Sentinel-1 derived Coherence Time-series for Crop Monitoring in Indian Agriculture Region

2021 ◽  
pp. 1-17
Author(s):  
Ankur Pandit ◽  
Suryakant Sawant ◽  
Jayantrao Mohite ◽  
Srinivasu Pappula
2018 ◽  
Vol 10 (8) ◽  
pp. 1272 ◽  
Author(s):  
Stephanie Olen ◽  
Bodo Bookhagen

The emergence of the Sentinel-1A and 1B satellites now offers freely available and widely accessible Synthetic Aperture Radar (SAR) data. Near-global coverage and rapid repeat time (6–12 days) gives Sentinel-1 data the potential to be widely used for monitoring the Earth’s surface. Subtle land-cover and land surface changes can affect the phase and amplitude of the C-band SAR signal, and thus the coherence between two images collected before and after such changes. Analysis of SAR coherence therefore serves as a rapidly deployable and powerful tool to track both seasonal changes and rapid surface disturbances following natural disasters. An advantage of using Sentinel-1 C-band radar data is the ability to easily construct time series of coherence for a region of interest at low cost. In this paper, we propose a new method for Potentially Affected Area (PAA) detection following a natural hazard event. Based on the coherence time series, the proposed method (1) determines the natural variability of coherence within each pixel in the region of interest, accounting for factors such as seasonality and the inherent noise of variable surfaces; and (2) compares pixel-by-pixel syn-event coherence to temporal coherence distributions to determine where statistically significant coherence loss has occurred. The user can determine to what degree the syn-event coherence value (e.g., 1st, 5th percentile of pre-event distribution) constitutes a PAA, and integrate pertinent regional data, such as population density, to rank and prioritise PAAs. We apply the method to two case studies, Sarpol-e, Iran following the 2017 Iran-Iraq earthquake, and a landslide-prone region of NW Argentina, to demonstrate how rapid identification and interpretation of potentially affected areas can be performed shortly following a natural hazard event.


Author(s):  
Felix Rembold ◽  
Michele Meroni ◽  
Ferdinando Urbano ◽  
Antoine Royer ◽  
Clement Atzberger ◽  
...  

2016 ◽  
Vol 8 (11) ◽  
pp. 903 ◽  
Author(s):  
Sofia Antonova ◽  
Claude Duguay ◽  
Andreas Kääb ◽  
Birgit Heim ◽  
Moritz Langer ◽  
...  

2021 ◽  
Author(s):  
Santiago Belda ◽  
Matías Salinero ◽  
Eatidal Amin ◽  
Luca Pipia ◽  
Pablo Morcillo-Pallarés ◽  
...  

<p>In general, modeling phenological evolution represents a challenging task mainly because of time series gaps and noisy data, coming from different viewing and illumination geometries, cloud cover, seasonal snow and the interval needed to revisit and acquire data for the exact same location. For that reason, the use of reliable gap-filling fitting functions and smoothing filters is frequently required for retrievals at the highest feasible accuracy. Of specific interest to filling gaps in time series is the emergence of machine learning regression algorithms (MLRAs) which can serve as fitting functions. Among the multiple MLRA approaches currently available, the kernel-based methods developed in a Bayesian framework deserve special attention because of both being adaptive and providing associated uncertainty estimates, such as Gaussian Process Regression (GPR).</p><p>Recent studies demonstrated the effectiveness of GPR for gap-filling of biophysical parameter time series because the hyperparameters can be optimally set for each time series (one for each pixel in the area) with a single optimization procedure. The entire procedure of learning a GPR model only relies on appropriate selection of the type of kernel and the hyperparameters involved in the estimation of input data covariance. Despite its clear strategic advantage, the most important shortcomings of this technique are the (1) high computational cost and (2) memory requirements of their training, which grows cubically and quadratically with the number of model’s samples, respectively. This can become problematic in view of processing a large amount of data, such as in Sentinel-2 (S2) time series tiles. Hence, optimization strategies need to be developed on how to speed up the GPR processing while maintaining the superior performance in terms of accuracy.</p><p>To mitigate its computational burden and to address such shortcoming and repetitive procedure, we evaluated whether the GPR hyperparameters can be preoptimized over a reduced set of representative pixels and kept fixed over a more extended crop area. We used S2 LAI time series over an agricultural region in Castile and Leon (North-West Spain) and testing different functions for Covariance estimation such as exponential Kernel, Squared exponential kernel and matern kernel with parameter 3/2 or 5/2. The performance of image reconstructions was compared against the standard per-pixel GPR time series training process. Results showed that accuracies were on the same order (12% RMSE degradation) whereas processing time accelerated up to 90 times. Crop phenology indicators were also calculated and compared, revealing similar temporal patterns with differences in start and end of growing season of no more than five days. To the benefit of crop monitoring applications, all the gap-filling and phenology indicators retrieval techniques have been implemented into the <strong>freely downloadable GUI toolbox DATimeS</strong> (Decomposition and Analysis of Time Series Software - https://artmotoolbox.com/).</p>


Author(s):  
Priscilla Gail Minotti ◽  
Mariela Rajngewerc ◽  
Vanesa Alí Santoro ◽  
Rafael Grimson

2013 ◽  
Vol 6 (1) ◽  
pp. 135-156 ◽  
Author(s):  
Nguyen-Thanh Son ◽  
Chi-Farn Chen ◽  
Cheng-Ru Chen ◽  
Huynh-Ngoc Duc ◽  
Ly-Yu Chang

2013 ◽  
Vol 1 (1) ◽  
pp. 37 ◽  
Author(s):  
Kaushalya Ramachandran ◽  
Bandi Venkateshwarlu ◽  
C.A. Ramarao ◽  
V.U.M. Rao ◽  
B.M.K. Raju ◽  
...  

2020 ◽  
Author(s):  
Stephanie Olen ◽  
Bodo Bookhagen

<p>Mountain landscapes are shaped by hillslope and fluvial processes that remove and transport material and sediment. Developing proxies to map these processes through space and time is a key element in better understanding their distribution and drivers. Remotely sensed and satellite observations of Earth’s surface are greatly expanding the reach of geomorphologists and presenting a myriad of new opportunities to explore and quantify Earth surface processes. Synthetic aperture radar (SAR), in particular, promises to be a powerful tool for mapping and quantifying geomorphic processes. Here, we exploit a time series of coherence estimates between SAR images from the Copernicus Sentinel-1 mission. Coherence is the spatial correlation between two SAR images and is sensitive to changes in both the phase (elevation) and amplitude (surface backscatter) of the received radar signal. Geomorphic processes such as landsliding, hillslope slump, cobble movement, or alluvial sediment transport can result in loss of SAR coherence. In regions without significant vegetation or anthropomorphic input, we therefore propose that coherence loss is a proxy for surface sediment movement and geomorphic activity. We constructed time series of Sentinel-1 coherence images spanning three to five years for arid and semi-arid regions of the Argentinian Central Andes and the north-western Himalaya. Both regions are characterized by active tectonics and seasonal climatic gradients. The relatively short revisit time of the Sentinel-1 satellites (~2-4 weeks in our regions of interest) mean that we can not only map geomorphic activity averaged over multiple years, but observe intra-annual and seasonal differences throughout a given year. We are also able to compare interannual geomorphic responses during years with, e.g.,  relatively strong or weak monsoon seasons.</p><p> </p><p>We couple our Sentinel-1 coherence time series with a compilation of published 10-Berrylium terrestrial cosmogenic nuclide basin-wide denudation rates from the Open Cosmogenic isoTOPe and lUmineScence (OCTOPUS) database. For basins with cosmogenic data, we derive temporal and spatial statistics of our coherence time series. Across regional gradients, the range of coherence within basins positively correlates to millennial denudation rates and to topographic metrics used to indicate long-term uplift (e.g., channel steepness). Outlying basins include those in which erosion is driven by large, deep-seeded landslides that occur over repeat times longer than our multi-year observation period. Our study suggests that a dense time series of interferometric coherence can be used as a proxy for surface sediment movement and landscape stability in vegetation-free settings at event to decadal timescales.</p>


Sign in / Sign up

Export Citation Format

Share Document