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A Methodology for Bridging the Gap between Regional- and City-Scale Climate Simulations for the Urban Thermal Environment

Climate, ISSN: 2225-1154, Vol: 10, Issue: 7
2022
  • 2
    Citations
  • 0
    Usage
  • 15
    Captures
  • 1
    Mentions
  • 0
    Social Media
Metric Options:   Counts1 Year3 Year

Metrics Details

  • Citations
    2
    • Citation Indexes
      2
  • Captures
    15
  • Mentions
    1
    • Blog Mentions
      1
      • 1

Most Recent Blog

Climate, Vol. 10, Pages 106: A Methodology for Bridging the Gap between Regional- and City-Scale Climate Simulations for the Urban Thermal Environment

Climate, Vol. 10, Pages 106: A Methodology for Bridging the Gap between Regional- and City-Scale Climate Simulations for the Urban Thermal Environment Climate doi: 10.3390/cli10070106

Article Description

The main objective of this study is to bridge the gap between regional- and city-scale climate simulations, with the focus given to the thermal environment. A dynamic-statistical downscaling methodology for defining daily maximum (T) and minimum (T) temperatures is developed based on artificial neural networks (ANNs) and multiple linear regression models (MLRs). The approach involves the use of simulations from two EURO-CORDEX regional climate models (RCMs) (at approximately 12 km × 12 km) that are further downscaled to a finer resolution (1 km × 1 km). A feature selection methodology is applied to select the optimum subset of parameters for training the machine learning models. The downscaling methodology is initially applied to two RCMs, driven by the ERA-Interim reanalysis (2008–2011) and high-resolution urban climate model simulations (UrbClims). The performance of the relationships is validated and found to successfully simulate the spatiotemporal distribution of T and T over Athens. Finally, the relationships that were extracted by the models are further used to quantify changes for T and T in high resolution, between the historical period (1971–2000) and mid-century (2041–2071) climate projections for two different representative concentration pathways (RCP4.5 and RCP8.5). Based on the results, both mean T and T are estimated to increase by 1.7 °C and 1.5 °C for RCP4.5 and 2.3 °C and 2.1 °C for RCP8.5, respectively, with distinct spatiotemporal patterns over the study area.

Bibliographic Details

Konstantina Koutroumanou-Kontosi; Constantinos Cartalis; Kostas Philippopoulos; Ilias Agathangelidis; Anastasios Polydoros

MDPI AG

Earth and Planetary Sciences

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