EEEP 2017
DOI: 10.32006/eeep.2017.2.1319
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Monitoring of Short-Lived Snow Coverage by Radar and Optical Data From Sentinel-1 and Sentinel-2 Satellites

Abstract: Snow cover monitoring shows the great importance of this rainfall, the time-lines of the data from this event, and the spatial range and area of the observed object. The main aim of the presented research is to trace the use of different satellite data and approaches to track the dynamics of the development of the short-lived snow coverage. The subject of the study is short-lived snow coverage and its dynamics for 12 and 13 March 13, 2017 for Sofia city area, Bulgaria. The objects were analyzed and mapped acco… Show more

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Cited by 4 publications
(6 citation statements)
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“…Figure 16 (A, B) SAR images in dB SAR surface profiles cover the areas of interest (figure 17) and are in two polarizations to demonstrate that there is a difference in values, for homogeneous areas it is more appropriate to use vh, the presence of flooded areas vv polarization 41,42,43,44 . The difference in moisture is clearly visible (figure 18).…”
Section: B) Gorna Mahalamentioning
confidence: 99%
“…Figure 16 (A, B) SAR images in dB SAR surface profiles cover the areas of interest (figure 17) and are in two polarizations to demonstrate that there is a difference in values, for homogeneous areas it is more appropriate to use vh, the presence of flooded areas vv polarization 41,42,43,44 . The difference in moisture is clearly visible (figure 18).…”
Section: B) Gorna Mahalamentioning
confidence: 99%
“…, where σ is the microwave reflectance coefficient for time instant t1 (satellite image of earlier date ) and for time instant (satellite image of later date ), i, j are the row and column numbers of pixels in a given SAR image, and is the relative soil moisture content reported for the corresponding period between two images of one polarization. This mathematical approach was used between four images, showing promising results in identifying areas of moderate and high change in vegetation, wet snow, ice, and water 24,25,26 . The values above 2 register serious changes in the reflectance of a given object in selected areas, and low values below 1.0 indicate little or no change in an object's reflectance.…”
Section: Data Processingmentioning
confidence: 99%
“…The availability of ground-based data in addition allows effective and cost-effective monitoring of climate change in remote areas using SAR data. The SAR C-band enables the effective study of various objects [5][6][7][8][9][10][11][12][13][14][15] and especially wet snow and ice 3,4,[16][17][18][19] . Using SAR data, we studied the type of changes in the digital value of the reflected signal (Q) from various objects, including water in different phase states.…”
Section: Introductionmentioning
confidence: 99%
“…Using SAR data, we studied the type of changes in the digital value of the reflected signal (Q) from various objects, including water in different phase states. For the study of vegetation [20][21][22][23][24]26,27 (herbaceous sp., lichens, and mosses), water 16,25 (in all aggregate states), and soils 26,27 , numerous optical indices have been used to demonstrate the changes occurring in them. Most of the indices are developed to monitor vegetation but they could also be informative for detecting changes in other types of objects, especially in their transition stages.…”
Section: Introductionmentioning
confidence: 99%