Seasonal variations in the surface energy and CO2 flux over a high‐rise, high‐population, residential urban area in the East Asian monsoon region

Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea. The study area is affected by the Asian mo...

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Veröffentlicht in:International journal of climatology 2020-08, Vol.40 (10), p.4384-4407
Hauptverfasser: Hong, Je‐Woo, Lee, Sang‐Dae, Lee, Keunmin, Hong, Jinkyu
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creator Hong, Je‐Woo
Lee, Sang‐Dae
Lee, Keunmin
Hong, Jinkyu
description Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea. The study area is affected by the Asian monsoon, which is accompanied by long rain spells and a related mid‐season depression of solar radiation in the summer. Our analysis shows that the urban surface energy balance and turbulence characteristics demonstrate typical urban properties. Unstable conditions dominate all day, and the storage heat flux (night‐time and morning) and sensible heat flux (afternoon) significantly affect the diurnal variations in the urban surface energy balance. Owing to the rough urban surface, the turbulence intensities are higher than those reported previously in other cities. The annual CO2 emission rate is approximately 13.1 kg CO2 m−2⋅year−1 with traffic, which is the major source of CO2 (+2.3 μmol⋅m−2⋅s−1 per 100 vehicles). Ecosystem respiration, including that by vegetation, soil, and humans, becomes dominant in the night‐time (00:00–05:00), thus contributing significantly to the annual CO2 budget. Further analysis indicates a unique coupling of urban surface energy partitioning and CO2 emission rates with the seasonal progression of the Asian monsoon: (a) surface albedo has annual minima in late summer when the sun elevation angle, is relatively higher and the urban surface condition is wetter than in other seasons; (b) the Bowen ratio ranges from 1.7 (summer) to 7.0 (winter); and (c) CO2 emission rates show seasonal variations with the progress of the summer monsoon. Using the eddy covariance method, this study reports the one‐year turbulent fluxes of momentum, energy, and CO2, and their seasonal variations over a recently redeveloped high‐rise, high‐population, residential area in the metropolitan city of Seoul, Korea.
doi_str_mv 10.1002/joc.6463
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subjects Albedo
Albedo (solar)
Asian monsoon
Bowen ratio
Carbon dioxide
Carbon dioxide emissions
Carbon dioxide flux
CO2 emission
Covariance
Diurnal variations
East Asian monsoon
Eddy covariance
eddy covariance method
Elevation angle
Emission
Energy balance
Enthalpy
Fluctuations
Heat flux
Heat transfer
high‐rise residential area
Momentum
Monsoons
Night
Residential areas
Seasonal variation
Seasonal variations
Seasons
Sensible heat
Sensible heat flux
Sensible heat transfer
Seoul
Soil
Solar radiation
Storage
Summer
Summer monsoon
Surface energy
Surface energy balance
Surface properties
Turbulence
Turbulence intensities
Turbulent fluxes
Urban areas
urban climate
Wind
title Seasonal variations in the surface energy and CO2 flux over a high‐rise, high‐population, residential urban area in the East Asian monsoon region
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