Abstract
Climate change and urbanization expose a growing number of people to
health risks due to increased ambient temperature (Ta). Chronic and
acute Ta exposure are associated with increased mortality and morbidity,
especially among vulnerable populations such as the elderly and infants.
Understanding and monitoring these risks requires spatially- and
temporally-resolved Ta at high resolutions. This is challenging both in
rural areas, which have large spatial extents and often few weather
stations, and urban areas, where the complex built environment can
produce temperature variation at scales of a few hundred meters. We
present a model of daily minimum, maximum, and mean Ta from 2000 through
2016 at a base resolution of 1 km2 across continental France and at an
increased resolution of 200 x 200 m2 over large urban areas. We start by
extending a technique that was previously used to predict 1 km daily
mean Ta in France (Kloog et al., 2017): we use linear mixed models to
calibrate Ta observations from weather stations with remotely sensed
daily 1 km land surface temperature (LST) from the MODIS instrument on
the Terra and Aqua satellites. We also include MODIS monthly composite 1
km NDVI, elevation, population density, and land cover. We use these
mixed models to predict daily 1 km Ta, then fill gaps where LST is
missing (e.g. due to cloud cover) with a second set of linear mixed
models that calibrate our 1 km Ta predictions at each location with Ta
observations from nearby stations. This base resolution model performs
very well, with ten-fold cross-validated R2 of 0.921 (Tmin), 0.968
(Tmean), and 0.954 (Tmax), MAE of 1.4 ˚ C (Tmin), 0.9 ˚ C
(Tmean), and 1.4 ˚ C (Tmax), and RMSE of 1.9 ˚ C (Tmin), 1.3
˚ C (Tmean), and 1.8 ˚ C (Tmax) for the initial calibration
stage. To increase the spatial resolution over urban areas, we train
random forest and gradient boosting regression models to predict the
daily residuals of the 1 km Ta models on a 200 x 200 m2 grid. These
models are based on latitude, longitude, day of year, 1 km predicted Ta,
elevation, population density, land cover, and top-of-atmosphere
brightness temperature and NDVI from the Landsat 5, 7, and 8 satellites
composited by month across all years in the study period. Finally, we
use a generalized additive model to ensemble the random forest and
gradient boosting models with spatially varying weights. We add the
resulting daily 200 m predicted residuals to the daily 1 km predicted Ta
to obtain daily 200 m predicted Ta. This model also performs well, with
the ensemble stage achieving ten-fold cross-validated R2 of 0.792
(Residmin), 0.892 (Residmean), and 0.845 (Residmax), MAE of 0.4
(Residmin), 0.3 (Residmean), and 0.3 (Residmax), and RMSE of 0.6
(Residmin), 0.4 (Residmean), and 0.5 (Residmax). Kloog, I., Nordio,
F., Lepeule, J., Padoan, A., Lee, M., Auffray, A., Schwartz, J., 2017.
Modelling spatio-temporally resolved air temperature across the complex
geo-climate area of France using satellite-derived land surface
temperature data. Int. J. Climatol. 37, 296-304.
https://doi.org/10.1002/joc.4705
Original language | English GB |
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Title of host publication | 21st EGU General Assembly, EGU2019, Proceedings from the conference held 7-12 April, 2019 in Vienna, Austria |
Pages | 10399 |
Volume | 21 |
State | Published - 1 Apr 2019 |