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High resolution model simulation of
Department of Climatology and Landscape Ecology University of Szeged, Hungary High resolution model simulation of Urban Heat Island for a medium sized Hungarian city Case studies and verification András Zénó Gyöngyösi, Gergely Molnár, and Tamás Gál
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Motivation Small area (280 km2), 170k inhabitants,
Surface of (low or high intensity) urban landuse is even much less Frequent hot, summer nights (tropical nights/“beer-garden” days: 50/80d per annum, respectively). Heat waves are relatively common Only few grid cells are involved High model resolution is required
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Szeged
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Szeged
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Szeged
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UC monitoring sys Stations installed Represent LCZs
Installation: light poles Electricity + protection
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UC monitoring sys 22 (urban) + 2 (rural) stations
Minute average observations at 4 mAGL T, Rh From end of March, 2014 w/ gaps
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Typical diurnal variation
Representative stations BAR urban HMS rural Other stations Nocturnal UHI ΔT defined as: ΔT=TBAR – THMS Daily variations ΔTn: 06 – 12Z ΔTx: 00 – 06Z
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UC monitoring sys HMS BAR
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Seasonal variation Clear summer nights: ΔT=[-2,+6] (ΔT)x ≠Δ(Tx)
Modeling 26 days in 2015 summer – reproduction
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Test period in 2015 Selection criteria: ∆T Observed larger than 4.5°C
Clear conditions: Radiation larger than 750Wm-2 No precip
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Test period in 2015 Periods (26 days) Cases (7) 31st May – 7th June
1st – 7th July 5th – 14th August Cases (7) 3rd June 03rd, 6th and 7th July 6th, 7th and14th August
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Model domain ∆x = 10km
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Model domain
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Model domain ∆x = 2km
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Model domain
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Model domain ∆x = 0.4km
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Model domain 97 x 97
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Model domain
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Model domain
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Model domain HMS BAR
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Model setup More info: Poster H60 Molnar et al.
MP RA SFC LSM PBL CU e_vert WSM5 RRTMG revMM5 Noah BouLac KF 44 WSM6 MYJ nil 500hPa test0 test1 test2 test3 nil UCM BEP BEM Modified URB PARM table Modified geog database Landuse USGS → CORINE → LandSat Soiltype FAO → DKSIS More info: Poster H60 Molnar et al.
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Modified URB PARM data More info: Poster H60 Molnar et al.
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Geog database More info: Poster H60 Molnar et al. LU ST DKSIS geog0
USGS CORINE CORINE+LandSat modified geog2 ST FAO DKSIS More info: Poster H60 Molnar et al.
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Modeling strategy 48-hour runs on GFS .25 3-hourly input
24-hour overlap for spin-up Urban heat effects appear in the model results only on the second evening Output in urban (BAR) and rural (HMS) grid cells at every time steps (60, 12 and 2.4s resp). 1-minute average 2m Temperature Comparison to observations
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Results – Output from different model setups have been compared to observed urban effects Sensitivities for geographic database resolution parameterizations urban parameters have been tested.
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Results –
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Results – Temporal and spatial variation patterns have been captured properly Tx and ΔT values are acceptable However, both URB and RUR Tn values are too high compared to measurements Best performance: 3 domains, geog3 modified database, UCM urban physics and modified urban parameter table Even for 2 domains results were acceptable Further tests were performed on two domains with uniform setup
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More results... Temporal and spatial variation patterns have been captured properly Tx and ΔT values are acceptable However, both URB and RUR Tn values are too high compared to measurements
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Conclusions An appropriate modeling system for the representation of urban heat effects for a medium size city in Hungary have been established Appropriate static data and evaluation method have been constructed Model results have been verified on extensive and representative measurements Good agreement is found but further development is necessary Inclusion of anthropogenic heat Definition of more urban categories based on LCZs Testing further parameterization schemes (RAD?) and domain setups
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Thank you very much for your kind attention
Urban Climate Research Group at the University of Szeged, Hungary Thank you very much for your kind attention Hungarian Scientific Research Fund (OTKA K )
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