Climate Change and Adoption Strategies – A Report from the Republic of Serbia

Author(s):  
Vesela Radovic
Keyword(s):  
2021 ◽  
pp. 14-20
Author(s):  
M. I. LOSKIN ◽  

The current state of agricultural land reclamation in the Republic of Sakha (Yakutia), its role in agricultural production of the republic, taking into account the impact of climate change on irrigation facilities, is considered. It has been established that at present in the sphere of public administration in the field of land reclamation in the republic there are estuary irrigation systems, drainage systems and agricultural water supply facilities, as well as group water pipelines for water supply of rural settlements and irrigation of agricultural land.


2020 ◽  
Vol 11 (S1) ◽  
pp. 289-309 ◽  
Author(s):  
Hrachuhi Galstyan ◽  
Shamshad Khan ◽  
Hovik Sayadyan ◽  
Artur Sargsyan ◽  
Tatevik Safaryan

Abstract The primary goal of the study is to analyze the spatial-temporal trends and distribution of flood events in the context of climate change in Armenia. For that purpose, some meteorological parameters, physical-geographical factors and the flood events data were studied for the 1994–2019 period. The linear trends demonstrate an increasing tendency of air temperature and precipitation. Those trends expressed increased flood occurrences, especially for the 2000s, whereas the Mann–Kendall (MK) trend test reveals no significant change. The number of flood events reaches its maximum in 2011 with its peak in May. Out of 191 flood events, half of the occurrences are recorded in the flat areas and southern aspects of the mountains (22% of the country's territory). There is a certain clustering of flood events in the areas with up to 5° slopes (66% of flood events). The most flood vulnerable areas were analyzed and mapped via Geographical Information System (GIS). The GIS-based mapping shows the location of flood vulnerable areas in the central, northern parts of the country, and the coastal areas of Lake Sevan. Our methodological approach elaborates the localization of flood-prone sites. It can be used for the flood hazard assessment mapping and risk management.


Author(s):  
Peter Rudiak-Gould

The Republic of the Marshall Islands, an archipelago of low-lying coral atolls in eastern Micronesia, is one of four sovereign nations that may be rendered uninhabitable by climate change in the present century. It is not merely sea level rise which is expected to undermine life in these islands, but the synergy of multiple climatic threats (Barnett and Adger 2003). Rising oceans and increasingly frequent typhoons will exacerbate flooding at the same time that the islands’ natural protection—coral reefs—will die from warming waters and ocean acidification. Fresh water resources will be threatened by both droughts and salt contamination from flooding. Although the reaction of the coral atoll environment to climate change is uncertain, it is likely that the islands will no longer be able to support human habitation within fifty or a hundred years (Barnett and Adger 2003: 326)—quite possibly within the lifetimes of many Marshall Islanders living today. In the public imagination, climate change in vulnerable, remote locations is the intrusion of contamination into a formerly pristine environment, of danger into a once secure sanctuary, of change into a once static microcosm (see Lynas 2004: 81, 124). Archaeologists, of course, know better than this: every place has a history of environmental upheavals, and the Marshall Islands is no exception. Researchers agree that coral atolls are among the most precarious and marginal environments that humans have managed to inhabit (Weisler 1999; Yamaguchi et al. 2005: 27), existing only ‘on the margins of sustainability’ (Weisler 2001). The islands in fact only recently formed: while the reefs are tens of millions of years old, the islets that sit on them emerged from the sea only recently, probably around 2000 BP (Weisler et al. 2000: 194; Yamaguchi et al. 2005: 31–2), just before the first people arrived (Yamaguchi et al. 2005: 31–2). The new home that these early seafarers found was not so much an ancient safe haven as a fragile geological experiment—land whose very existence was tenuous long before humans were altering the global climate.


2020 ◽  
Vol 2020 ◽  
pp. 1-16 ◽  
Author(s):  
Mohammadreza Mohammadi ◽  
John Finnan ◽  
Chris Baker ◽  
Mark Sterling

This paper examines the impact that climate change may have on the lodging of oats in the Republic of Ireland and the UK. Through the consideration of a novel lodging model representing the motion of an oat plant due to the interaction of wind and rain and integrating future predictions of wind and rainfall due to climate change, appropriate conclusions have been made. In order to provide meteorological data for the lodging model, wind and rainfall inputs are analysed using 30 years’ time series corresponding to peak lodging months (June and July) from 38 meteorological stations in the United Kingdom and the Irish Republic, which enables the relevant probability density functions (PDFs) to be established. Moreover, climate data for the next six decades in the British Isles produced by UK climate change projections (UKCP18) are analysed, and future wind and rainfall PDFs are obtained. It is observed that the predicted changes likely to occur during the key growing period (June to July) in the next 30 years are in keeping with variations, which can occur due to different husbandry treatments/plant varieties. In addition, the utility of a double exponential function for representing the rainfall probability has been observed with appropriate values for the constants given.


2014 ◽  
Vol 8 (2) ◽  
pp. 163-169
Author(s):  
Maria Nedealcov ◽  
Dumitru Drumea

Abstract The accelerating pace of climate change mainly on the adjacent territory of the Danube basin, contribute to the essential eutrophication of water basins within the region. The results indicate that air temperature recorded a double warming compared to territories from the central part of the country. On the background the accelerated warming there is a declining trend and of annual rainfall amounts. These climate changes, especially in recent decades have led to significant increase of water temperature in rivers and lakes. Thus, it constituted in the years 1990-2000 by 0.7 and 1.50C compared to the period 1980-1990, and by 1.0...2,00C accordingly in the years 2000-2013 compared to the previous decade. The significant increase of temperature during the last decade contributed to the intensification of algae growth and together with other factors contributed to the increase by about 20% of the nitrogen content, thus ensuring the ―flowering‖ with 50% of the water bodies’ volume.


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