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EFFECTS OF TEMPERATURE AND PRECIPITATION ANOMALIES ON CARBON DIOXIDE FLUXES IN THE EXTRATROPICAL FORESTS OF THE NORTHERN HEMISPHERE 温度和降水异常对北半球热带外层森林二氧化碳通量的影响
Pub Date : 2024-06-04 DOI: 10.55959/msu0579-9414.5.79.2.2
E. Satosina, D. Gushchina, M. Tarasova, I. Zheleznova, E. Emelianova, R. Gibadullin, A. Osipov, A. V. Olchev
Modern climate change, accompanied by rapidly increasing global air temperature, changing precipitation patterns, frequency and severity of extreme weather events, may have a significant impact on the functioning, growth, and development of forest ecosystems. The aim of the study was to assess the effects of extreme weather events (significant positive and negative anomalies in air temperature and precipitation) on the carbon dioxide (CO2) fluxes in boreal and temperate forest ecosystems in the Northern Hemisphere. 26 greenhouse gas (GHG) flux monitoring stations of the global FLUXNET network with the most continuous observations were selected for the analysis of CO2 fluxes. The stations are located in forest ecosystems of different biome types according to the IGBP classification. Meteorological conditions were analyzed using observations from meteorological stations and ERA5 reanalysis data. The results showed that the response of CO2 fluxes to temperature and precipitation anomalies varies depending mainly on the type of forest ecosystem, its geographical location and regional climatic conditions. Extremely high air temperature in any season leads to increased CO2 emissions to the atmosphere in all forest types studied, with the most pronounced response in coniferous forests. Negative air temperature anomalies in the warm season could have the opposite effect, either increasing or decreasing the CO2 uptake by forest ecosystems, depending on the forest ecosystem type. No significant response of CO2 fluxes to extremely low temperatures in the cold season was found. During periods of heavy precipitation, the emission of CO2 to the atmosphere dominated in all forest ecosystems under study. At the same time, after a large amount of precipitation during the warm season, a cumulative effect of available soil moisture in the plant root zone on CO2 fluxes was revealed. As a result the CO2 uptake by vegetation increases due to the growing rate of plant photosynthesis under sufficient soil moisture conditions.
现代气候变化伴随着全球气温的快速上升、降水模式的改变、极端天气事件的频率和严重程度,可能会对森林生态系统的功能、生长和发展产生重大影响。研究的目的是评估极端天气事件(气温和降水的显著正负异常)对北半球北方和温带森林生态系统二氧化碳(CO2)通量的影响。在全球 FLUXNET 网络中选择了 26 个具有最连续观测数据的温室气体通量监测站进行二氧化碳通量分析。根据 IGBP 的分类,这些监测站位于不同生物群落类型的森林生态系统中。利用气象站的观测数据和ERA5再分析数据分析了气象条件。结果表明,二氧化碳通量对温度和降水异常的响应主要取决于森林生态系统的类型、地理位置和区域气候条件。在研究的所有森林类型中,任何季节极高的气温都会导致向大气排放的二氧化碳增加,针叶林的反应最为明显。暖季的负气温异常则会产生相反的效果,增加或减少森林生态系统对二氧化碳的吸收,这取决于森林生态系统的类型。在寒冷季节,二氧化碳通量对极端低温没有明显反应。在强降水期间,研究中的所有森林生态系统都会向大气排放二氧化碳。同时,在暖季大量降水之后,植物根区可用土壤水分对二氧化碳通量的累积效应也显现出来。因此,在充足的土壤水分条件下,植物光合作用的速度不断加快,植被对二氧化碳的吸收量也随之增加。
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引用次数: 0
New rural residents and forms of their territorial organization in the Voskresensky district of the Nizhny Novgorod region 下诺夫哥罗德州沃斯克列先斯基市的新农村居民及其地域组织形式
Pub Date : 2024-06-04 DOI: 10.55959/msu0579-9414.5.79.2.6
O. D. Krutov, N. K. Grelya, A.A. Veprickij, Ya.K. Kuksin, G.A. Nazarenko, O.E. Prusihin, P.A. Shirokova, Yu.L. Kruze, A. Alekseev
The article examines the influence of “new rural residents” – immigrants from Nizhny Novgorod and Moscow, on a semi-peripheral district of the Non-Chernozem Region, as well as the transformation of its economy and society in connection with population replacement. Issues related to the territorial heterogeneity of the “new rural” influence are also considered. The research site, i.e. the Voskresensky district of the Nizhny Novgorod region is located 145 kilometers north of the city of Nizhny Novgorod. The presence of unique natural and symbolic resources, such as the Svetloyar Lake and the Vetluga River, attracts migrants from the large cities here. Research methods included in-depth and expert interviews, focus groups, participant observation and strategic sessions with local residents. The analysis of obtained data resulted in a typology of “new rural” residents, each type producing a different impact on the surrounding space. Key transformations of the lifestyle associated with the “new rural” are identified, namely new non-traditional types of agriculture, formation of “urban type” leisure, development of rural tourism by new-comers, complete replacement of the population in the most attractive settlements for city residents, as well as the emergence of associations of new-comers both territorial, and communities of “interests”. Key social conflicts were also identified among the new-comers and between them and indigenous residents, which limit the possibilities for development of the territory.
文章探讨了 "新农村居民"--来自下诺夫哥罗德和莫斯科的移民--对非切尔诺泽姆州半边缘地区的影响,以及该地区在人口更替过程中的经济和社会变革。还考虑了与 "新农村 "影响的地域异质性有关的问题。研究地点,即下诺夫哥罗德州沃斯克列先斯基区位于下诺夫哥罗德市以北 145 公里处。斯韦特罗亚尔湖和韦特卢加河等独特的自然和象征性资源吸引着来自大城市的移民。研究方法包括深入访谈和专家访谈、焦点小组、参与观察以及与当地居民的战略会议。通过对获得的数据进行分析,得出了 "新农村 "居民的类型,每种类型都对周围空间产生了不同的影响。确定了与 "新农村 "相关的生活方式的主要转变,即新的非传统农业类型、"城市型 "休闲的形成、新移民对乡村旅游的开发、在对城市居民最具吸引力的居住区人口的完全替代,以及新移民的地域协会和 "利益 "社区的出现。此外,还发现了新移民之间以及他们与当地居民之间的主要社会冲突,这些冲突限制了该地区发展的可能性。
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引用次数: 0
Sea level modeling in the Kazakhstan part of the Caspian Sea using the MIKE 21 model 利用 MIKE 21 模型建立里海哈萨克斯坦部分的海平面模型
Pub Date : 2024-06-04 DOI: 10.55959/msu0579-9414.5.79.2.7
A. Yeltay, N. Ivkina
The article presents the results of adaptation of the MIKE 21 Flow Model FM hydrodynamic module of the MIKE Zero software package to the Caspian Sea region using reanalysis data of wind and pressure fields, both for individual years and for a long-term period (2000–2020). The quality of modeling results was assessed using the statistical methods. The correlation coefficient between observed and simulated water levels for the period of 2000–2020 was 0,97 for Fort Shevchenko and 0,95 for Aktau. Model calibration allowed obtaining optimal values of model parameters, such as the Smagorinsky turbulent viscosity coefficient of 0,5 and the Manning roughness coefficient of 0,031. The evaluation for the multi-year period and the individual cases demonstrated that the modeling quality criteria were within acceptable limits. The results of the model verification based on the data for 2000–2020 and its testing for the storm surge on March 5–7, 2022, indicated that in the future the MIKE Zero software package could be used for operational sea level forecasting.
文章介绍了利用个别年份和长期(2000-2020 年)的风场和气压场再分析数据对 MIKE Zero 软件包的 MIKE 21 流动模型 FM 流体动力模块进行里海地区调整的结果。使用统计方法评估了建模结果的质量。2000-2020 年期间,谢甫琴科堡的观测水位与模拟水位之间的相关系数为 0.97,阿克套的相关系数为 0.95。通过模型校准,可以获得最佳的模型参数值,例如斯马戈林斯基湍流粘度系数为 0.5,曼宁粗糙度系数为 0.031。多年期和单个案例的评估结果表明,模型质量标准在可接受范围内。基于 2000-2020 年数据的模型验证结果以及对 2022 年 3 月 5-7 日风暴潮的测试结果表明,MIKE Zero 软件包今后可用于海平面业务预报。
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引用次数: 0
CHANGES OF ENVIRONMENTAL CHARACTERISTICS OF THE ASIAN “ECONOMIC GIANTS” IN THE CONTEXT OF THE GEOECOLOGICAL TRANSITION 地质生态转型背景下亚洲 "经济巨人 "环境特征的变化
Pub Date : 2024-06-04 DOI: 10.55959/msu0579-9414.5.79.2.3
N. N. Alekseeva, D. Lopatnikov, A. I. Bancheva
Since the end of the last century the epicenter of environmental problems and global environmental threats has moved to Asia. Three economic giants played the main role: at first Japan, then China and India. In recent decades increasingly complicated and multidirectional environmentally significant processes have taken place in these Asian countries, which are at different stages of socio-economic development. The purpose of the study was to identify the main trends in the basic environmental characteristics of Japan, China and India and study the dynamics of their position in the context of the geoecological transition. The work was based on the concepts of the environmental Kuznets curve (EKC) and the geoecological transition of D.L. Lopatnikov. Comparison of environmental and economic parameters was carried out on the basis of statistical data from the World Bank, OECD and national databases. Time series for sulfur dioxide, nitrogen oxides, particulate matter and carbon dioxide emissions were analyzed mainly for the period 1990-2020. The dynamics of the countries’ position on the curve over a 30-year period makes it possible to identify the trajectories of their environmental development, as well as determine prospects for the short-term future. According to the dynamics of key indicators, Japan is steadily on a downward segment of the curve, while China and India are on a downward segment for some indicators, having passed an inflection point during the period under study, and on an upward segment for other ones. The interpretation of dynamics of the environmental indicators revealed the main factors (economic, institutional, technological, etc.) which lay behind their environmental advancement. At the same time, the economic slowdown during the 2008-2009 global economic crisis and the COVID-19 pandemic had a different impact on the key indicators of the three countries. The position of countries in the international environmental ratings correlates with the level of socio-economic development, which fits into the logic of the EKC. While the first signs of a turn towards the greener economy are already visible in China, the same is still not true for India. The environmentally positive trends which were identified for the economic giants of Asia, with the exception of Japan, cannot yet be considered a long-term trend due to the relatively short series of data and the continuing diversity of their environmental prospects.
自上世纪末以来,环境问题和全球环境威胁的中心已转移到亚洲。三个经济大国发挥了主要作用:首先是日本,然后是中国和印度。近几十年来,处于不同社会经济发展阶段的这些亚洲国家出现了日益复杂和多向的重大环境进程。研究的目的是确定日本、中国和印度基本环境特征的主要趋势,并研究它们在地质生态转型背景下的动态地位。这项工作以环境库兹涅茨曲线(EKC)和 D.L. 洛帕特尼科夫的地质生态转型概念为基础。根据世界银行、经合组织和国家数据库的统计数据,对环境参数和经济参数进行了比较。主要分析了 1990-2020 年期间二氧化硫、氮氧化物、颗粒物和二氧化碳排放量的时间序列。通过各国在 30 年间曲线上的动态位置,可以确定其环境发展的轨迹,并确定短期未来的前景。根据主要指标的动态变化,日本正稳步处于曲线的下行段,而中国和印度的某些指标处于下行段,在研究期间已经过了一个拐点,其他指标则处于上行段。对环境指标动态的解读揭示了其环境进步背后的主要因素(经济、制度、技术等)。同时,2008-2009 年全球经济危机期间的经济放缓和 COVID-19 大流行对这三个国家的主要指标产生了不同的影响。各国在国际环境评级中的地位与社会经济发展水平相关,这符合 EKC 的逻辑。虽然中国已经出现了转向绿色经济的初步迹象,但印度的情况仍不尽人意。除日本外,亚洲其他经济大国在环境方面的积极趋势尚不能被视为一种长期趋势,原因是数据序列相对较短,而且其环境前景持续多样化。
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引用次数: 0
GEOGRAPHICAL FACTORS OF REVITALIZATION OF RURAL SETTLEMENTS “WITHOUT POPULATION 振兴 "无人口 "农村住区的地理因素
Pub Date : 2024-03-02 DOI: 10.55959/msu0579-9414.5.78.1.11
A. Smirnova
The article proposes a method for identifying “reviving” rural settlements (RS). Case studies of the Tver region RS revealed what features of the geographical location determine a settlement opportunities for revitalization. The previous typology, based on the analysis of satellite images, showed a considerable differentiation in the degree of RS degradation, classified according to the 2010 census as “without population”. Further work to determine the leading factors of revitalization was based on the study of those RS where the houses and outbuildings, identified by satellite images, have been preserved to the greatest extent. Nearness to rivers and water bodies, position relative to federal and regional highways, and location near the regional and/or district center were chosen as key features of the geographical location that have an effect on the prospects for revitalization of a territory. The presence of registered residents (according to current records) and demarcated cadastral plots are indicators of the RS revitalization. The study showed that one third of all RS, which fell into the category “without population” according to 2010 statistics, could now be considered “reviving”. A key factor in the revitalization of rural settlements of the Tver region is their nearness to the river, mainly to the Volga River. Another important factor is the location in the zone of influence of main centers, primarily the city of Tver. The main function is the recreational (dacha) use of such villages.
文章提出了一种确定 "振兴 "农村定居点(RS)的方法。对特维尔地区乡村居民点的案例研究揭示了地理位置的哪些特征决定了居民点的振兴机会。之前基于卫星图像分析的类型学显示,根据 2010 年人口普查被归类为 "无人口 "的乡村居民点在退化程度上存在很大差异。为进一步确定振兴的主要因素,我们对卫星图像所确定的房屋和附属建筑得到最大程度保留的塞族共和国进行了研究。临近河流和水体、与联邦和地区高速公路的相对位置以及靠近地区和/或区中心的位置被选为对地区振兴前景有影响的主要地理位置特征。登记居民的存在(根据现有记录)和划定的地籍地块是振兴塞尔维亚共和国的指标。研究表明,根据 2010 年的统计数据,三分之一的塞族共和国属于 "无人口 "类别,但现在可以被视为 "正在振兴"。特维尔地区农村居民点振兴的一个关键因素是靠近河流,主要是伏尔加河。另一个重要因素是位于主要中心(主要是特维尔市)的影响区内。这些村庄的主要功能是娱乐(别墅)用途。
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引用次数: 0
SEAFLOOR MORPHOLOGY OF THE OB RIVER GULF, KARA SEA 喀拉海奥布江海湾的海底形态
Pub Date : 2024-03-02 DOI: 10.55959/msu0579-9414.5.79.1.7
A. Ermolov, G. Kazhukalo, A. I. Noskov, S. Ogorodov
The article presents the results of an extensive study of the bottom topography of the Ob River Gulf in the Kara Sea, which is a follow-up to the long-term studies of the authors. It refines the existing ideas and aims at solving a fundamental problem of reconstructing the conditions for the formation of bottom topography in the shallow bays of the Kara Sea in the Late Pleistocene and Holocene. The work aims to create a regional characteristic of the geomorphologic structure of the Ob River Gulf bottom. The initial data on the bottom topography were taken from marine navigational maps and sounding boards at a scale of 1:50 000 - 1:100 000. We processed and interpreted the collected cartographic material to create a detailed DEM of the bottom and a bathymetric map at a scale of 1:200 000 with an isobaths interval of 1 m. In addition to bathymetric data, the compilation of a geomorphologic map engaged a large amount of literature and stock materials on geomorphology, geology, and geocryology of the region. The original morphogenetic legend was elaborated with due account of current ideas regarding the conditions for the formation of periglacial plains relief at the regressive stage of the Kara Sea shelf evolution. It was found that the relict fluvial relief prevails within the gulf and was partly modified by subaqueous processes during post-LGM transgression and the current epoch. We have indicated the most critical features of the structure and pattern of the flooded pravalley of the Ob River, as well as the total ancient erosion network. The selected individual forms and relief elements take into account the scale of objects and the degree of their generalization on the map and give an idea of the development of relief-forming processes both at the subaerial stage and under subaqueous conditions, including specific features of modern dynamics of the coastal and bottom relief.
文章介绍了对喀拉海鄂毕河湾海底地形进行广泛研究的结果,这是作者长期研究的后续工作。它完善了现有观点,旨在解决一个基本问题,即重建晚更新世和全新世喀拉海浅海湾海底地形形成的条件。这项工作旨在建立鄂毕河海湾底部地貌结构的区域特征。有关海底地形的初始数据来自比例尺为 1:50 000 - 1:100 000 的海洋导航图和探测板。我们对收集到的制图资料进行了处理和解释,绘制了详细的海底 DEM 图和比例尺为 1:200 000、等深线间距为 1 米的测深图。在绘制原始形态图例时,适当考虑了当前关于喀拉海大陆架演化倒退阶段围冰期平原地貌形成条件的观点。研究发现,海湾内普遍存在残留的冰川地貌,在后大地构造横断和本纪期间,部分地貌被水下过程所改变。我们指出了鄂毕河洪积草原结构和形态的最关键特征,以及整个古代侵蚀网络。所选的单个形态和地貌要素考虑到了对象的比例尺及其在地图上的概括程度,并提供了在亚陆相阶段和水下条件下地貌形成过程的发展概念,包括海岸和底部地貌的现代动态的具体特征。
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引用次数: 0
PALAEOECOLOGICAL SITUATION IN PRE-DELTA AREA OF THE NORTH CASPIAN SEA DURING THE HOLOCENE 全新世时期北里海前三角洲地区的古生态状况
Pub Date : 2024-03-02 DOI: 10.55959/msu0579-9414.5.79.1.5
E. Lysenko, A.A. Tkach, R. Makshaev, T. Yanina, M. Zenina
Palaeoecoligical reconstructions of predelta area of the North Caspian Sea were based on the multidisciplinary study of the core from the Rybachya borehole containing the Holocene deposits. Geochemical, grain size, mollusk fauna, diatom and ostracod analyses were performed, and the radiocarbon dating was carried out. The structure of deposits reflects palaeogeographic events of different scales including the inception of a palaeoincision in the Lower Khvalynian deposits, accompanied by erosion of the Upper Khvalynian deposits; its development during the Mangyshlak regression and gradual filling during the multistage Holocene Neocaspian transgression. The Holocene age of the deposits filling the palaeodepression is confirmed by radiocarbon dates - 8070 ± 110 and 7020 ± 140 cal. BP. The paleontological data indicate the interchange of tranquil and dynamic water regimes and the quasicyclical change in the conditions of the water basin, from brackish to freshwater and to marine during the stage of sedimentation, corresponding to the presentday conditions on the North Caspian shelf.
对含有全新世沉积物的 Rybachya 钻孔岩芯进行了多学科研究,在此基础上重建了北里海前三角洲地区的古生态环境。对岩心进行了地球化学、粒度、软体动物、硅藻和浮游动物分析,并进行了放射性碳测年。沉积物的结构反映了不同尺度的古地理事件,包括下赫瓦利年沉积物古冲积的开始,伴随着上赫瓦利年沉积物的侵蚀;其在曼吉斯拉克回归期间的发展,以及在多级全新世新里海横断期间的逐渐填充。填充古洼地的沉积物的全新世年龄得到了放射性碳年代的证实--8070 ± 110 和 7020 ± 140 cal.公元前。古生物学数据表明,在沉积阶段,宁静的水体和动态的水体相互交替,水流域的条件也发生了类周期变化,从咸水到淡水,再到海洋,这与北里海大陆架目前的条件相吻合。
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引用次数: 0
VARIATIONS OF δ18О AND δ2H VALUES OF PRECIPITATION IN MOSCOW FROM 2017 TO 2019 2017 至 2019 年莫斯科δ18О和δ2H 预采值的变化情况
Pub Date : 2024-03-02 DOI: 10.55959/msu0579-9414.5.79.1.9
Yu.K. Vasilchuk, N.A. Budantseva, J. Vasilchuk, A. Vasilchuk, I. Eremina, Y. Chizhova
To reveal variations in the iso topic composition of O and H in the atmospheric precipitation in Moscow and the processes influencing the isotope composition, all events of precipitation in 2017-2019 were sampled at the Meteorological Observatory of the Moscow State University: 158 samples in 2017, 119 samples in 2018 and 143 samples in 2019. The study is a prolongation of continuous measurements of the isotope composition of precipitation, started by authors in 2014. The study of the isotope composition of precipitation at the MSU Meteorological Observatory was supported by the IAEA and became a part of the Global Network of Isotopes in Precipitation (GNIP) database. It has been found that the intra-annual variability of the isotop e composition of precipitation has a pronounced seasonality. The most isotopically heavy precipitation falls from May to August, and the most isotop ically light precipitation at December-February, mainly due to seasonal air temperature variations. The ratio of the average monthly δ18O values in precipitation and air temperature for the study period varied from 0.34 to 0.39‰/°C, which is consistent with the previously obtained data for precipitation in Moscow. The δ2H-δ18O ratio in precipitation was clos e to that of the Global Meteoric Water Line, pointing to the equilibrium conditions during precipitation formation. It was established that in the summer months isotopic composition is significantly influenced by undercloud evaporation. The deuterium excess va lues in precipitation are not markedly seasonal; however, lower dexc values (below the 3-year average of 11‰) are typical for the summer months (July-August). It is most likely due to undercloud evaporation in conditions of low relative humidity and high air temperatures. Higher dexc values (above 11‰) prevailed from October to April.
为了揭示莫斯科大气降水中 O 和 H 的同位素组成变化以及影响同位素组成的过程,莫斯科国立大学气象观测台对 2017-2019 年的所有降水事件进行了采样:2017 年 158 个样本,2018 年 119 个样本,2019 年 143 个样本。这项研究是作者于 2014 年开始的降水同位素组成连续测量的延续。在 MSU 气象观测站进行的降水同位素组成研究得到了国际原子能机构的支持,并成为全球降水同位素网络(GNIP)数据库的一部分。研究发现,降水同位素组成的年内变化具有明显的季节性。5 月至 8 月的降水同位素含量最高,12 月至 2 月的降水同位素含量最低,这主要是由于季节性气温变化造成的。研究期间降水和气温的月平均δ18O 值之比在 0.34 至 0.39‰/℃之间变化,这与之前获得的莫斯科降水数据一致。降水中的δ2H-δ18O 比值与全球陨水线的比值接近,表明降水形成过程中的平衡条件。研究证实,在夏季,同位素组成受到云下蒸发的显著影响。降水中的氘过剩值没有明显的季节性;然而,较低的氘过剩值(低于三年平均值 11‰)是夏季(7-8 月)的典型特征。这很可能是由于在相对湿度低和气温高的条件下云下蒸发造成的。10 月至 4 月的脱氧核糖核酸(dexc)值较高(高于 11‰)。
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引用次数: 0
ECOLOGICAL CONDITION OF THE OGLAKHTY SITE OF THE KHAKASS NATURE RESERVE BASED ON THE RESULTS OF 2022 OBSERVATIONS 基于 2022 年观测结果的哈卡斯自然保护区奥格拉赫蒂遗址的生态状况
Pub Date : 2024-03-02 DOI: 10.55959/msu0579-9414.5.79.1.3
А.О. Afanaseva, S.А. Lebedeva
The article presents the results of the ecological module of complex recreational monitoring in specially protected natural territories of federal importance. The work was carried out according to the methodological recommendations elaborated in 2021 by a team of authors (V.V. Nepomnyaschy, A.V. Zavadskaya, V.P. Chizhova).Monitoring of the state of natural complexes under the influence of tourist and recreational activities was carried out in the zone of areal and linear impacts at the Oglakhty site of the Khakass reserve. The main results are presented for the 2022 tourist season. Currently, the entire territory of the Oglakhty site is mainly occupied by quasinatural complexes. The linear impact is concentrated mainly on patrol roads and manifests itself in the pedestrian movement zone. The areal impact is on the stopover places near information banners and display objects on the routes, as well as in places of the economic activities. Recommendations for the effective development of ecotourism on the Oglakhty site include the construction of additional flooring on the most popular route, as well as the redistribution of tourist flow to the less attended routes with sufficient capacity, increasing their attractiveness for various target audiences.
文章介绍了在具有联邦重要性的特别保护自然区内进行综合娱乐监测的生态模块结果。在哈卡斯保护区奥格拉赫季景点的区域和线性影响区对旅游和娱乐活动影响下的自然综合体状况进行了监测。主要结果针对 2022 年旅游季节。目前,奥格拉赫蒂保护区的整个区域主要是准自然综合体。线性影响主要集中在巡逻路上,表现在行人活动区。区域性影响则体现在路线上的信息标语和展示物附近的停留点以及经济活动场所。为有效发展奥格拉赫季生态旅游而提出的建议包括:在最受欢迎的路线上增设地 面,以及将游客流重新分配到客流量较少且容量充足的路线上,增加其对不同目标受众 的吸引力。
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引用次数: 0
ASSESSMENT OF PYROGENIC IMPACT ON FOREST AREAS IN THE TVER REGION 评估热原对特维尔地区林区的影响
Pub Date : 2024-03-02 DOI: 10.55959/msu0579-9414.5.79.1.10
S.N. Zharinov, E. Golubeva, M.V. Zimin
We consider the potential and limitations of widely accepted remote sensing algorithms for detecting forest areas damaged by fires, which allow the monitoring systems to automatically form data about the fire areas and the areas where death of tree stands is subsequently recorded. The resulting size of the detected areas has a measurement error, which is typically determined on the basis of a onetime survey for a large territory and one forest fire season. Depending on the geographical features of the territory, forest fires have specific spatiotemporal and qualitative characteristics, and are accompanied by specific heterogeneous damage to forests, which affect the accuracy of remote detection of a burnt area or firedamaged forest. Hence the use of the unified largearea error estimate for locallevel surveys could lead to inaccurate results. The analysis of space images of forest fund lands in the Tver region for the period 2007-2022 demonstrated the need to establish regional values of the measurement error for fireimpacted areas. By comparing the medium spatial resolution data with the data of high spatial resolution we identify a regional bias, which is significant given the relatively small size of the detected areas. The study demonstrates the expediency of establishing regional error values for measurements of pyrogenic impact on forest areas. By implementing the suggested changes we could improve the accuracy of remotely-sensed estimates of fireimpacted areas and the amount of associated damage to forests.
我们考虑了广泛接受的遥感算法的潜力和局限性,这些算法用于检测受火灾破坏的森林区域,使监测系统能够自动形成有关火灾区域和随后记录林木死亡区域的数据。探测到的区域面积有一定的测量误差,通常是根据对大片区域和一个森林火灾季节的一次性调查确定的。根据地域的地理特征,森林火灾具有特定的时空和质量特征,并伴随着对森林的特定的异质性破坏,这影响了对烧毁区域或被火烧过的森林进行远程检测的准确性。因此,在地方级调查中使用统一的大面积误差估计可能会导致不准确的结果。对特维尔地区 2007-2022 年期间森林基金土地空间图像的分析表明,有必要确定火灾影响区域的测量误差区域值。通过将中等空间分辨率数据与高空间分辨率数据进行比较,我们发现了区域偏差,鉴于检测到的区域面积相对较小,这种偏差非常明显。这项研究表明,在测量林区火成影响时,建立区域误差值是很有必要的。通过实施建议的修改,我们可以提高火灾影响区域遥感估算的准确性以及相关的森林损失量。
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Lomonosov Geography Journal
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