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Showing 384 results for Type of Study: Research

Gholam Reza Maghami Moghim,
Volume 12, Issue 46 (9-2025)
Abstract

Objective: “The main and overall objective of this research was to identify natural hazards threatening Saluk National Park and Protected Area. In this regard, based on the assumptions of this research, in addition to the main objective, three sub-objectives were also determined for it. The sub-objectives include identifying hazards arising from climatic, geomorphological, and hydrological conditions.
Method: This research was conducted using field and library methods and descriptive analytical methods. The aim of the field studies was to identify the plant and animal species of this park and protected area, which was done using interviews with environmentalists, people living in villages adjacent to the park, and the results of censuses conducted by the Environment Organization. In library studies, concepts and definitions related to the environment and natural hazards were extracted from books available in libraries and documents of the Environment Organization. Statistics from meteorological stations in the region were used to study the climate of the region.
Results: Initial studies suggested that climatic, geomorphological, and hydrological hazards may be the most important natural hazards of the park. Based on the studies, climatic hazards including drought, frost, and frost have greater impacts in the study area. Geomorphological hazards of the park resulting from external dynamic processes including landslides, landslides, and erosion are ranked second, and hydrological hazards, especially river floods in the eastern part of the park in the Ruin River valley and the southern alluvial fans of the park, are ranked third.
Conclusions:
The most important conclusion of this research is that the natural hazards of this park naturally act as an ecological moderator. And these hazards can have detrimental effects on this park when they interact with negative human interventions, but if they are aligned with positive human actions, their effects will not have a significant destructive impact on this park.





 
Dr Saleh Arekhi, Mr Habib Allah Kour, Somia Emadaddian,
Volume 12, Issue 46 (9-2025)
Abstract

Reducing the emissions caused by deforestation and forest degradation REDD is a strategy to moderate climate change, which is used to reduce the intensity of deforestation and greenhouse gas emissions in developing countries. In the last few decades, drastic changes in land use have caused a significant decrease in Hyrkan forests located in Mazandaran province. For this purpose, the aim of this study is to investigate the changes in land use and its prediction for the year 2050 using the Markov chain and the REDD project to reduce carbon dioxide emissions for the cities of Nowshahr and Chalus. Using the images of TM and ETM+ sensors of Landsat satellite, a land use map has been prepared in three time periods related to the years 1989, 2000 and 2021. Maximum likelihood method was used to classify images from supervised classification. From the error matrix, the Kappa coefficient in this evaluation was equal to 0.83 for 1989, 0.81 for 2000, and 0.92 for 2021. The results show that the forest cover decreases in 2050. In contrast, the area of ​​range land, city, barren land, agriculture and wetland will increase. Based on the goals of the REDD project, the amount of carbon dioxide emissions was calculated until 2050. If the REDD project is not implemented, a large area of ​​forest cover will be destroyed and a lot of carbon dioxide is released. The amount of carbon dioxide in the project area in 2021 is 49,681 tons and will reach 806,732 tons by 2051, and with the implementation of the REDD project in the region, this amount of gas can be increased to the equivalent of 402,321 tons. 404411 tons of carbon dioxide was prevented from entering the upper atmosphere of the earth. Examining changes using satellite images can help managers and planners to make more informed decisions.
 
Dr Saeedmohammad Sabouri, Dr Sayed Amirhossien Garakani,
Volume 12, Issue 46 (9-2025)
Abstract

Objective: Investigating the occurrence of land subsidence in the country and the extent to which rural settlements are exposed to the phenomenon of land subsidence.
Methods: The present study was based on library surveys and studies, field observations and impressions. Using information received from the National Mapping Organization, a map of the country's subsidence zones and the degree of risk of each zone, including very low, low, medium, high and very high risk, was drawn, and the aforementioned maps were compared with the location of the villages.
Results: According to the analysis of the available data, 302 villages are at very high risk, 768 villages are at high risk, 834 villages are in the medium risk zone, and 573 villages are in the low risk zone. In terms of percentage weight, about 4 percent of the country's villages are at medium to very high risk of subsidence, of which 1,904 villages are at medium to very high risk, and 573 villages are at low risk.
Conclusions: The highest provincial distribution of villages at risk of subsidence in the country with a very high degree is in the provinces of Alborz, Tehran, Khorasan Razavi, Qazvin, Kerman, Golestan and Hamedan, and the highest provincial distribution with a high degree is in the provinces of West Azerbaijan, Isfahan, Alborz, Tehran, Khorasan Razavi, Semnan, Qazvin, Kerman, Golestan, East Azerbaijan, Hamedan and Yazd. Also, the highest provincial distribution of villages at risk of medium-level subsidence is in the provinces of East and West Azerbaijan, Isfahan, Alborz, Tehran, Semnan, Qazvin, Kerman, Golestan, Mazandaran, Markazi, Hormozgan, Hamedan, and Yazd.

Dr. Sousan Heidari, Dr. Mostafa Karimi, Dr. Ghasem Azizi, Dr. Aliakbar Shamsipour,
Volume 12, Issue 46 (9-2025)
Abstract

Drought is one of the most significant natural hazards, characterized by complex spatiotemporal patterns. This study analyzes the structural and spatial characteristics of droughts in Iran across three temporal scales: annual, seasonal, and monthly. To achieve this, the intensity and extent of droughts were calculated using the RAI index and ERA5 monthly precipitation data over 42 years (1979–2021). Initially, the spatial distribution and directional trends of the drought centroid were examined, and its spatial variations over the years were analyzed. Additionally, the relationship between the location of the drought centroid and its extent was investigated. The results revealed that during the cold season, the drought centroid is primarily concentrated in central Iran, while in the warm season, it shifts toward the northwest, the Caspian Sea coast, and the southeastern regions of the country. The distribution pattern of droughts at all scales predominantly follows a northwest-to-southeast trajectory. Furthermore, shifts in the drought centroid toward the northeast, east, southeast, and south were observed to coincide with an increase in drought extent, whereas shifts toward the north, northwest, and west were associated with a reduction in drought extent. Overall, the findings of this study demonstrate a direct relationship between the location of the drought centroid and changes in drought extent, despite the fact that droughts in Iran lack consistent and predictable spatiotemporal patterns
 

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