North Liadeshti Glacier
Let us consider the retreat of the North Liadesh glacier of the Enguri basin using the SRS. Let us compare the resulting contour with the glacier contour shown on the topographic map. We found that the area of the North Liadesh glaciers according to the TDS is 3.4 km2, while the catalogue gives the same value, which indicates that there is an inaccuracy in the catalogue. Correction with the topographic map deter­mi­ned that its area was 4.3 km2.
A detailed analysis of the retreat of the North Liadesh glacier showed that the glacier retreat is described by a parabolic curve:

                                                                   Y = 0.1321 x2+7.148 x-12
a
b
North Liadesti Glacier: a − Schematic representation of retreat, shown against the background of a September 29, 2020 image from the SPOT 6 satellite; b − Retreat graph
Kvishi Glacier
The Kvishi Glacier is the next large glacier in the Enguri Glacial Basin, from west to east, which needs to be studied. Similarly, as in the previous cases, let us consider its retreat and obtain that the glacier retreat is described by a parabolic curve:
                                                                 Y = 0.5138 x2+3.2826 x   
a
b
Kvishi Glacier: a − Schematic image of glacier retreat; b − Retreat graph
Adishi Glacier
a
b
Adishi Glacier: a − Schematic image of retreat against the background of the Landsat 8 OLI TIRS sensor image of August 25, 2022. Green pins show the results obtained based on field expeditions; b − Graphs comparing the ground data of the SRS and field observations
Shkhara Glacier
To determine the contours of the retreat of the Shkhara glacier, data from various Landsat satellite sensors were used for the time points indicated on the drawing.
The picture shows a schematic image of the retreat of the Shkhara glacier against the background of the Landsat 9 OLI TIRS sensor image of September 18, 2022. Additionally, on the same image the locations of glacier determined based on GBO with green pins are shown.

Using the SRS data,  the location of glaciers at different points in time has been determined, which are shown by contours of different colors on the schematic image of retreat. The contours have been drawn using manual digitization. The numerical value of glacier Shkhara retreat is calculated by means of the white dashed line crossing the contours. Based on these values retreat graph is created and corresponding trend is shown. As indicated in the drawing, the initial state of the Shkhara Glacier corresponds to 1986.
The conducted analysis showed that the nonlinear retreat of the Shkhara Glacier is described with high accuracy by a second-order polynomial, which in this case is a parabola. The Shkhara Glacier retreat graph constructed based on the field expedition data used for the quality assessment and control of the results is also described with high accuracy by a parabolic curve. As can be seen from graphs comparing the ground data of the SRS and field observations
, the ground-based data of the Shkhara Glacier SRS and field observations are in good agreement with each other.
a
b
Shkhara Glacier: a − Schematic image of retreat against the background of the Landsat 9 OLI TIRS sensor image of September 18, 2022. Green pins show the results obtained based on field expeditions; b − Graphs comparing the ground data of the SRS and field observations.
The retreat of the Shkhara glacier based on SRS is given by the equation:
Y = 0.1868x2 + 4.0426x – 5.4252                                                                                        
Using GBO the corresponding equation is:
          Y = 0.13x2 + 5.0426x - 5.4252  
The comparison of these equations and consequently of the obtained analytical equations shows that they are in good agreement with each other, which confirms the relevance of using GBO for QA/QC of  the results
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