{"title":"Floods, overflows and their management. Case studies on the lower course of the Ciorogârla River","authors":"Manuela Bărbărie","doi":"10.24193/RCJ2019_10","DOIUrl":"https://doi.org/10.24193/RCJ2019_10","url":null,"abstract":"","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":"9 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"124615657","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}
{"title":"Prospecting of Natural and Human Tourism Potential of Salaj County","authors":"Oana Moigrădean","doi":"10.24193/RCJ2019_2","DOIUrl":"https://doi.org/10.24193/RCJ2019_2","url":null,"abstract":"","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130121585","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}
{"title":"Climate risks in the Babadag Plateau, Dobrogea, Southeastern Romania","authors":"S. Sava","doi":"10.24193/RCJ2019_7","DOIUrl":"https://doi.org/10.24193/RCJ2019_7","url":null,"abstract":"","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":"102 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"132579737","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}
{"title":"GIS for spatial landslide distribution analysis in the Transylvanian Depression.","authors":"Gheorghe Roșian, C. Horváth","doi":"10.24193/RCJ2019_3","DOIUrl":"https://doi.org/10.24193/RCJ2019_3","url":null,"abstract":"","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":" 23","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2019-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"113946181","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}
Salaj county has a rich and diversified tourism potential induced by the water resources. This is related to the presence of mineral waters mainly sulfurous and thermal, which have been known and used since the previous century, the spectacular landscapes created by some peculiarities of the river valley and also to the presence of a few lakes. The tourism potential is not fully capitalized even though there are some spas where the healing properties of the mineral waters are used, while others have been turned into ruins and destroyed. The tourism potential of running waters is given by the presence of some spectacular valley sectors (gorges, canyons). Lakes attract the tourists especially for their fishing resources.
{"title":"Prospection and human facilities related to tourism of water resources in Sălaj county.","authors":"Oana Moigrădean","doi":"10.24193/RCJ2018_14","DOIUrl":"https://doi.org/10.24193/RCJ2018_14","url":null,"abstract":"Salaj county has a rich and diversified tourism potential induced by the water resources. This is related to the presence of mineral waters mainly sulfurous and thermal, which have been known and used since the previous century, the spectacular landscapes created by some peculiarities of the river valley and also to the presence of a few lakes. The tourism potential is not fully capitalized even though there are some spas where the healing properties of the mineral waters are used, while others have been turned into ruins and destroyed. The tourism potential of running waters is given by the presence of some spectacular valley sectors (gorges, canyons). Lakes attract the tourists especially for their fishing resources.","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":"130 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130330969","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}
Octavia Bogdan, Bucureşti Institutul de Geografie al Academiei Române
Climatic anomalies in Oltenia in the winter and spring of 2018. In the winter of 2017-2018 and the spring of 2018 at the level of the entire Northern Hemisphere a series of climatic anomalies occurred. As a result, such phenomena have also been recorded in Romania, and at regional level, in the southwest of the country, they have been specific. All the winter months were warm, and of these, December 2017 was the warmest with the monthly mean temperature for the Oltenia region of 2.7°C and the deviation from the previous century of 2.5°C, followed by the February with an average of 0.9°C and deviation from the previous century of 1.4°C and January with 0.8°C and a deviation of 3.4°C. In the spring months, the alternating climatic processes continued. Thus, during March, between 18-23.III.2018 there was a snowy period that had deposited a consistent layer of snow accompanied by low temperatures. This climatic process of late cooling of the weather and the return of winter phenomena has affected all of Eurasia. In Oltenia, it produced lower mean temperatures than normal with negative deviations from the normal last century (average for the whole region was 3.6°C and -1.0°C deviation.) March was pluviometric excessively rainy with the average for the entire region of 95.3 mm and the percentage deviation from the normal last century of 126.2% .The month of April was the warmest in the history of meteorological observations, and May was particularly warm after the deviations of the monthly mean temperature from normal. highlighting climate change in Oltenia, climate change and their consequences (Bogdan Octavia, Marinică I., Mic Loredana-Elena 2008, Bogdan Octavia & Marinică I. 2009, Bogdan Octavia, Marinică I., Marinică Andreea Floriana 2010, 2017; Ion Marinică, Andreea Floriana Marinică, 2016).
{"title":"Climatic anomalies in Oltenia in the winter and spring of 2018","authors":"Octavia Bogdan, Bucureşti Institutul de Geografie al Academiei Române","doi":"10.24193/rcj2018_18","DOIUrl":"https://doi.org/10.24193/rcj2018_18","url":null,"abstract":"Climatic anomalies in Oltenia in the winter and spring of 2018. In the winter of 2017-2018 and the spring of 2018 at the level of the entire Northern Hemisphere a series of climatic anomalies occurred. As a result, such phenomena have also been recorded in Romania, and at regional level, in the southwest of the country, they have been specific. All the winter months were warm, and of these, December 2017 was the warmest with the monthly mean temperature for the Oltenia region of 2.7°C and the deviation from the previous century of 2.5°C, followed by the February with an average of 0.9°C and deviation from the previous century of 1.4°C and January with 0.8°C and a deviation of 3.4°C. In the spring months, the alternating climatic processes continued. Thus, during March, between 18-23.III.2018 there was a snowy period that had deposited a consistent layer of snow accompanied by low temperatures. This climatic process of late cooling of the weather and the return of winter phenomena has affected all of Eurasia. In Oltenia, it produced lower mean temperatures than normal with negative deviations from the normal last century (average for the whole region was 3.6°C and -1.0°C deviation.) March was pluviometric excessively rainy with the average for the entire region of 95.3 mm and the percentage deviation from the normal last century of 126.2% .The month of April was the warmest in the history of meteorological observations, and May was particularly warm after the deviations of the monthly mean temperature from normal. highlighting climate change in Oltenia, climate change and their consequences (Bogdan Octavia, Marinică I., Mic Loredana-Elena 2008, Bogdan Octavia & Marinică I. 2009, Bogdan Octavia, Marinică I., Marinică Andreea Floriana 2010, 2017; Ion Marinică, Andreea Floriana Marinică, 2016).","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":"243 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127692587","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}
{"title":"The susceptibility of the Iara Depression to contemporary geomorphological processes","authors":"G. Rus","doi":"10.24193/rcj2018_17","DOIUrl":"https://doi.org/10.24193/rcj2018_17","url":null,"abstract":"","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":"35 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115837854","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}
Climate variability in the spring of 2018 in the south-west of Romania in the context of climate change. The paper analyses climatic variability in south-western Romania in the spring of 2018. After the warm winter, from the late winter phenomena with snow layer, recorded in March in the intervals 1-8.III and 19-27.III, it followed the warmest month of April, by temperature averages, throughout the history of climate observations, and the warm weather has continued throughout May. In March there was an absolute climatic record of the minimum temperature at Tg. Logrești of -24.8°C (1.III.2018). In April the weather was warm on most of the Northern Hemisphere except the North American continent. The temperature averages registered in April 2018 have become absolute climatic records not only in Oltenia but even in the whole country and an extended area on the European continent. In Oltenia, April was excessively droughty, but heavy rainfall in March provided the groundwater reserve throughout the month, although some cereal crops have been affected. April was warm in all Oltenia with a general average deviation of 2.5°C, and the rainfalls returned, but the drought continued in the Romanați Plain. Climatic variability was particularly high, the climate evolving from an extreme to the other, but nevertheless the statistical analysis of the climatic data shows that the climate warming continued. The paper is part of an extensive series of studies on climate variability in Oltenia and climatic risk phenomena (Bogdan, Marinica, Andreea Floriana Marinică 2010, 2017; Marinică, Andreea Floriana Marinică 2016) being useful to all interested in climate problems in the south-west Romania.
{"title":"Climate variability in the spring of 2018 in the south-west of Romania in the context of climate change","authors":"I. Marinică","doi":"10.24193/RCJ2018_19","DOIUrl":"https://doi.org/10.24193/RCJ2018_19","url":null,"abstract":"Climate variability in the spring of 2018 in the south-west of Romania in the context of climate change. The paper analyses climatic variability in south-western Romania in the spring of 2018. After the warm winter, from the late winter phenomena with snow layer, recorded in March in the intervals 1-8.III and 19-27.III, it followed the warmest month of April, by temperature averages, throughout the history of climate observations, and the warm weather has continued throughout May. In March there was an absolute climatic record of the minimum temperature at Tg. Logrești of -24.8°C (1.III.2018). In April the weather was warm on most of the Northern Hemisphere except the North American continent. The temperature averages registered in April 2018 have become absolute climatic records not only in Oltenia but even in the whole country and an extended area on the European continent. In Oltenia, April was excessively droughty, but heavy rainfall in March provided the groundwater reserve throughout the month, although some cereal crops have been affected. April was warm in all Oltenia with a general average deviation of 2.5°C, and the rainfalls returned, but the drought continued in the Romanați Plain. Climatic variability was particularly high, the climate evolving from an extreme to the other, but nevertheless the statistical analysis of the climatic data shows that the climate warming continued. The paper is part of an extensive series of studies on climate variability in Oltenia and climatic risk phenomena (Bogdan, Marinica, Andreea Floriana Marinică 2010, 2017; Marinică, Andreea Floriana Marinică 2016) being useful to all interested in climate problems in the south-west Romania.","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":"21 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"133070966","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}
Shape of demographic risk factors in Ciuc Depression. The complexity of a system as the population of a given area, involves shaping the evolution process, identify the many interdependent factors which give consistency to the system as a whole. In case of a major geodemographic variables that influence its evolution given the multifactorial model extrapolation of risks and disasters components include physical, economic, financial and socio-cultural, ie spatial dimension. Risk is the amplification of demographic aging in the third period of transition, is exceeding the point where population decline is stabilizing, according to the theory of the second demographic transition (Crenshaw, Oakey and Cristenson 1999) which is common in European countries. This phenomenon coincides with the degradation of the economic profile and in rural areas of agricultural, leading to unemployment which Amplifier migration, subsistence agriculture and poverty. Key-words: risks and vulnerabilities, demographic indicators and human geography, horizon of expectation, official data base and inadvertence af
慢性抑郁症人口危险因素的形态。系统的复杂性作为一个给定区域的人口，涉及塑造进化过程，确定许多相互依赖的因素，这些因素使系统作为一个整体保持一致性。考虑到多因素模型，影响其演变的主要地理人口变量包括物质、经济、金融和社会文化，即空间方面的风险和灾害组成部分的外推。根据欧洲国家常见的第二次人口转型理论(Crenshaw, Oakey and Cristenson 1999)，风险是人口老龄化在第三次转型时期的放大，超过了人口下降趋于稳定的点。这一现象与经济状况的恶化和农村地区农业的恶化相吻合，导致失业，从而扩大了移徙、自给农业和贫困。关键词:风险与脆弱性;人口指标与人文地理;预期视界
{"title":"Shape of demographic risk factors in Ciuc Depression","authors":"B. Holircă","doi":"10.24193/rcj2018_23","DOIUrl":"https://doi.org/10.24193/rcj2018_23","url":null,"abstract":"Shape of demographic risk factors in Ciuc Depression. The complexity of a system as the population of a given area, involves shaping the evolution process, identify the many interdependent factors which give consistency to the system as a whole. In case of a major geodemographic variables that influence its evolution given the multifactorial model extrapolation of risks and disasters components include physical, economic, financial and socio-cultural, ie spatial dimension. Risk is the amplification of demographic aging in the third period of transition, is exceeding the point where population decline is stabilizing, according to the theory of the second demographic transition (Crenshaw, Oakey and Cristenson 1999) which is common in European countries. This phenomenon coincides with the degradation of the economic profile and in rural areas of agricultural, leading to unemployment which Amplifier migration, subsistence agriculture and poverty. Key-words: risks and vulnerabilities, demographic indicators and human geography, horizon of expectation, official data base and inadvertence af","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":"17 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"129371570","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}
The role of snow in the formation of water flow in Suceava hydrographic basin. The hydrographic basin of the Suceava River is situated in the North-East sector of the Northern Carpathian Group from the Romanian Carpathians, more precisely, and much of the Suceava Plateau, a subunit of the Moldavian Plateau. The floods produced on the rivers in this basin were directly influenced by fallen liquid precipitations. The study is based on the processing and interpretation of climatic data about the snow layer recorded throughout the period. Also, data on the floods in the Suceava River Basin were recorded at eight hydrometer stations, three of which are located on the main course and five are on the main tributaries. The analysed period for the snow layer and its influence on the water flow formation in the study basin during the period 1961-2015, focusing on the variation in snow thickness and length over the analysed period. Finally, the influence of the snow layer on the drainage of the water and the drainage of the Suceava river basin during the analysed period with effect on large waters, floods and small waters was presented.
{"title":"The role of snow in the formation of water flow in Suceava hydrographic basin","authors":"A. Porcuţan","doi":"10.24193/RCJ2018_21","DOIUrl":"https://doi.org/10.24193/RCJ2018_21","url":null,"abstract":"The role of snow in the formation of water flow in Suceava hydrographic basin. The hydrographic basin of the Suceava River is situated in the North-East sector of the Northern Carpathian Group from the Romanian Carpathians, more precisely, and much of the Suceava Plateau, a subunit of the Moldavian Plateau. The floods produced on the rivers in this basin were directly influenced by fallen liquid precipitations. The study is based on the processing and interpretation of climatic data about the snow layer recorded throughout the period. Also, data on the floods in the Suceava River Basin were recorded at eight hydrometer stations, three of which are located on the main course and five are on the main tributaries. The analysed period for the snow layer and its influence on the water flow formation in the study basin during the period 1961-2015, focusing on the variation in snow thickness and length over the analysed period. Finally, the influence of the snow layer on the drainage of the water and the drainage of the Suceava river basin during the analysed period with effect on large waters, floods and small waters was presented.","PeriodicalId":326907,"journal":{"name":"Risks and Catastrophes Journal","volume":"49 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2018-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"124269576","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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