逐时地表气温插值——一种时空统计模型在复杂地形中的应用

IF 2.8 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES
Louis Frey, Christoph Frei
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引用次数: 0

摘要

目前,在地气候观测的网格数据集大多以日分辨率构建。为了表示日变化,需要扩展到亚日分辨率,特别是地表空气温度。在这里,我们设计并研究了一种在复杂地形(瑞士)地区产生小时温度网格的方法。动态线性模型(DLM)将空间气候学中广泛使用的模型(kriging with external drift, KED)扩展为时空统计模型,同时保留了适应区域特点的灵活性。我们为已知的中尺度效应(逆温、冷空气池、山谷和湖泊效应)配置了协变量,假设相关系数的准谐波演变。该方法应用于一次冬季逆温事件和一次夏季高压事件,数据来自259个台站。我们将DLM与顺序应用的KED进行比较,并在交叉验证中评估预测。结果表明,DLM可以准确再现复杂的时空变化,包括逐渐形成的逆温和昼夜之间不同的温度模式。平均绝对误差在平原和丘陵地形(两期)的0.65°C到冬季山谷地区的1.6°C之间。DLM在时间上比KED产生更多的连续效应系数,这证实了时空建模的预期优势。然而,除了人为减少台站数据的实验外,DLM的预测误差并没有明显减小。在我们的应用程序的数据丰富的条件下,时空方法似乎比空间模型没有什么优势。然而,在观测值较少或协变量较多的情况下,其优势可能更为突出。DLM是一种开发亚日气候数据集的通用方法,本研究为将其应用于特定地区的气候条件提供了有价值的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Interpolation of Hourly Surface Air Temperature—Application of a Spatio-Temporal Statistical Model in Complex Terrain

Interpolation of Hourly Surface Air Temperature—Application of a Spatio-Temporal Statistical Model in Complex Terrain

At present, grid datasets of in situ climate observations are mostly constructed in daily time resolution. An extension to sub-daily resolution is desirable, particularly for surface air temperature, in order to represent diurnal variations. Here, we devise and investigate a method to produce hourly temperature grids in a region of complex topography (Switzerland). The method, a dynamic linear model (DLM), extends a model widely used in spatial climatology (kriging with external drift, KED), into a spatio-temporal statistical model, while preserving its flexibility to adapt to the specifics of a region. We configure the method with covariates for known mesoscale effects (inversions, cold-air pooling, valley- and lake effects), assuming quasi-harmonic evolutions in the related coefficients. The method is applied to a wintertime inversion episode and a summertime high-pressure episode, with data from 259 stations. We compare DLM to a sequentially applied KED and evaluate the predictions in cross-validation. The results demonstrate that DLM can accurately reproduce complex spatio-temporal variations, including the gradual build-up of an inversion and the distinct temperature patterns between day- and night-time. The mean absolute error ranges from 0.65°C in flat and hilly terrain (both episodes) to 1.6°C in mountain valleys in winter. DLM yields temporally more continuous effect coefficients than KED, which corroborates the expected advantage from spatio-temporal modelling. However, the prediction errors of DLM are not significantly smaller, except in experiments where the station data was artificially reduced. It seems that the spatio-temporal approach had little advantage over a spatial model in the data-rich conditions of our application. However, its advantage may be more prominent in conditions with fewer observations or with more covariates. DLM is a versatile method for developing sub-daily climate datasets and this study provides valuable insight on its adoption to the climatic conditions of a specific region.

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来源期刊
International Journal of Climatology
International Journal of Climatology 地学-气象与大气科学
CiteScore
7.50
自引率
7.70%
发文量
417
审稿时长
4 months
期刊介绍: The International Journal of Climatology aims to span the well established but rapidly growing field of climatology, through the publication of research papers, short communications, major reviews of progress and reviews of new books and reports in the area of climate science. The Journal’s main role is to stimulate and report research in climatology, from the expansive fields of the atmospheric, biophysical, engineering and social sciences. Coverage includes: Climate system science; Local to global scale climate observations and modelling; Seasonal to interannual climate prediction; Climatic variability and climate change; Synoptic, dynamic and urban climatology, hydroclimatology, human bioclimatology, ecoclimatology, dendroclimatology, palaeoclimatology, marine climatology and atmosphere-ocean interactions; Application of climatological knowledge to environmental assessment and management and economic production; Climate and society interactions
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