2016
DOI: 10.1002/2015jd024354
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Time series decomposition of remotely sensed land surface temperature and investigation of trends and seasonal variations in surface urban heat islands

Abstract: Previous time series methods have difficulties in simultaneous characterization of seasonal, gradual, and abrupt changes of remotely sensed land surface temperature (LST). This study proposed a model to decompose LST time series into trend, seasonal, and noise components. The trend component indicates long-term climate change and land development and is described as a piecewise linear function with iterative breakpoint detection. The seasonal component illustrates annual insolation variations and is modeled as… Show more

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Cited by 97 publications
(77 citation statements)
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“…The decreasing vegetation and increasing impervious surfaces can increase heat stored during daytime. Therefore, more heat will be released from impervious surfaces during nighttime, leading to the increasing nighttime SUHII [25,55]. One unique phenomenon was that the SUHII was significantly negatively correlated with ∆EVI at 4 of 10 cities in winter nights.…”
Section: The Relationships Between Suhii and ∆Evimentioning
confidence: 89%
“…The decreasing vegetation and increasing impervious surfaces can increase heat stored during daytime. Therefore, more heat will be released from impervious surfaces during nighttime, leading to the increasing nighttime SUHII [25,55]. One unique phenomenon was that the SUHII was significantly negatively correlated with ∆EVI at 4 of 10 cities in winter nights.…”
Section: The Relationships Between Suhii and ∆Evimentioning
confidence: 89%
“…The seasonal component is a regular and periodic change at an annual scale, primarily driven by the annual variation in insolation. The noise component is a stochastic and irregular variation that is caused by observation conditions (e.g., signal-to-noise ratio), atmospheric environments (e.g., clouds and aerosols) [41]. BFAST can be used to analyze different types of satellite image time series, and applied to other disciplines dealing with seasonal or non-seasonal time series, such as hydrology, climatology, and econometrics.…”
Section: Trend and Season Decomposition Modelmentioning
confidence: 99%
“…NDVI and NDWI represent greenness and wetness, respectively [74], both of which strongly influence evapotranspiration and surface cooling [75], and thus a decrease in NDVI/NDWI is usually followed by a Ta rise. Similarly, ISA contributes to enhancing sensible heat flux while reducing latent heat flux [40,69] and consequently heating up the atmosphere. BSA (or albedo) indicates a reflective proportion of incoming solar radiation, and therefore a low albedo increases solar heat absorption as well as heat release to the atmosphere [13,57].…”
Section: The Seven Predictors and Complementary Predictorsmentioning
confidence: 99%
“…The root mean square error (RMSE), mean absolute error (MAE), mean error (ME), and correlation coefficient (R 2 ) of the predicted Ta versus the measured Ta for each withheld weather station were calculated and then summarized across space (by land cover and site) and time (by year, season and month). To further evaluate the representation of temporal patterns by the predicted Ta, trend and seasonal decomposition [69] was performed on both the predicted and the measured Ta time series during the study period. The derived inter-and intra-annual variation parameters (mainly trend slope, seasonal amplitude and annual average temperature) were compared over each weather station.…”
Section: Model Evaluationmentioning
confidence: 99%
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