Abstract:The GRACE gravity satellite mission has provided monthly gravity field solutions for about 15 years enabling a unique opportunity to monitor large scale mass variation processes. By the end of the GRACE, the GRACE-FO mission was launched in order to continue the time series of monthly gravity fields. The two missions are similar in most aspects apart from the improved intersatellite range rate measurements, which is performed with lasers in addition to microwaves. An obvious demand for the geoscientific applic… Show more
“…This study is a continuation and a refinement of the work of Földváry et al [5]. According to Figure 6 of Földváry et al [5] in the reservoir of the Aral Sea, the correlation between water volume change and gravity anomaly was found to be 0.8636, which is a quite convincing relationship.…”
Section: Introductionsupporting
confidence: 74%
“…This study is a continuation and a refinement of the work of Földváry et al [5]. According to Figure 6 of Földváry et al [5] in the reservoir of the Aral Sea, the correlation between water volume change and gravity anomaly was found to be 0.8636, which is a quite convincing relationship. However, from 2002 to about mid-2005, an increase in gravity anomaly was determined, which is opposite to the water volume change tendencies.…”
Section: Introductionsupporting
confidence: 74%
“…In Földváry et al [5] gravity anomaly time series have been determined for the period of April 2002 to November 2019. The present study has been extended until January 2022.…”
Section: Resultsmentioning
confidence: 99%
“…Subsequently, a linear trend on the resulting time series has been fitted to capture longterm mass variations. The resulting trends are visualized in Figure 1 [5]. Clearly, mass variations of the Caspian Sea have an impact on the gravity anomaly variations of the Aral Sea.…”
The GRACE large-scale sequent GRACE-FO gravity satellite mission is providing monthly gravity field solutions for almost 20 years enabling a unique opportunity to monitor large-scale mass variation processes. The gravity anomaly time series for the Aral Sea region has been derived for the period of April 2002 to January 2022. The method of determining gravity anomaly time series from GRACE and GRACE-FO monthly solutions has been improved by taking into account the mass variations of the Caspian Sea. The gravity anomaly time series then has been compared to mass anomaly estimates. For deriving mass anomaly, beyond the available water volume data, density variations were determined by taking into account salinity and temperature changes. Unfortunately, no reliable information either on the salinity or on water temperature changes is available or accessible. Furthermore, not only the data but also the methodology of determining the density is not reliable. Still, the tests suggest that slight improvement in correlation due to the involvement of salinity information occurs.
“…This study is a continuation and a refinement of the work of Földváry et al [5]. According to Figure 6 of Földváry et al [5] in the reservoir of the Aral Sea, the correlation between water volume change and gravity anomaly was found to be 0.8636, which is a quite convincing relationship.…”
Section: Introductionsupporting
confidence: 74%
“…This study is a continuation and a refinement of the work of Földváry et al [5]. According to Figure 6 of Földváry et al [5] in the reservoir of the Aral Sea, the correlation between water volume change and gravity anomaly was found to be 0.8636, which is a quite convincing relationship. However, from 2002 to about mid-2005, an increase in gravity anomaly was determined, which is opposite to the water volume change tendencies.…”
Section: Introductionsupporting
confidence: 74%
“…In Földváry et al [5] gravity anomaly time series have been determined for the period of April 2002 to November 2019. The present study has been extended until January 2022.…”
Section: Resultsmentioning
confidence: 99%
“…Subsequently, a linear trend on the resulting time series has been fitted to capture longterm mass variations. The resulting trends are visualized in Figure 1 [5]. Clearly, mass variations of the Caspian Sea have an impact on the gravity anomaly variations of the Aral Sea.…”
The GRACE large-scale sequent GRACE-FO gravity satellite mission is providing monthly gravity field solutions for almost 20 years enabling a unique opportunity to monitor large-scale mass variation processes. The gravity anomaly time series for the Aral Sea region has been derived for the period of April 2002 to January 2022. The method of determining gravity anomaly time series from GRACE and GRACE-FO monthly solutions has been improved by taking into account the mass variations of the Caspian Sea. The gravity anomaly time series then has been compared to mass anomaly estimates. For deriving mass anomaly, beyond the available water volume data, density variations were determined by taking into account salinity and temperature changes. Unfortunately, no reliable information either on the salinity or on water temperature changes is available or accessible. Furthermore, not only the data but also the methodology of determining the density is not reliable. Still, the tests suggest that slight improvement in correlation due to the involvement of salinity information occurs.
“…In particular, 11.5% of 1.08 million ha of irrigated land in Kyrgyzstan, 16.0% of 719,200 ha in Tajikistan, 33.0% of 2.31 million ha in Kazakhstan, 95.9% of 1.74 million ha in Turkmenistan, and around 50% of 4.28 million ha in Uzbekistan are prone to soil salinization at different levels [7][8]. Many scientists and experts in developed and developing countries have studied the relationship between the salinity levels of irrigated areas and groundwater levels and its mineralization, and other anthropogenic influences using and comparing GIS-based methods (interpolation, vegetation, and hydrological indices) [9][10][11].…”
The salinization of soils impacts many arid areas. In the world, about 62 million hectares of agricultural land are subject to salinization. At present, about 47% of the irrigated lands in Uzbekistan are subject to some degree of salinity. Landsat satellite photos taken across an exact time span (from 1993 to 2021) with timeframes of 8 to 10 years were utilized in this study to monitor soil salinity. To analyze soil salinity level, salinity index, and classification method using Google Earth was performed. During the entire study period, changes in the indicator of soil salinity improvement work were shown. Especially related to non-saline soil, which was around 4,670 ha in 1993, and it increased to 10,533 ha in 2021 and reached 19.2 % after thirty years. Slightly saline soil class has the propensity to decrease and included its largest area of 15,941 ha (52.1 %) in 1993, but then dropped quickly to 9,649 ha (31.5 %) in 2021. Saline soil maximum increased in 2001 to 10.251 ha (33.5 %), then started steadily contracting and reaches a minimum of 7,440 ha (24.3%) in 2011. Strongly saline soil starts reaching from 1,771 ha to 5,069 ha between 1993-2001.
The Gravity Recovery and Climate Experiment (GRACE) and its successor, the GRACE Follow-On (GRACE-FO) gravity satellite missions, have been providing monthly gravity field solutions for almost 20 years, enabling a unique opportunity to monitor large-scale mass variation processes. The gravity anomaly time series for the Aral Sea region has been obtained for the period of April 2002 to January 2022. The method of determining the gravity anomaly time series from GRACE and GRACE-FO monthly solutions has been improved by considering the mass variations of the Caspian Sea. The gravity anomaly time series was then compared to water mass changes determined by considering variations in the salinity and temperature of seawater. Nevertheless, the tests suggest that improvements in correlation with such information might occur, although the relevance of the improvement should not be overestimated. All in all, it can be demonstrated that salinity changes relevantly influence the gravity field; however, the signal is too weak to inversely obtain information from satellite-borne gravity observations on salinity variations.
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