Pub Date : 2021-01-01DOI: 10.31857/s0435428121030056
В. А. Иванов, Сергей Романович Чалов
{"title":"ОЦЕНКА БАЛАНСА НАНОСОВ РЕК ОБЬ И ЕНИСЕЙ","authors":"В. А. Иванов, Сергей Романович Чалов","doi":"10.31857/s0435428121030056","DOIUrl":"https://doi.org/10.31857/s0435428121030056","url":null,"abstract":"","PeriodicalId":35940,"journal":{"name":"Geomorfologiya","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69739185","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 : 2021-01-01DOI: 10.31857/s043542812103010x
Ф. А. Романенко, Е А Балдина, Н. Н. Луговой, Е. Ю. Жданова
{"title":"ДИНАМИКА БЕРЕГОВ ОСТРОВОВ СЕВЕРНОЙ ЧАСТИ КАРСКОГО МОРЯ (ст. 1. Остров Ушакова)","authors":"Ф. А. Романенко, Е А Балдина, Н. Н. Луговой, Е. Ю. Жданова","doi":"10.31857/s043542812103010x","DOIUrl":"https://doi.org/10.31857/s043542812103010x","url":null,"abstract":"","PeriodicalId":35940,"journal":{"name":"Geomorfologiya","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69739691","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 : 2021-01-01DOI: 10.31857/s0435428121030032
Р. С. Чалов, А. С. Чалова, Г. Б. Голубцов
{"title":"О ТЕРМИНОЛОГИИ И КЛАССИФИКАЦИИ РАЗВЕТВЛЕНИЙ РУСЕЛ РАВНИННЫХ РЕК","authors":"Р. С. Чалов, А. С. Чалова, Г. Б. Голубцов","doi":"10.31857/s0435428121030032","DOIUrl":"https://doi.org/10.31857/s0435428121030032","url":null,"abstract":"","PeriodicalId":35940,"journal":{"name":"Geomorfologiya","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69739211","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 : 2021-01-01DOI: 10.31857/s0435428121040052
А. Ю. Сидорчук, О. К. Борисова, Nikolay Kovaliukh, Алексей Викторович Панин, Александр Викторович Чернов
{"title":"МОРФОЛОГИЯ И ИСТОРИЯ РАЗВИТИЯ ДОЛИНЫ РЕКИ МОСКВЫ В ПОЗДНЕЛЕДНИКОВЬЕ И ГОЛОЦЕНЕ","authors":"А. Ю. Сидорчук, О. К. Борисова, Nikolay Kovaliukh, Алексей Викторович Панин, Александр Викторович Чернов","doi":"10.31857/s0435428121040052","DOIUrl":"https://doi.org/10.31857/s0435428121040052","url":null,"abstract":"","PeriodicalId":35940,"journal":{"name":"Geomorfologiya","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69739422","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 : 2021-01-01DOI: 10.31857/s0435428121040040
Д.С. Хомченко, Т.А. Янина, О. К. Борисова, Р. Н. Курбанов, В.Р. Беляев, Е.В. Гаранкина, А.А. Бердникова, Н.Г. Константинова, А.И. Рудинская
{"title":"ИСТОРИЯ ФОРМИРОВАНИЯ РЕЛЬЕФА ЗАПАДНОЙ ЧАСТИ ТУРАНО-УЮКСКОЙ КОТЛОВИНЫ (ТУВИНСКОЕ НАГОРЬЕ) В ПОЗДНЕМ ПЛЕЙСТОЦЕНЕ","authors":"Д.С. Хомченко, Т.А. Янина, О. К. Борисова, Р. Н. Курбанов, В.Р. Беляев, Е.В. Гаранкина, А.А. Бердникова, Н.Г. Константинова, А.И. Рудинская","doi":"10.31857/s0435428121040040","DOIUrl":"https://doi.org/10.31857/s0435428121040040","url":null,"abstract":"","PeriodicalId":35940,"journal":{"name":"Geomorfologiya","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69739730","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 : 2021-01-01DOI: 10.31857/s0435428121030044
И. Ю. Григорьев, Иван Иванович Рысин
{"title":"ОЦЕНКА ЛИНЕЙНОГО И ПЛОЩАДНОГО ПРИРОСТА ОВРАГОВ С ПРИМЕНЕНИЕМ ИНСТРУМЕНТАЛЬНЫХ МЕТОДОВ (НА ТЕРРИТОРИИ УДМУРТИИ)","authors":"И. Ю. Григорьев, Иван Иванович Рысин","doi":"10.31857/s0435428121030044","DOIUrl":"https://doi.org/10.31857/s0435428121030044","url":null,"abstract":"","PeriodicalId":35940,"journal":{"name":"Geomorfologiya","volume":"1 1","pages":""},"PeriodicalIF":0.0,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"69739090","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 : 2019-11-08DOI: 10.31857/s0435-42812019427-39
G. Rychagov
The main focus of the article is the significance of the geomorphological method for the reconstruction of paleogeographic events that took place in the Late Pleistocene and Holocene. The specific data obtained as a result of applying this method are given. A reasonable curve of the Caspian Sea level fluctuations in the Holocene was compiled. A risk zone has been defined, within which the level of the Caspian Sea will fluctuate in the future, under modern physics-geographical conditions, which is fundamental importance when planning any economic measures in the coastal zone. Predictions were made and later justified of the Caspian Sea level fluctuations in the 20thearly 21st centuries. The climatic nature of the Caspian transgressions was confirmed. Obtained were new data on the evolution of the shores of the Caspian Sea under rising level conditions, which can be used when forecasting the development of the shores of other seas in the conditions of the present-day rise of the World Ocean level.
{"title":"To the methods of geomorphological research (geomorphological lessons of the Caspian)","authors":"G. Rychagov","doi":"10.31857/s0435-42812019427-39","DOIUrl":"https://doi.org/10.31857/s0435-42812019427-39","url":null,"abstract":"The main focus of the article is the significance of the geomorphological method for the reconstruction of paleogeographic events that took place in the Late Pleistocene and Holocene. The specific data obtained as a result of applying this method are given. A reasonable curve of the Caspian Sea level fluctuations in the Holocene was compiled. A risk zone has been defined, within which the level of the Caspian Sea will fluctuate in the future, under modern physics-geographical conditions, which is fundamental importance when planning any economic measures in the coastal zone. Predictions were made and later justified of the Caspian Sea level fluctuations in the 20thearly 21st centuries. The climatic nature of the Caspian transgressions was confirmed. Obtained were new data on the evolution of the shores of the Caspian Sea under rising level conditions, which can be used when forecasting the development of the shores of other seas in the conditions of the present-day rise of the World Ocean level.","PeriodicalId":35940,"journal":{"name":"Geomorfologiya","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-11-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43895698","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 : 2019-11-08DOI: 10.31857/s0435-42812019440-48
D. Korzinin, Д В Корзинин, I. Leont’yev, И О Леонтьев, M. Shtremel, М Н Штремель
Central part of Narva bay is characterized by accretive coast, which is formed due to the presence of significant volumes of sand deposits. In the paper, the current state of coastal relief was analyzed and the forecast of its evolution under the prevailing wave climate was performed. The problem of the equilibrium of the coastal morphosystem for a given sediment budget and the probable trend of relative sea level was considered. Morphodynamic forecast for the period of the next decades was justified for designing the crossing of the coastal zone by the main pipeline route. Increasing of the role of accumulation processes from the south to the north has been identified through the field survey and analysis of satellite images, and has been shown by the nature of the beach relief and the underwater coastal slope. The calculation of the longshore sediment drift revealed the existence of a convergence zone for two differently directed sediment flows. Convergence of the sediment flows leads to accumulation of sand deposits at the rate of 19.0 m3 per one running meter per year. Estimates of the sediment budget resulted in the estimation of the accumulation rate at 8 m3 per one running meter per year in the coastal zone of area of the pipeline route. Sand accumulation leads to coastal accretion at the rate of 1 m per year. The obtained results lead to the conclusion on the stability of the coast in the coming decades unless the change of the sources of sand sediments and tendencies of its transport.
{"title":"Coastal dynamics in the Narva bay of the Baltic sea: present-day state and development tendencies","authors":"D. Korzinin, Д В Корзинин, I. Leont’yev, И О Леонтьев, M. Shtremel, М Н Штремель","doi":"10.31857/s0435-42812019440-48","DOIUrl":"https://doi.org/10.31857/s0435-42812019440-48","url":null,"abstract":"Central part of Narva bay is characterized by accretive coast, which is formed due to the presence of significant volumes of sand deposits. In the paper, the current state of coastal relief was analyzed and the forecast of its evolution under the prevailing wave climate was performed. The problem of the equilibrium of the coastal morphosystem for a given sediment budget and the probable trend of relative sea level was considered. Morphodynamic forecast for the period of the next decades was justified for designing the crossing of the coastal zone by the main pipeline route. Increasing of the role of accumulation processes from the south to the north has been identified through the field survey and analysis of satellite images, and has been shown by the nature of the beach relief and the underwater coastal slope. The calculation of the longshore sediment drift revealed the existence of a convergence zone for two differently directed sediment flows. Convergence of the sediment flows leads to accumulation of sand deposits at the rate of 19.0 m3 per one running meter per year. Estimates of the sediment budget resulted in the estimation of the accumulation rate at 8 m3 per one running meter per year in the coastal zone of area of the pipeline route. Sand accumulation leads to coastal accretion at the rate of 1 m per year. The obtained results lead to the conclusion on the stability of the coast in the coming decades unless the change of the sources of sand sediments and tendencies of its transport.","PeriodicalId":35940,"journal":{"name":"Geomorfologiya","volume":" ","pages":""},"PeriodicalIF":0.0,"publicationDate":"2019-11-08","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"47471287","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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