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Heat load assessment in Central European cities using an urban climate model and observational monitoring data

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985807%3A_____%2F19%3A00507089" target="_blank" >RIV/67985807:_____/19:00507089 - isvavai.cz</a>

  • Alternative codes found

    RIV/86652079:_____/19:00507085 RIV/00216224:14310/19:00107723 RIV/61989592:15310/19:73596778

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.enbuild.2019.07.023" target="_blank" >http://dx.doi.org/10.1016/j.enbuild.2019.07.023</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.enbuild.2019.07.023" target="_blank" >10.1016/j.enbuild.2019.07.023</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Heat load assessment in Central European cities using an urban climate model and observational monitoring data

  • Original language description

    Diurnal variability of spatial pattern of air temperature was studied in five cities in Central Europe: Bratislava (Slovakia), Brno (Czech Republic), Kraków (Poland), Szeged (Hungary) and Vienna (Austria), during one of the heat waves in 2015 (4–14 August), with the application of micro-climate model MUKLIMO_3. 8th August was chosen to study in detail the urban heat load at 10.00, 16.00, 22.00 and 4.00 CEST. Local Climate Zones concept was used to supply data for the model and for the interpretation of the results obtained. Model outcomes were validated with measurement data from 86 points belonging to the networks which operate in the cities studied. The results obtained show that among urban LCZ, the highest heat load was observed for LCZ 2 and 3 from 16.00 to 4.00, while at 10.00 there is no such clear pattern. Unlike forested areas, open green areas can contribute to the generation of high air temperature: >35°C during day time and >30°C during night time. Important factors controlling the intra-zonal and inter-zonal variability of air temperature in particular LCZs are the local environmental conditions. During the day time, diversified relief in the area of the city and its vicinities generates higher heat load in the valleys’ floors than in areas located above, both in rural and urban areas. The same landforms experience lower heat load during the night time due to air temperature inversions effect.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10509 - Meteorology and atmospheric sciences

Result continuities

  • Project

    <a href="/en/project/GA205%2F09%2F1297" target="_blank" >GA205/09/1297: Multilevel analysis of the urban and suburban climate taking medium-sized towns as an example</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2019

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Energy and Buildings

  • ISSN

    0378-7788

  • e-ISSN

  • Volume of the periodical

    201

  • Issue of the periodical within the volume

    October

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    17

  • Pages from-to

    53-69

  • UT code for WoS article

    000488143400005

  • EID of the result in the Scopus database

    2-s2.0-85069723855