Urban storage heat flux variability explored using satellite, meteorological and geodata

Springer Science and Business Media LLC - Tập 141 Số 1-2 - Trang 271-284 - 2020
Fredrik Lindberg1, K. Frans G. Olofson1, Ting Sun2, C. S. B. Grimmond2, Christian Feigenwinter3
1Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden
2Department of Meteorology, University of Reading, Reading, UK
3Institute of Meteorology, Climatology and Remote Sensing, University of Basel, Basel, Switzerland

Tóm tắt

Abstract

The storage heat flux (ΔQS) is the net flow of heat stored within a volume that may include the air, trees, buildings and ground. Given the difficulty of measurement of this important and large flux in urban areas, we explore the use of Earth Observation (EO) data. EO surface temperatures are used with ground-based meteorological forcing, urban morphology, land cover and land use information to estimate spatial variations of ΔQSin urban areas using the Element Surface Temperature Method (ESTM). First, we evaluate ESTM for four “simpler” surfaces. These have good agreement with observed values. ESTM coupled to SUEWS (an urban land surface model) is applied to three European cities (Basel, Heraklion, London), allowing EO data to enhance the exploration of the spatial variability in ΔQS. The impervious surfaces (paved and buildings) contribute most to ΔQS. Building wall area seems to explain variation of ΔQSmost consistently. As the paved fraction increases up to 0.4, there is a clear increase in ΔQS. With a larger paved fraction, the fraction of buildings and wall area is lower which reduces the high values of ΔQS.

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Springer Science and Business Media LLC

Tập 141 Số 1-2

271-284

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