Resources Environment and Information Engineering <p><a title="Registered Journal" href="" target="_blank" rel="noopener"><img class="journalreviewercredits" src="/journal/public/site/images/jasongong/Logo_ReviewerCredits-journal.jpg" alt="ReviewerCredits" align="right"></a><strong>Resources Environment and Information Engineering (REIE)</strong> (ISSN: 2661-3131) is an open access, continuously published, international, refereed&nbsp; journal which mainly studies the interdisciplinary and comprehensive fields of geospatial information science, resource science and environmental science. REIE publishes high quality special report, investigations, techniques and methods, original research work etc.</p> <p><strong>REIE</strong> will accept high-profile submissions including but not limited to: <br>• Environmental engineering<br>• Environmental Science <br>• Environmental monitoring and evaluation <br>• Improvement of ecological environment and pollution control <br>• Water pollution control theory and technology <br>• Air pollution control and catalytic technology <br>• Environmental planning and management <br>• Surveying and Mapping Engineering <br>• Geographic information system <br>• Remote sensing science and technology</p> en-US <p>Authors contributing to&nbsp;<em>Resources Environment and Information Engineering</em>&nbsp;agree to publish their articles under the&nbsp;<a href="">Creative Commons Attribution-Noncommercial 4.0 International License</a>, allowing third parties to share their work (copy, distribute, transmit) and to adapt it, under the condition that the authors are given credit, that the work is not used for commercial purposes, and that in the event of reuse or distribution, the terms of this license are made clear.</p> (Snowy Wang) (Alan Tan) Mon, 06 Mar 2023 08:45:15 +0800 OJS 60 Ecological resources of boreal forests in the adsorption of greenhouse gases and in adaptation to global warming <p>One of the most important ways to achieve the goals stipulated by the Paris (2015) Agreement on Climate Change is to solve a two-fold task: 1) the absorption of CO<sub>2</sub> by the forest communities from the atmosphere during global warming and 2) their adaptation to these climate changes, which should ensure the effectiveness of adsorption itself. Given report presents the regional experience of the numerical solution of this task. Calculations of the carbon balance of forest formations in the Oka-Volga River basin were carried out for global forecasts of moderate and extreme warming. The proposed index of labile elastic-plastic stability of forest ecosystems, which characterizes their isomorphic-restorative potential, was used as an indicator of adaptation. &nbsp; For the territory of the Oka river basin&nbsp; using multiple regression methods, a numerical experiment was conducted to assess the effect of the elastic stability of forest formations and the predicted climatic conditions on the carbon balance. A total of 11 linear equations were obtained (with a significance level of P &lt;10<sup>-6</sup>). In the upcoming 100-year forecast period, the overall elastic-plastic stability of forest formations should increase, and to the greatest extent with extreme warming. Accordingly, one should expect a significant increase in the ability of boreal forests to absorb greenhouse gases. A comparison of the carbon balance values ​​of forest formations obtained with initial (base) and final (final) stability indices gives an unambiguous picture of a significant increase in the adsorption capacity of boreal forests with an increase in their regenerative potential. A decisive contribution to increasing the adsorption of greenhouse gases is made by the growth of reforestation adaptation, which plays the role of a direct environmental factor.</p> Erland G. Kolomyts ##submission.copyrightStatement## Wed, 28 Jun 2023 16:08:20 +0800 Pacific ocean mega ecotone of Northern Eruasia as the belt of the origin of the modern continental biosphere <p>The Pacific Ocean margin of Eurasia includes the age row (at the geologic time scale) of geoecotone objects which can be imagined by certain nodal stages of the evolutionary trajectory of exogenous landscape genesis in the continental biosphere. The reported strategy of scientific research is aimed at the establishment of zonal-regional and local regularities of landscape organization of insular and marginal-continental land in different morphotectonic and macroclimatic sectors of the Pacific Ocean mega-ecotone of Northern Eurasia, which is considered as a natural laboratory for studying the modern stage of development of the geographical envelope&nbsp;&nbsp;&nbsp;&nbsp; The empirical statistical models of the island-arc stage of continental biosphere development in the North-West Pacific have been created by the example of experimental test ground of the active Mendeleev volcano on the Kunashir Island (the South Kuril Ridge). It was shown that on this initial stage local geomorphological and hydro-edaphic conditions created the centers of origin of diverse phytocoenological structures. An exceptionally high percentage of green mass in the structure of production results in the acceleration of the biological cycle as a factor of stability of forest community under unfavorable conditions of “cold” oceanicity. Geothermal energy induces rearrangement of the plant cover towards the increase in its flora- and phytocoenotic diversity to the detriment of biomass formation rate. The “climatically unjustified” but sufficiently stable sub-boreal forest ecosystems were formed, as well as the early stages of buffer forest communities.&nbsp;&nbsp;&nbsp;&nbsp; The multidimensional empirical-statistical modeling of landscape connections in the marginal-continental sector of the Pacific Ocean mega ecotone has been performed based on an experimental site in the Lower By-Amur Region. The ecology of the boreal-forest landscape of the continental margin characterizes the mature stage of evolution of the continental biosphere. The regularities and causal mechanisms of the formation of buffer forest communities typical of ecotone systems have been represented more integrally. Forests of this phenomenal buffer flora are distinguished by extremely high parameters of structural and functional development and have reached the state approaching the evolutionary climax. The previously advanced concepts of the Pacific ecotone of Northern Eurasia as a focus of evolutionary processes in the continental biosphere have been confirmed.</p> Erland G. Kolomyts ##submission.copyrightStatement## Mon, 06 Mar 2023 00:00:00 +0800