Use of multi-annual MODIS Land Surface Temperature data for the characterization of the heat requirements for grapevine varieties

R. Zorer, D. Rocchini, L. Delucchi, F. Zottele, F. Meggio, M. Neteler
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引用次数: 12

Abstract

Heat requirements for grapevine varieties have been widely used to characterize potential growing regions for viticulture. One of the most important indices is the Winkler Index (WI) defined as the total summation of daily average air temperature above 10 °C from 1st of April to 31th of October in the Northern hemisphere [1]. Mapping of the WI is commonly based on temperature data from meteorological stations. However, in complex terrain such as the European Alps, these are usually irregularly and sparsely distributed or unavailable. This renders traditional geospatial interpolation approaches difficult to become reliable. As an alternative, thermal remote sensing data, which are intrinsically spatialised, can be used. The aim of this work was to provide time series of Winkler Index maps from 2003 to 2010, by means of the MODIS Land Surface Temperature (LST) data and to validate the maps using ground truth data, collected by two weather station networks.
利用多年MODIS地表温度数据表征葡萄品种的热需求
葡萄品种的热需求已被广泛用于表征葡萄栽培的潜在种植区。其中最重要的一个指标是Winkler指数(WI),它是北半球4月1日至10月31日10℃以上的日平均气温的总和[1]。WI的制图通常是根据气象站的温度数据。然而,在复杂的地形,如欧洲阿尔卑斯山,这些通常是不规则和稀疏分布或不可用的。这使得传统的地理空间插值方法难以变得可靠。作为一种替代方案,可以使用本质上是空间化的热遥感数据。这项工作的目的是通过MODIS地表温度(LST)数据提供2003年至2010年温克勒指数地图的时间序列,并使用两个气象站网络收集的地面真实数据验证地图。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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