Pub Date : 2022-12-20DOI: 10.54668/2789-6323-2022-105-2-25-31
S.B. Kalabaev
The article is devoted to the study of morphometric features of lakes located on the territory of Karakalpakstan. At the same time, the standard Google Earth platform and SAS Planet software were used. Fluctuations in the levels and areas of lake mirrors depending on the water content of the Amu Darya River are revealed. At the next stage of the research, the water balance of the lake was studied. The study of the elements of the water balance of the lakes of the Southern Aral Sea region makes it possible to determine trends towards a decrease or increase in their water volume over a calculated time interval.
{"title":"MORPHOMETRIC PARAMETERS OF LAKES IN AREA OF THE SOUTHERN ARAL (FOR EXAMPLE SHEGEKUL LAKE)","authors":"S.B. Kalabaev","doi":"10.54668/2789-6323-2022-105-2-25-31","DOIUrl":"https://doi.org/10.54668/2789-6323-2022-105-2-25-31","url":null,"abstract":"The article is devoted to the study of morphometric features of lakes located on the territory of Karakalpakstan. At the same time, the standard Google Earth platform and SAS Planet software were used. Fluctuations in the levels and areas of lake mirrors depending on the water content of the Amu Darya River are revealed. At the next stage of the research, the water balance of the lake was studied. The study of the elements of the water balance of the lakes of the Southern Aral Sea region makes it possible to determine trends towards a decrease or increase in their water volume over a calculated time interval.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"45 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"121955643","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-12-20DOI: 10.54668/2789-6323-2022-105-2-47-58
Y. Beldeubayev, D. Kissebayev
In this paper we are considering the processes of ice destruction on Balkash Lake during extremely warm months. A significant correlation found between the average monthly air temperature of March and the dates of ice destruction beginning, complete freezing ending and water clear of ice. The Bagrov-Tokarev anomaly criterion for March was calculated and the extreme months were determined. The features of ice destruction during the spring season for the years with extremely warm months were analyzed. The number of days with certain types of ice phenomena are calculated, the various types of ice phenomena were analyzed for extremely warm months. The maps of ice thickness distribution were compiled. The deviation of the dates of ice destruction beginning, complete freezing ending and water clear of ice from the averages dates in extremely warm months was found. The data source were hydrological guides, monthly average air temperature data, and data reanalysis using the CDS Copernicus climate database of the European Center.
{"title":"FEATURES OF SPRING ICE PHENOMENA ON BALKASH LAKE IN EXTREMELY WARM MONTHS","authors":"Y. Beldeubayev, D. Kissebayev","doi":"10.54668/2789-6323-2022-105-2-47-58","DOIUrl":"https://doi.org/10.54668/2789-6323-2022-105-2-47-58","url":null,"abstract":"In this paper we are considering the processes of ice destruction on Balkash Lake during extremely warm months. A significant correlation found between the average monthly air temperature of March and the dates of ice destruction beginning, complete freezing ending and water clear of ice. The Bagrov-Tokarev anomaly criterion for March was calculated and the extreme months were determined. The features of ice destruction during the spring season for the years with extremely warm months were analyzed. The number of days with certain types of ice phenomena are calculated, the various types of ice phenomena were analyzed for extremely warm months. The maps of ice thickness distribution were compiled. The deviation of the dates of ice destruction beginning, complete freezing ending and water clear of ice from the averages dates in extremely warm months was found. The data source were hydrological guides, monthly average air temperature data, and data reanalysis using the CDS Copernicus climate database of the European Center.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"26 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125629745","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-12-20DOI: 10.54668/2789-6323-2022-105-2-59-77
B. Stepanov, R. K. Yafyazova
The characteristics of each local volume of debris flow are continuously changing depending on the characteristics: a path of its movement (slope, width and roughness of channel), dis-charge, granulometric and mineralogical compositions of debris involved in debris-flow-formation, density, viscosity and plasticity of debris-flow mass, etc. Up to now, it believes that the debris-flow mass density depends unambiguously on the slope of path of a debris-flow. As a result of experimental and theoretical studies carried out at the Kazakh Research Hydrometeorological Institute (KazNIGMI), it was found that the course of the debris-flow process depends on the density of debris-flow mass. Identification of the ambiguity of the debris-flow mass density from the slope of the debris flow path led to the discovery of a nat-ural phenomenon: an abrupt change of the density of debris-flow mass when the critical val-ue of the slope of the debris flow path is exceeded (the Stepanov’s effect). Taking into ac-count the ambiguity of the debris-flow mass density from the slope of the debris flow path is a key element in computing debris flow characteristics.
{"title":"THE PHENOMENON OF AN EPOSITIVE INCREASE IN THE DENSITY OF THE MURDER MASS – THE CONSEQUENCE OF ITS AMBIGUOUS DEPENDENCE ON THE SLOPE WAYS OF MOVEMENT","authors":"B. Stepanov, R. K. Yafyazova","doi":"10.54668/2789-6323-2022-105-2-59-77","DOIUrl":"https://doi.org/10.54668/2789-6323-2022-105-2-59-77","url":null,"abstract":"The characteristics of each local volume of debris flow are continuously changing depending on the characteristics: a path of its movement (slope, width and roughness of channel), dis-charge, granulometric and mineralogical compositions of debris involved in debris-flow-formation, density, viscosity and plasticity of debris-flow mass, etc. Up to now, it believes that the debris-flow mass density depends unambiguously on the slope of path of a debris-flow. As a result of experimental and theoretical studies carried out at the Kazakh Research Hydrometeorological Institute (KazNIGMI), it was found that the course of the debris-flow process depends on the density of debris-flow mass. Identification of the ambiguity of the debris-flow mass density from the slope of the debris flow path led to the discovery of a nat-ural phenomenon: an abrupt change of the density of debris-flow mass when the critical val-ue of the slope of the debris flow path is exceeded (the Stepanov’s effect). Taking into ac-count the ambiguity of the debris-flow mass density from the slope of the debris flow path is a key element in computing debris flow characteristics.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"55 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127823643","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-12-20DOI: 10.54668/2789-6323-2022-105-2-32-46
Z. Mustafayev, A. Kozykeyeva, S. Dauletbay
An analysis of changes in the hydrological indicators of the catchment area of the transboundary Shu River basin in the spatio-temporal aspect, based on information and analytical materials from the hy-drological posts of Kochkarka, Orto-Tokai, Milyanfan, Tashotkol, the Furmanovs hydroelectric com-plex and Ulanbel in a long period of observations covering 1931…2020, shows the presence of their constant fluctuations over the years under the influence of natural and anthropogenic factors. The hy-drological regime of the catchment area of the transboundary Shu River basin on a spatio-temporal scale with a positive or negative trend in the average annual water discharge is determined by the gen-eral nature of natural factors and changes due to increased anthropogenic activity on river systems. The results obtained indicate that the influence of natural and anthropogenic factors are less pronounced in the mountainous and foothill geographic zones than in the foothill-plain and desert zones of the catch-ment area of the transboundary river Shu.
{"title":"HYDROLOGICAL PROFILE OF THE DRAINAGE COLLECTION OF THE TRANS-BOUNDARY SHU RIVER BASIN","authors":"Z. Mustafayev, A. Kozykeyeva, S. Dauletbay","doi":"10.54668/2789-6323-2022-105-2-32-46","DOIUrl":"https://doi.org/10.54668/2789-6323-2022-105-2-32-46","url":null,"abstract":"An analysis of changes in the hydrological indicators of the catchment area of the transboundary Shu River basin in the spatio-temporal aspect, based on information and analytical materials from the hy-drological posts of Kochkarka, Orto-Tokai, Milyanfan, Tashotkol, the Furmanovs hydroelectric com-plex and Ulanbel in a long period of observations covering 1931…2020, shows the presence of their constant fluctuations over the years under the influence of natural and anthropogenic factors. The hy-drological regime of the catchment area of the transboundary Shu River basin on a spatio-temporal scale with a positive or negative trend in the average annual water discharge is determined by the gen-eral nature of natural factors and changes due to increased anthropogenic activity on river systems. The results obtained indicate that the influence of natural and anthropogenic factors are less pronounced in the mountainous and foothill geographic zones than in the foothill-plain and desert zones of the catch-ment area of the transboundary river Shu.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"15 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-12-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128493711","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-28DOI: 10.54668/2789-6323-2022-104-1-83-94
A. Karimov
Water-saving forms a base for reallocation of water resources and more balanced integrated development of economic sectors of Central Asian countries. Implementation of water-saving programs can highly contribute to objectives laid down in the Strategic Scheme of Integrated Use and Protection of Water Resources of the Republic of Kazakhstan. All three scenarios of water and land use studied in the scheme relay on water-saving, however an approach of water-saving is not clarified. This study discusses benefits and shortages of potential approaches to achieve water-saving at a basin scale using lessons from countries implemented basin scale water-saving projects. Three water use accounting methods discussed are as follows: (a) accounting efficiency; (б) accounting water use; (с) accounting water consumption. It is argued that the strategic scheme has to relay on real water-savings to meet growing water demand of different sectors of the economy.
{"title":"CCOUNTING WATER USE OR WATER CONSUMPTION – WHERE THE WAY TO WATER-SAVING?","authors":"A. Karimov","doi":"10.54668/2789-6323-2022-104-1-83-94","DOIUrl":"https://doi.org/10.54668/2789-6323-2022-104-1-83-94","url":null,"abstract":"Water-saving forms a base for reallocation of water resources and more balanced integrated development of economic sectors of Central Asian countries. Implementation of water-saving programs can highly contribute to objectives laid down in the Strategic Scheme of Integrated Use and Protection of Water Resources of the Republic of Kazakhstan. All three scenarios of water and land use studied in the scheme relay on water-saving, however an approach of water-saving is not clarified. This study discusses benefits and shortages of potential approaches to achieve water-saving at a basin scale using lessons from countries implemented basin scale water-saving projects. Three water use accounting methods discussed are as follows: (a) accounting efficiency; (б) accounting water use; (с) accounting water consumption. It is argued that the strategic scheme has to relay on real water-savings to meet growing water demand of different sectors of the economy.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"105 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-06-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114648436","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-28DOI: 10.54668/2789-6323-2022-104-1-103-114
B. Kerimbay
The study is based on a geosystem-basin approach, a method for determining the seasonal rhythm of the annual cycle, processing data from remote sensing of the Earth (ERS) and global monitoring in the integrated modules web browser of the digital platform (EOS). Spatial-temporal and seasonal linear NDVI series of key areas of high-mountain geosystems of the Sharyn river basin were constructed, and seasonal rhythms of the annual cycle were determined based on analytical data. As a result, a classification of the seasonal structure of the annual cycle was compiled, were revealedand the variability and dynamics of the geosystems of the nival-glacial belt above the snow line (3601...4100 m) and the high mountain belt (2601...3600 m).
{"title":"DYNAMICS AND VARIABILITY OF HIGH-MOUNTAIN GEOSYSTEMS OF THE SHARYN RIVER BASIN","authors":"B. Kerimbay","doi":"10.54668/2789-6323-2022-104-1-103-114","DOIUrl":"https://doi.org/10.54668/2789-6323-2022-104-1-103-114","url":null,"abstract":"The study is based on a geosystem-basin approach, a method for determining the seasonal rhythm of the annual cycle, processing data from remote sensing of the Earth (ERS) and global monitoring in the integrated modules web browser of the digital platform (EOS). Spatial-temporal and seasonal linear NDVI series of key areas of high-mountain geosystems of the Sharyn river basin were constructed, and seasonal rhythms of the annual cycle were determined based on analytical data. As a result, a classification of the seasonal structure of the annual cycle was compiled, were revealedand the variability and dynamics of the geosystems of the nival-glacial belt above the snow line (3601...4100 m) and the high mountain belt (2601...3600 m).","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"11 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-06-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126364224","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-28DOI: 10.54668/2789-6323-2022-104-1-17-30
A. Bazbekova, A. Kauazov
The article analyzes quantitative indicators of severity and favorability of the weather for the meteorological stations of Almaty and Nur-Sultan from 2015 to 2020 for the warm (аpril-september) and cold (october-march) seasons of the year. The equivalent-effective temperature index, the Sayple wind cooling index and the Bodman severity index were obtained. During the quantitative assessment, it was found that winter in the city of Nur-Sultan is 1.7 times more severe, and wind cooling is 2.7 times more significant than in the city of Almaty. Weather indicators on the EET index characterize the conditions in Nur-Sultan as less favorable compared to Almaty. It is shown that the equivalent-effective temperature index is the most preferable for assessing the comfort of the weather.
{"title":"BIOCLIMATIC ASSESSMENT OF FAVORABLE WEATHER CONDITIONS IN ALMATY AND NUR-SULTAN","authors":"A. Bazbekova, A. Kauazov","doi":"10.54668/2789-6323-2022-104-1-17-30","DOIUrl":"https://doi.org/10.54668/2789-6323-2022-104-1-17-30","url":null,"abstract":"The article analyzes quantitative indicators of severity and favorability of the weather for the meteorological stations of Almaty and Nur-Sultan from 2015 to 2020 for the warm (аpril-september) and cold (october-march) seasons of the year. The equivalent-effective temperature index, the Sayple wind cooling index and the Bodman severity index were obtained. During the quantitative assessment, it was found that winter in the city of Nur-Sultan is 1.7 times more severe, and wind cooling is 2.7 times more significant than in the city of Almaty. Weather indicators on the EET index characterize the conditions in Nur-Sultan as less favorable compared to Almaty. It is shown that the equivalent-effective temperature index is the most preferable for assessing the comfort of the weather.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"26 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-06-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125924830","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-28DOI: 10.54668/2789-6323-2022-104-1-40-49
B. Aitymova, A. Pshenchinova, N. Abayev
The study presents results of assessing the resources of the river flow of the Tobyl - Torgai water management basin. The purpose of the work is to update the previously developed methodology for assessing the annual runoff resources of individual rivers and river runoff resources of the considered water management basin of the Republic of Kazakhstan. The calculations used the average monthly and average annual water discharge of the main rivers. Methods have been developed for determining and restoring the observed and natural runoff, long-term statistical characteristics and its values of probability of exceeding. The equations for determining the water resources of local runoff and water resources coming from other regions are obtained. As a result of the work done on the preliminary calculation, the total surface water resources for the Tobyl – Torgai water management basin, formed in Kazakhstan and coming from the territory of the Russian Federation for a long-term period from 1931 to 2019, on average amount to 1,67 km3, of which: resources formed within Kazakhstan - 1,33 km3, inflow – 0,34 km3. The runoff formed in the territory of the basin, for the disturbed period, relative to the conditionally natural period, decreased by 8%, the runoff coming from the Russian Federation decreased by 12%, and the total water resources by 9%
{"title":"DYNAMICS OF CHANGES IN THE RESOURCES OF THE RIVER FLOW OF THE TOBYL -TORGAI WATER BASIN","authors":"B. Aitymova, A. Pshenchinova, N. Abayev","doi":"10.54668/2789-6323-2022-104-1-40-49","DOIUrl":"https://doi.org/10.54668/2789-6323-2022-104-1-40-49","url":null,"abstract":"The study presents results of assessing the resources of the river flow of the Tobyl - Torgai water management basin. The purpose of the work is to update the previously developed methodology for assessing the annual runoff resources of individual rivers and river runoff resources of the considered water management basin of the Republic of Kazakhstan. The calculations used the average monthly and average annual water discharge of the main rivers. Methods have been developed for determining and restoring the observed and natural runoff, long-term statistical characteristics and its values of probability of exceeding. The equations for determining the water resources of local runoff and water resources coming from other regions are obtained. As a result of the work done on the preliminary calculation, the total surface water resources for the Tobyl – Torgai water management basin, formed in Kazakhstan and coming from the territory of the Russian Federation for a long-term period from 1931 to 2019, on average amount to 1,67 km3, of which: resources formed within Kazakhstan - 1,33 km3, inflow – 0,34 km3. The runoff formed in the territory of the basin, for the disturbed period, relative to the conditionally natural period, decreased by 8%, the runoff coming from the Russian Federation decreased by 12%, and the total water resources by 9%","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"18 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-06-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126366579","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-28DOI: 10.54668/2789-6323-2022-104-1-115-128
M. Burlibayev, A. Saparova
The article changes the question of the mineralization of the Kazakh part of the Syrdarya River. The hydrological posts Kokbulak were chosen as the main creators, which is a border post for assessing the degree of mineralization of pine from the side of Uzbekistan and Kazaly, which in turn is the closure of the creator, taking into account the needs of the river ecosystem of the lower reaches and the Aral Sea. The article analyzes the changes in the total mineralization and the main ions of the Kazakhstani part of the river. Syrdarya, depending on the water content of the year (25%, 50%, 75%, 95% availability) both for periods with a conditionally natural and disturbed regime. A general analysis of changes in the intra-annual total distribution of minerals and groups of basic ions showed that at an important level, i.e. in the disturbed period of the absence of winter maxima and summer minima, there was more room for stochasticity alien to the conditionally natural period of the hydrological regime.
{"title":"FEATURES OF MINERALIZATION OF THE KAZAKHSTAN PART OF THE SYRDARIA RIVERKAZAKHSTAN","authors":"M. Burlibayev, A. Saparova","doi":"10.54668/2789-6323-2022-104-1-115-128","DOIUrl":"https://doi.org/10.54668/2789-6323-2022-104-1-115-128","url":null,"abstract":"The article changes the question of the mineralization of the Kazakh part of the Syrdarya River. The hydrological posts Kokbulak were chosen as the main creators, which is a border post for assessing the degree of mineralization of pine from the side of Uzbekistan and Kazaly, which in turn is the closure of the creator, taking into account the needs of the river ecosystem of the lower reaches and the Aral Sea. The article analyzes the changes in the total mineralization and the main ions of the Kazakhstani part of the river. Syrdarya, depending on the water content of the year (25%, 50%, 75%, 95% availability) both for periods with a conditionally natural and disturbed regime. A general analysis of changes in the intra-annual total distribution of minerals and groups of basic ions showed that at an important level, i.e. in the disturbed period of the absence of winter maxima and summer minima, there was more room for stochasticity alien to the conditionally natural period of the hydrological regime.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"88 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-06-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115624872","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-28DOI: 10.54668/2789-6323-2022-104-1-50-64
Z. Mustafayev, A. Kozykeyeva, S. Dauletbay
Based on the analysis of long-term information and analytical materials, the National Statistical Committee of the Kyrgyz Republic and the Bureau of National Statistics of the Agency for Statistical Planning and Reforms of the Republic of Kazakhstan on the economic use of the catchment area of the transboundary Shu River Basin conducted an assessment of the indirect anthropogenic load based on indicators of areal and linear-network impacts (demographic, agricultural and industrial) in the context of water management areas and administrative regions.
{"title":"COMPREHENSIVE ASSESSMENT OF INDIRECT EFFECTS OF HUMAN ANTHROPOGENIC ACTIVITIES ON THE WATER CATCHMENT OF THE SHU RIVER BASIN","authors":"Z. Mustafayev, A. Kozykeyeva, S. Dauletbay","doi":"10.54668/2789-6323-2022-104-1-50-64","DOIUrl":"https://doi.org/10.54668/2789-6323-2022-104-1-50-64","url":null,"abstract":"Based on the analysis of long-term information and analytical materials, the National Statistical Committee of the Kyrgyz Republic and the Bureau of National Statistics of the Agency for Statistical Planning and Reforms of the Republic of Kazakhstan on the economic use of the catchment area of the transboundary Shu River Basin conducted an assessment of the indirect anthropogenic load based on indicators of areal and linear-network impacts (demographic, agricultural and industrial) in the context of water management areas and administrative regions.","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"10 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2022-06-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134092084","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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