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1. Identity statement
Reference TypeJournal Article
Sitemtc-m21d.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier8JMKD3MGP3W34T/4578HQB
Repositorysid.inpe.br/mtc-m21d/2021/08.02.13.09   (restricted access)
Last Update2021:08.02.13.09.58 (UTC) simone
Metadata Repositorysid.inpe.br/mtc-m21d/2021/08.02.13.09.58
Metadata Last Update2022:04.03.22.27.29 (UTC) administrator
DOI10.1007/s00703-021-00812-2
ISSN0177-7971
Citation KeySampaioRoVoSiArRo:2021:SeHeFl
TitleSensible heat flux assessment in a complex coastal-mountain urban area in the metropolitan area of Rio de Janeiro, Brazil
Year2021
Access Date2024, May 19
Type of Workjournal article
Secondary TypePRE PI
Number of Files1
Size3055 KiB
2. Context
Author1 Sampaio, Rafael João
2 Rodriguez, Daniel Andres
3 Von Randow, Celso
4 Silva, Fabrício Polifke da
5 Araújo, Afonso Augusto Magalhães de
6 Rotunno Filho, Otto Correa
ORCID1 0000-0003-3399-6214
Group1
2
3 DIIAV-CGCT-INPE-MCTI-GOV-BR
Affiliation1 Universidade Federal do Rio de Janeiro (UFRJ)
2 Universidade Federal do Rio de Janeiro (UFRJ)
3 Instituto Nacional de Pesquisas Espaciais (INPE)
4 Universidade Federal do Rio de Janeiro (UFRJ)
5 Universidade Federal do Rio de Janeiro (UFRJ)
6 Universidade Federal do Rio de Janeiro (UFRJ)
Author e-Mail Address1 samprafael@gmail.com
2
3 celso.vonrandow@inpe.br
JournalMeteorology and Atmospheric Physics
Volume133
Pages973-987
Secondary MarkB1_INTERDISCIPLINAR B1_GEOCIÊNCIAS B1_CIÊNCIAS_AMBIENTAIS B5_ASTRONOMIA_/_FÍSICA
History (UTC)2021-08-02 13:09:58 :: simone -> administrator ::
2021-08-02 13:09:58 :: administrator -> simone :: 2021
2021-08-02 13:10:55 :: simone -> administrator :: 2021
2022-04-03 22:27:29 :: administrator -> simone :: 2021
3. Content and structure
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Content TypeExternal Contribution
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AbstractObtaining accurate estimates of surface-atmosphere energy exchanges and improved comprehension of the mechanisms generating turbulent fluxes over non-uniform landscapes are both challenging goals and essential for validating numerical weather forecasting modeling. In this work, a large-aperture scintillometer (LAS) was deployed to evaluate the effect of mesoscale sea and valley breezes with respect to diurnal sensible heat flux (H) variability over an urban area close to a coastal bay near the metropolitan area of Rio de Janeiro (MARJ) during the austral summer of 2017-2018 time span. The region is characterized by a densely urbanized environment, surrounded by mountainous relief and bounded by a large ocean bay. The transmitter and the receiver of the LAS system were installed 1955 m apart. Diurnal cycle was divided into four periods according to the local time: dawn (00 a.m. to 6 a.m.), morning (6 a.m. to 12 a.m.), afternoon (12 a.m. to 6 p.m.), and night (6 p.m. to 00 a.m.). The results demonstrated the sensitivity of the LAS to record variations in H over the course of the day, taking into account the corresponding sea and valley breezes and the relative humidity variability. During the morning, when valley breezes are predominant, footprint area shrinks to its smallest size, encompassing an area of approximately 2 km(2). On the other side, during afternoon and night time periods, during afternoon and night time periods, the presence of sea breeze jointly with a densely urbanized continental area contribute to promote significant changes in the footprint area ranging from 2.05 to 5.38 km(2). The effects of topography are also well captured in the diurnal H cycle once sunset and corresponding shading in the late afternoon abruptly reduces heat-sensible flux. Diurnal variations in footprint shape and area lead to modifications in terms of the mode each type of urban surface will contribute to H, increasing the influence of anthropogenic elements in afternoon and early evening. Complementarily, it is noteworthy to mention that a sensitivity test was performed to assess uncertainties in H estimates for the free convection method, which requires the estimation of an empirical constant b. Variations in this constant introduce larger dispersion in H estimates than potential errors in LAS effective height (Z(eff)) estimations or temperature measurements. These last results highlight the importance of conducting further evaluations as the one pursued in this study to more rigorously validate the outputs of numerical mesoscale and local hydrometeorological models and remotely sensed products.
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Languageen
Target Filesampaio_sensible_2021.pdf
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Read Permissiondeny from all and allow from 150.163
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5. Allied materials
Next Higher Units8JMKD3MGPCW/46KUATE
DisseminationWEBSCI; PORTALCAPES; COMPENDEX.
Host Collectionurlib.net/www/2021/06.04.03.40
6. Notes
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