Department of Environmental Biology, Faculty of Sciences, University of Navarra, Pamplona, Navarra, Spain.
Laboratory of Green Energy and Environment, Nazarbayev University, Astana, Kazakhstan.
PLoS One. 2020 Oct 2;15(10):e0239514. doi: 10.1371/journal.pone.0239514. eCollection 2020.
We evaluate bioclimatic changes in Kazakhstan from the end of the 20th century until the middle of the 21st century to offer natural resource managers a tool that facilitates their decision-making on measures to adapt agriculture and environmental care to foreseeable climate change. We use climatic data from the "Providing REgional Climates for Impact Studies" (PRECIS) prediction and study them following the Worldwide Bioclimatic Classification System (WBCS) of Rivas-Martínez. For three 25-year intervals (1980-2004, 2010-2034 and 2035-2059), we identify the continentality, macrobioclimates, bioclimates, bioclimatic variants, thermotypes, ombrotypes and isobioclimates of the study area. The results of the work allow us to: locate the territories where bioclimatic conditions will change, quantify the magnitude of the predicted climate changes, and determine the trends of predictable climate change. We present the results in maps, tables and graphs. For the 80-year interval, we identify 3 macroclimates, 3 bioclimatic variants, 10 bioclimates, 11 thermotypes, 10 ombrotypes and 43 isobioclimates. Some of those found bioclimates, thermotypes, ombrotypes and isobioclimates are only located in the E, SE and S mountains, where they occupy very small areas, that decrease in a generalized way as the 20th century progresses. Comparing the three successive periods, the following trends are observed: 36.2% of the territory increases in thermicity; 7.3% of the territory increases in continentality; 9.7% of the territory increases in annual aridity; 9.5% of the territory increases in summer aridity or mediterraneity; and generalized losses occur in the areas of all mountain isobioclimates. The climate change foreseen by the PRECIS model for the middle of the 21st century leads to bioclimatic homogenization, with 20.8% losses in bioclimatic diversity. We indicate on maps the locations of all the predicted bioclimatic changes; these maps may provide decision makers with a scientific basis to take necessary adaptation measures.
我们评估了 20 世纪末至 21 世纪中叶哈萨克斯坦的生物气候变化,为自然资源管理者提供了一种工具,帮助他们就适应农业和环境护理的措施做出决策,以应对可预见的气候变化。我们使用来自“提供区域气候以进行影响研究”(PRECIS)预测的气候数据,并根据里瓦斯-马丁内斯的全球生物气候分类系统(WBCS)对其进行研究。对于三个 25 年的时间间隔(1980-2004 年、2010-2034 年和 2035-2059 年),我们确定了研究区域的大陆性、大生物气候、生物气候、生物气候变体、热型、雨型和等生物气候。该工作的结果使我们能够:确定生物气候条件将发生变化的区域,量化预测的气候变化幅度,并确定可预测的气候变化趋势。我们以地图、表格和图表的形式呈现结果。对于 80 年的时间间隔,我们确定了 3 种大生物气候、3 种生物气候变体、10 种生物气候、11 种热型、10 种雨型和 43 种等生物气候。其中一些发现的生物气候、热型、雨型和等生物气候仅位于 E、SE 和 S 山脉,它们仅占据很小的区域,随着 20 世纪的发展,这些区域呈普遍减少的趋势。在比较三个连续的时期时,观察到以下趋势:36.2%的领土变暖;7.3%的领土大陆性增加;9.7%的领土年干旱度增加;9.5%的领土夏季干旱度或地中海度增加;所有山地等生物气候区的面积普遍减少。PRECIS 模型预测的 21 世纪中叶的气候变化导致生物气候趋同,生物气候多样性损失 20.8%。我们在地图上标明了所有预测的生物气候变化的位置;这些地图可以为决策者提供科学依据,以便采取必要的适应措施。