structure and disturbance metrics derived from Synthetic Aperture Radar and 2.) mapping information services for rapid forest disturbance assessment. A set of practical questions to be answered at three demonstration case study sites will evaluate the technical, scientific, and commercial feasibility. A direct outcome is the creation of rapid, automated forest structure metrics, disturbance assessment, and decision support tools to improve our understanding of forest health and sustainability; quantify the impacts of disturbance; and help characterize the impacts of climate change and invasive species on forest resources. This SBIR also addresses a NIFA Societal Challenge Area, "Climate Change", by developing standardized assessment metrics that will contribute to carbon science and reducing greenhouse gas emissions through programs such as Forest Inventory and Analysis (FIA) National Program and international programs such as Reducing Emissions from Deforestation and Degradation (REDD).
Animal Health Component
70%
Research Effort Categories
Basic
10%
Applied
70%
Developmental
20%
Classification

Knowledge Area (KA)Subject of Investigation (SOI)Field of Science (FOS)Percent
12372102060100%
Goals / Objectives
GoalOperationalize multiscale Synthetic Aperture Radar (SAR) forest structure and disturbance metricsTechnical Objectives Compile existing field data and gap fill with new field data campaign with strategic end usersOperationalize Interferometric Synthetic Aperture Radar (InSAR) forest stand height (FSH)Operationalize Polarimetric (PLR) L-band data for systematic metricsImplement and assess Radar Forest Degradation IndexAssess products across demonstration sites and work with USFS end usersCarry out total market opportunity assessment (TMOA) and conduct focus group
Project Methods
Advancing SARsatellite remote sensing technologies have an opportunity to become more commonplace and address innovation gaps if we can overcome barriers such as complex formats, access, intensive preprocessing requirements, and the lack of systematic products.In this Phase I SBIR we will evaluate the technical, scientific, and commercial feasibility of operationalizing strategic SAR products three demonstration case study applications in the northeast USA. We will work closely with USDA USFS and strategic end users. We will apply innovative approaches using the most cutting-edge SAR science while examining technology limitations, spatial and temporal resolution barriers, and cost efficiency for applications. We intend to operationalize SAR derived metrics of above ground live biomass, forest stand height, canopy cover, and degradation using L-band SAR measurements from the Japanese Aerospace Exploration Agency's (JAXA) Advanced Land Observation Satellite-1 (ALOS-1) and Advanced Land Observation Satellite-2 (ALOS-2) satellite platforms. In the coming years, NASA along with ESA plan to launch their own L-band satellites (e.g., DESDynI-R), which will further increase the availability of L-band remote sensing measurements and our applications. Synthetic Aperture Radar are active sensors that measure echo through clouds with sensitivity to vegetation structure, geometry, and moisture content (dielectric properties). Wavelength frequency, polarization, and viewing geometry are key factors determining choice of SAR data for a given application. In short, longer wavelengths (smaller frequency) have greater ability to 'penetrate' a given target (fig 2; Saatchi 2013, slide from pers com). SAR signal can transmit horizontal (H) or vertical (V) field vectors, and receive either horizontal (H) or vertical (V) return signals, or both. The incidence angle (θ) can be defined as the angle formed by the radar beam and a line perpendicular to the surface, or essentially determine the viewing geometry. By modeling the given responses of a target with known imaging parameters a detailed description of scattering can be generated (fig 3). At L-band (1.25 GHz; 23cm wavelength), radar waves penetrate into the forest canopy through gaps and areas with relatively low density of scatterers (sparse medium effect) and scatter back from various components of the forest such as the crown (leaves and branches) and stems (Saatchi and McDonald 1997). The co- and cross-polarized radar measurements contain different information about the orientation and structure of forest canopy and tree stems within the resolution cell of radar images (Ulaby and Elachi 1990). Thus, SAR has particular advantages over traditional optical satellite imaging at the same time creates barriers to use due to relatively more complexities and requirements for data handling.There is tremendous opportunity to take advantage of these SAR archives and new SAR imagery. SAR observations have been used in many forestry disturbance in research applications and academic institutions. The most common applications identify relationships between SAR backscatter and the vegetation structural attributes in one of two ways, via empirical models or mechanistic models. For example, Saatchi et al. (2007) used an empirical approach to map biomass and fuel loads in Yellowstone using L- and C- band radar. Mitchard et al (2009) used co-polarized L-band data to map above ground biomass across several sites of woody vegetation up to 150 Mg ha-1 before relationships became noisy from saturation. At high biomass L-band can become saturated (Saatchi et al 2011); Zheng et al (2008) showed that the average biomass in the northeast around 120 Mg-ha. As part of our feasibility we will assess potential limits to mapping AGB in the northeast with L-band from ALOS-1 and ALOS-2. Hame et al (2013) found L-band effective in mapping AGB in Laos with dense tropical forest, but noted many of those sites had undergone degradation. To estimate foliar biomass in conifer forests, Moghaddam et al. (2002) found that L-band data from AIRSAR in combination with C-band data and multispectral Landsat data improved results over any of the three sensors alone. Wolter and Townsend (2011) generated a suite of metrics from SAR and optical data and applied partial least squares regression to map forest species and abundance in Minnesota. Recently, Antropov et al (2013) developed a semi-empirical approach based on dual pol L-band to estimate stand-level stem volume for boreal sites in Finland.Other efforts (e.g. Treuhaft and Siqueira 2000, Papathanassiou and Cloude 2001) have used the full interferometric signature for estimating vegetation height. One advantage of these techniques, and others like it, is that they do not require an external measure of the bare ground topography. The magnitude, also known as the coherence, is related to the volume scattering within a resolution element and therefore can be used for determining height using simple volume-scattering models (Treuhaft and Siqueira 2004), or models that take in to account the motion of the scatterers between observing passes of the interferometric instrument (Lavalle et al. 2012).We designed three strategic demonstration case studies that represent varying "gradients of disturbance" at different intensity and scales: Tornado event (July 2008) in central New Hampshire: Severe damage can be caused by extreme weather with disturbance ranging from the leveling forest blocks to downed debris. Mid-elevational (500-1500') areas of central New Hampshire fall largely in the transition zone between the northern hardwoods-spruce and hardwood-pine-hemlock forests. Typical northern hardwoods-spruce forest species include sugar maple (Acer saccharum), yellow birch (Betula alleghaniensis), American beech (Fagus grandifolia), and red spruce (Picea rubens). Typical hardwood-pine-hemlock forest species include red maple (Acer rubrum), red oak (Quercus rubra), hemlock (Tsuga Canadensis), and white pine (Pinus strobus). Forests are generally mixed-species, disturbance prone, and fragmented and have a diverse anthropogenic history.Asian Longhorn Beetle Insect infestation (2008-present): Like Emerald Ash Border or Oak Roller, Asian Longhorn Beetle are invading forests in the northeast and act as defoliators. We will work with end users in the Boylston-Worcester area and Harvard Forest of central Massachusetts to assess disturbed sites. This region is largely comprised of the transitional hardwood-pine-hemlock forests the central New England. The forest is a mix of species associated with more southern forests such as black oak (Quercus velutina), white oak (Quercus alba), and hickory (Carya spp.), northeastern species such as northern red oak (Quercus rubra), sugar maple (Acer saccharum), white pine (Pinus strobus), and hemlock (Tsuga Canadensis). Forest stands have a strong human influence from agricultural clearing and are generally mid-successional.Penobscot Experimental Forest, Maine (2007-present): A variety of harvest (i.e., thinning) managements with plot level data collection exists and we will evaluate our metrics for monitoring varying management practices. The Penobscot Experimental Forest falls in the transition zone between the eastern broadleaf and Acadian forests. Stands at the Forest are a mix of temperate hard and softwoods such as red maple (Acer rubrum), white pine (Pinus strobus), and eastern hemlock (Tsuga Canadensis), colder climate species associated with the boreal region such as red spruce (Picea rubens), balsam fir (Abies balsamea), and aspen (Populus spp.), as well as transition species such as birch (Betula spp.) and northern white cedar (Thuja occidentalis). Forests are structurally diverse and trend toward late-successional stages.

Progress 06/01/14 to 01/31/16

Outputs
Target Audience:Advancing satellite remote sensing technologies such as Synthetic Aperture Radar (SAR) have been shown in many research applications to be capable of addressing information gaps unable to be filled by the use of optical sensors, such as the well-known Landsat constellation. SAR sensors are capable of penetrating canopies, observing in all weather conditions, and have sensitivity to key forest biophysical parameters. The sensitivity of SAR to structural information (biomass, density, vertical layering, spacing) makes SAR advantageous, especially when cloud cover is problematic. Many non-experts are becoming aware of Landsat-based forest monitoring products since the transition to open archives and the launch of tools like Google Earth Engine. For example, Matt Hanson's forest maps and platforms such as Global Forest Watch are changing the way decisions get made. With the release of PALSAR-1 L-band data and open policy of Sentinel-1 C-band data, now collecting operationally and free, the opportunity to develop operational SAR forest monitoring is enormous, however challenges remain. The wide adaptation of SAR data and accompanying techniques for disturbance mapping has not occurred primarily due to: complexity of data formats and challenges of data handling lack of operational algorithms for generating forest attribute metrics lack of high resolution Digital Elevation Models (DEM) required for processing cost, lack of coverage, and baseline observations scenarios not wall-to-wall collection challenges of data fusion and multitemporal analyses In a way these technical barriers have created an innovation gap and opportunity. Keep in mind that Landsat, which tends to be more intuitive since it covers the visible portion of the spectrum, has been around for nearly 50 years. While SAR technology has a long history its use has remained elusive. However, many of the early barriers to SAR development are falling. Today, DEMs are readily available anywhere and constantly improving. Space agencies are shifting toward open data policies and distribute free L- and C- band satellite data. Observation strategies are now wall-to-wall with improving resolutions and have thus created "BigData" opportunities. Advancing computational techniques and cloud computing are increasing access and transferring information to the masses. Many "research studies" have executed projects using SAR and space agencies are now beginning to democratize science. The next step is to advance the tools and science for operational algorithms to generate forest characteristic products and mapping services by taking advantage of new SAR missions. This will greatly enhance forest monitoring and improve decision making. Over the next decade a suite of even more SAR sensors (e.g., NISAR, BIOMASS) with more operational power are planned for launch. This SBIR Phase II addresses this exact opportunity and will provide the foundation for success. United States Department of Agriculture (USDA) United States Forest Service (USFS)- Forest lands comprise 304million hectares of the total land area in the US with 44% controlled by Federal, State, and local governments. Characterizing forest structure, quantifying forest disturbance, and monitoring forest utilization on these lands is a primary and continuous need by multiple end user communities, including the USDA USFS (see letters). Both natural and anthropogenic stressors are influencing forest disturbance processes and patterns. Climate change, extreme weather, renewable energy demands, timber, land conversion, and invasive species are several key actors influencing forest function and services. These can range in frequency, intensity, and magnitude. Timely and accurate assessment of disturbance events and condition are critical to respond effectively and appropriately at local, regional, and national scales. In addition, assessing the severity and understanding the scales of disturbance are critical for broad-scale management, policy, and economic decision-making. While optical-based mapping techniques have made significant contributions toward assessment, they are limited by cloud coverage and only provided limited information on stand structure. The wide adaptation of operational SAR derived metrics into USFS programs and disturbance protocol has remained elusive due to the technical barriers. In this SBIR we intend to bridge this gap and provide enhanced products and services (metrics, maps, techniques, and expertise) that are easy to apply and integrate into decision support tools. Monitoring, Reporting, and Verification (MRV) community- The rapid growth of carbon science and characterization of ecosystem services has created a huge market for tools, products, and services. International monitoring frameworks, such as Reducing Emissions from Deforestation and Degradation (REDD), have created the need for robust Monitoring, Reporting, and Verification (MRV) platforms that can serve programs and initiatives aimed at carbon cycle science, conservation, and conventions. Maps of deforestation and degradation at multiple scales have taken on increased importance with the recognition of the value of forests and the rates of forest loss. International programs, like REDD, are being constructed to help preserve the world's forests, improve livelihoods, and promote sustainable practices. Under REDD, emissions and removals of carbon due to changes in forests are estimated from two components: activity data (e.g. deforestation, degradation) and forest carbon stock data (e.g. carbon in biomass, soil c). As systems are built in which some people pay others to slow the rate of carbon emissions from forest loss, the need for accurate, spatially explicit, and timely information on forests and forest change becomes critical. Satellite observations have been used to map forests since the 1970s. While optical reflectance data are the most abundant and common type of observations available, radar and Lidar data can be used to effectively map forest characteristics and changes. Optical reflectance observations passively measure the sun's radiation off of the land surface. Trees, forested areas, and changes in these areas are identified based on the amount and change in reflectance. SAR and Lidar are active systems that send out energy to the Earth's surface and measure the subsequent energy return. These active systems often provide more information regarding forest structure and, therefore, are useful for biomass and carbon content. Additionally, SAR systems are much less sensitive to cloud and haze cover than are optical systems, making them useful for forest monitoring in cloudy areas. However, many MRV/REDD platforms do not have the capacity to integrate SAR forest metrics. In this SBIR, we have strategically aligned the goals to serve this community (see letters). Our small business (AGS) has several high profile example MRV or "Decision Support Tools" (DST) currently operating that blend satellite maps, geospatial information, graphing and tabular data, mobile Apps, and end user options within web-GIS. Changes/Problems: Nothing Reported What opportunities for training and professional development has the project provided?Training and workshops to partners and end users. How have the results been disseminated to communities of interest?Yes What do you plan to do during the next reporting period to accomplish the goals? Nothing Reported

Impacts
What was accomplished under these goals? We determined RFDI was not optimal for our "low impact" case study disturbance (minor infestation) in the northeast. However, we note the Asian Longhorn Beetle "field data" from partners was not ideal given the lack of positional accuracy and quantitative metrics. Therefore, we also tried backscatter thresholding and examining multitemporal changes in sigma nought while comparing to optical indices such as Landsat NDVI. During Phase II we will co-collect this data with partners. We note that scale is a key element throughout this work and therefore emphasize the need to consider multiscale SAR data linked to the scale (or minimum mapping unit) of the field data AND issue to truly understand the strengths and limitations of detecting varying disturbance levels in an automated approach. The Phase II plan will address these scales directly with quantifiable metrics and field data. We also will support USFS programs with these metrics during the Phase II. We know we can automate RFDI for "high impact" case studies and scaling is not an issue (ie, CONUS product feasible) and we will continue to work with ForWarn. During Phase I we also tested JAXA's "Forest Non-Forest" (FNF) Mosaics generated from a decision tree approach. We created before and after products for disturbances. The FNF maps did poorly in mapping the disturbance demonstration case studies. A conclusion during Phase I was that FNF maps need to be locally tuned using sigma nought values as the "global" calibration was not sensitive to changes that were on the order of ~4db resulting from the tornado disturbance. RFDI was not useful for predicting AGB, or CCC in our case studies. During Phase II we will focus on locally tuned indices, multitemporal change vectors analyses, and add Sentinel-1 C-band data in addition to PALSAR-2 for a more thorough and robust toolset. Summarizing a case study, during Phase I, we evaluated empirical and semi-analytical models to generate SAR derived metrics of AGB, CCC, basal area, and disturbance. To evaluate performance we used a suite of statistics (R2, RMSE, Q-Q plots, residuals, Cook's distance, AIC, etc...) and expert judgement while considering cost and approach. For CCC and AGB we relied on semi-empirical regression using our compiled field sites across the region. We considered the explanatory power of the polarizations, ease of model execution, and benefits of more straightforward models vs models with higher accuracy but more complexity to pick an optimal approach for mapping attributes at the demonstration sites. Using the multicriteria approach the optimal models underwent n-folds cross validation to provide out of sample evaluation statistics (i.e., goodness of fit, RMSE) for predictions. During Phase I we achieved target accuracy goals for our AGB, basal area, and CCC metrics with R2 or 0.74, 0.79, and 0.75, respectively. Below we highlight AGB and CCC scatterplots of the cross validation (fig 6) where we mapped at 12.5m spatial resolution. We then extrapolated the models to the demonstration sites and region to help with assessment. During Phase I we also tested processing / modeling approaches including Water-Cloud and Random Volume over Ground. During Phase II we will enhance the number of field sites and integrate FIA data to expand regions with tuned estimates. Further, with this increase inn we can scale using more robust modeling approaches (i.e., physical retrieval models) as we generalize and integrate Sentinel-1 and Landsat 8 fusion. During Phase I our assessment concluded that in Carroll County more than 2500 hectares had modest (>50%) canopy damage and 1410 hectares had severe damage with a mean AGB loss of ~114 Mg / hectares in that severe damaged path. Total AGB loss in Carroll County was approximately 298,250Mg from the tornado (fig 7). From a cost perspective this would be a fraction of airborne Lidar (0.01 / hectare) considering the scalability. Phase 1 InSAR Forest Stand Height (FSH) During Phase I we tested repeat-pass InSAR techniques to map FSH at sites in the WMNH, NH sea coast, and across the entire northeast. Repeat-pass InSAR correlation measurements, assuming that the ground scattering effects can be ignored for cross-polarized SAR returns and also the interferometric vertical wavenumber, , is small (e.g., <0.05 rad/m), is the temporal change effects that dominate the repeat-pass InSAR correlation. The temporal change effects here refer to both the moisture change and random motion of the tree components during the repeat period of the satellite. As long as vegetation height dependence of the random motion effect, it is possible to utilize this dependence to invert forest height. In particular, the cross polarized repeat-pass InSAR correlation magnitude, , is connected to the physical forest height, , by the following relationship; where (from 0 to 1; unitless) is the model parameter accounting for moisture change and (>0; in the unit of meters) relates to random motion. We scaled up a forest stand height map (left) using repeat-pass InSAR using WMNF lidar. The WMNF scatterplot highlights InSAR inverted FSH and GRANIT Lidar-derived canopy height at 200m x 200m scale. We used more than 200 PALSAR-1 pairs to refine down to the optimal 36 InSAR scenes identified by coherence values for generating the map. We did notice weather driven moisture issues that we plan to address in Phase II. Python code was built to automate this process which is theoretically scalable to any sized region, such as CONUS. Stand scale or ~5 hectare minimum mapping unit is more appropriate than pixel level in this case.

Publications