Abstract

Air temperature (Tair or T2m) is an important climatological variable for forest biosphere processes and climate change research. Due to the low density and the uneven distribution of weather stations, traditional ground-based observations cannot accurately capture the spatial distribution of Tair. In this study, Tair in Berlin is estimated during the day and night time over six land cover/land use (LC/LU) types by satellite remote sensing data over a large domain and a relatively long period (7 years). Aqua and Terra MODIS (Moderate Resolution Imaging Spectroradiometer) data and meteorological data for the period from 2007 to 2013 were collected to estimate Tair. Twelve environmental variables (land surface temperature (LST), normalized difference vegetation index (NDVI), Julian day, latitude, longitude, Emissivity31, Emissivity32, altitude, albedo, wind speed, wind direction and air pressure) were selected as predictors. Moreover, a comparison between LST from MODIS Terra and Aqua with daytime and night time air temperatures (Tday, Tnight) was done respectively and in addition, the spatial variability of LST and Tair relationship by applying a varying window size on the MODIS LST grid was examined. An analysis of the relationship between the observed Tair and the spatially averaged remotely sensed LST, indicated that 3 × 3 and 1 × 1 pixel size was the optimal window size for the statistical model estimating Tair from MODIS data during the day and night time, respectively. Three supervised learning methods (Adaptive Neuro Fuzzy Inference system (ANFIS), Artificial Neural Network (ANN) and Support vector machine (SVR)) were used to estimate Tair during the day and night time, and their performances were validated by cross-validation for each LC/LU. Moreover, tuning the hyper parameters of some models like SVR and ANN were investigated. For tuning the hyper parameters of SVR, Simulated Annealing (SA) was applied (SA-SVR model) and a multiple-layer feed-forward (MLF) neural networks with three layers and different nodes in hidden layers are used with Levenber-Marquardt back-propagation (LM-BP), in order to achieve higher accuracy in the estimation of Tair. Results indicated that the ANN model achieved better accuracy (RMSE= 2.16°C, MAE = 1.69°C, R2 = 0.95) than SA_SVR model (RMSE= 2.50°C, MAE = 1.92°C, R2 = 0.91) and ANFIS model (RMSE= 2.88°C, MAE= 2.2°C, R2 = 0.89) over six LC/LU during the day and night time. The Q-Q diagram of SA-SVR, ANFIS and NN show that all three models slightly tended to underestimate and overestimate the extreme and low temperatures for all LC/LU classes during the day and night time. The weak performance in the extreme and low temperatures are a consequence of the small number of data in these temperatures. These satisfactory results indicate that this approach is proper for estimating air temperature and spatial window size is an important factor that should be considered in the estimation of air temperature.

Highlights

  • The standard meteorological Tair is measured in a shelter at 2m height (Brunel, 1989; Jin and Dickinson, 2010)

  • The results showed that all models have similar capability in the training phase for estimating Tnight but the Artificial Neural Network (ANN) has a higher adjusted R2 which ranged from 0.89 to 0.93, RMSE and ranged from 2.13 °C to 2.35°C and MAE ranged from 1.54 °C to 1.84 °C values in the test phase in comparison to adaptive network-based fuzzy inference system (ANFIS) and Simulated Annealing (SA)-support vector machine (SVR)

  • The comparison shows that LSTday and LSTnight from both Terra and Aqua, with the mean relative bias above and under zero tended to overestimate Tday and underestimate Tnight respectively, and a higher relative RMSD and bias values were seen for the Aqua LSTdaytime than the Terra LSTdaytime which might be given the fact that more solar radiation has been received at the time of the aqua Moderate Resolution Imaging Spectroradiometer (MODIS) overpass later in the day

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Summary

Introduction

The standard meteorological Tair is measured in a shelter at 2m height (Brunel, 1989; Jin and Dickinson, 2010) It is an important indicator of terrestrial environmental conditions across the earth (Prihodko and Goward (1997); Peón et al, 2014) and one of the most widely used climatic variables in global change studies. It plays an important role in multiple biological and physical processes among the hydrosphere, atmosphere and biosphere (Stisen et al, 2007; Shamir et al, 2014; Benali et al, 2012). Detailed knowledge of the spatial variability of air temperature is of interest for many research and management

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