The James Hutton Institute, Craigiebuckler, AB158QH Aberdeen, Scotland, UK.
The James Hutton Institute, Craigiebuckler, AB158QH Aberdeen, Scotland, UK; School of Biosciences and Veterinary Medicine, Plant Diversity and Ecosystems Management Unit, University of Camerino, 62032 Camerino, MC, Italy.
Sci Total Environ. 2018 Jun 1;625:1628-1643. doi: 10.1016/j.scitotenv.2017.12.258. Epub 2018 Jan 16.
Climatic change in the last few decades has had a widespread impact on both natural and human systems, observable on all continents. Ecological and environmental models using climatic data often rely on gridded data, such as WorldClim. The main aim of this study was to devise and evaluate a computationally efficient approach to produce new high resolution (100m) estimates of current and future climatic variables to be used at the national and regional scale. The test area was Great Britain, where local data are available and of good quality. Present and future climate surfaces were produced. For the present, the approach involved the integration, via spatial interpolation, of local climate information and WorldClim to reduce bias. For future climate scenarios the approach involved spatially downscaling of WorldClim (1km) to a finer resolution of 100m. The main advantages of the proposed approach are: 1. finer resolution, 2. locally adapted to the study area with use of higher number of meteorological stations and improved accuracy and bias, and 3. computationally efficient while making use of the existing resources provided by WorldClim. Two applications were presented to illustrate the practical consequences of improvements obtained with this method. The first is a measure of rainfall intensity, i.e. the R-factor, widely applied in erosion and catchment-scale studies. The second is an application to species distribution modelling, involving a range of bioclimatic variables. The results highlighted the importance of considering the spatial variability and structure of the data integrated in the modelling, and using data adapted to the geographical extent of the analysis, whenever possible. The results of the applications showed the advantage of using enhanced climatic data in applications such as the estimation of soil erosion, species range shift, carbon stocks and the provision of ecosystem services.
在过去几十年中,气候变化对自然和人类系统产生了广泛的影响,在各大洲都有明显的体现。使用气候数据的生态和环境模型通常依赖于网格化数据,例如 WorldClim。本研究的主要目的是设计和评估一种计算效率高的方法,以生成新的当前和未来气候变量的高分辨率(100m)估计值,用于国家和地区尺度。测试区域是英国,那里有可用且质量较好的本地数据。生成了当前和未来的气候表面。对于当前情况,该方法涉及通过空间插值整合本地气候信息和 WorldClim,以减少偏差。对于未来气候情景,该方法涉及将 WorldClim(1km)空间下采样到更精细的 100m 分辨率。所提出方法的主要优点是:1. 更高的分辨率,2. 使用更多气象站并提高精度和偏差,对研究区域进行本地化调整,3. 在利用 WorldClim 提供的现有资源的同时计算效率高。提出了两个应用程序来说明该方法获得的改进的实际后果。第一个是降雨强度的度量,即 R 因子,广泛应用于侵蚀和集水区尺度的研究中。第二个是物种分布模型的应用,涉及一系列生物气候变量。结果强调了在建模中考虑数据的空间变异性和结构的重要性,并尽可能使用适用于分析地理范围的数据。应用程序的结果表明,在估计土壤侵蚀、物种范围转移、碳储量和提供生态系统服务等应用中使用增强的气候数据具有优势。