A Multiscale Simulation Study of the Effects of Nantucket Island on Atmospheric Boundary Layer Flow.
Saved in:
| Title: | A Multiscale Simulation Study of the Effects of Nantucket Island on Atmospheric Boundary Layer Flow. |
|---|---|
| Authors: | Allouche, Mohammad1 (AUTHOR) allouche1@llnl.gov, Mirocha, Jeffrey D.1 (AUTHOR) |
| Source: | Journal of Applied Meteorology & Climatology. Jun2026, Vol. 65 Issue 6, p1-19. 19p. |
| Subjects: | Atmospheric boundary layer, Large eddy simulation models, Multiscale modeling, Atmospheric physics, Islands, Wind power, Atmospheric circulation, Ocean temperature |
| Geographic Terms: | Nantucket Island (Mass.) |
| Abstract: | Multiscale atmospheric simulations were conducted to investigate how Nantucket Island modifies the marine atmospheric boundary layer flow (ABL), how the mechanisms responsible are represented in mesoscale versus large-eddy simulation (LES) domains, and potential impacts on wind energy production downstream, in moderate and high wind speed cases. To isolate the effects of the island, each case study was simulated i) with and without island topography included, and ii) with observed versus spatially uniform sea surface temperature (SST) values, the latter removing the influence of spatial variability in SST, while also enabling examination of how the island effects vary with near-surface thermodynamic stability over the surrounding ocean. Island effects were found to be strongest during daytime heating, which generates convective rolls that redistribute momentum vertically over the island and downstream. Colder SSTs and weaker winds strengthen these rolls and extend their influence. Flow statistics within a representative wind turbine rotor-swept area downstream show that while vertical momentum redistribution enhances near-surface wind speeds, those aloft decrease, resulting in minimal net change to rotor-equivalent wind speed, and slightly reduced vertical shear. Comparisons of mesoscale and LES domains reveal that both capture the roughness-driven near-surface slowdown, but mesoscale models under-estimate vertical momentum transport compared to LES, which explicitly resolve convective rolls. Increasing LES resolution beyond the grid spacing required to begin capturing the largest convective-roll structures ∼ O (100m) yields minimal additional momentum transport but increases resolved turbulence kinetic energy, relevant for stress loading. [ABSTRACT FROM AUTHOR] |
| Copyright of Journal of Applied Meteorology & Climatology is the property of American Meteorological Society and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.) | |
| Database: | Engineering Source |
|
Full text is not displayed to guests.
Login for full access.
|
|
| FullText | Links: – Type: pdflink Text: Availability: 1 |
|---|---|
| Header | DbId: egs DbLabel: Engineering Source An: 194578049 AccessLevel: 6 PubType: Academic Journal PubTypeId: academicJournal PreciseRelevancyScore: 0 |
| IllustrationInfo | |
| Items | – Name: Title Label: Title Group: Ti Data: A Multiscale Simulation Study of the Effects of Nantucket Island on Atmospheric Boundary Layer Flow. – Name: Author Label: Authors Group: Au Data: <searchLink fieldCode="AR" term="%22Allouche%2C+Mohammad%22">Allouche, Mohammad</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> allouche1@llnl.gov</i><br /><searchLink fieldCode="AR" term="%22Mirocha%2C+Jeffrey+D%2E%22">Mirocha, Jeffrey D.</searchLink><relatesTo>1</relatesTo> (AUTHOR) – Name: TitleSource Label: Source Group: Src Data: <searchLink fieldCode="JN" term="%22Journal+of+Applied+Meteorology+%26+Climatology%22">Journal of Applied Meteorology & Climatology</searchLink>. Jun2026, Vol. 65 Issue 6, p1-19. 19p. – Name: Subject Label: Subjects Group: Su Data: <searchLink fieldCode="DE" term="%22Atmospheric+boundary+layer%22">Atmospheric boundary layer</searchLink><br /><searchLink fieldCode="DE" term="%22Large+eddy+simulation+models%22">Large eddy simulation models</searchLink><br /><searchLink fieldCode="DE" term="%22Multiscale+modeling%22">Multiscale modeling</searchLink><br /><searchLink fieldCode="DE" term="%22Atmospheric+physics%22">Atmospheric physics</searchLink><br /><searchLink fieldCode="DE" term="%22Islands%22">Islands</searchLink><br /><searchLink fieldCode="DE" term="%22Wind+power%22">Wind power</searchLink><br /><searchLink fieldCode="DE" term="%22Atmospheric+circulation%22">Atmospheric circulation</searchLink><br /><searchLink fieldCode="DE" term="%22Ocean+temperature%22">Ocean temperature</searchLink> – Name: SubjectGeographic Label: Geographic Terms Group: Su Data: <searchLink fieldCode="DE" term="%22Nantucket+Island+%28Mass%2E%29%22">Nantucket Island (Mass.)</searchLink> – Name: Abstract Label: Abstract Group: Ab Data: Multiscale atmospheric simulations were conducted to investigate how Nantucket Island modifies the marine atmospheric boundary layer flow (ABL), how the mechanisms responsible are represented in mesoscale versus large-eddy simulation (LES) domains, and potential impacts on wind energy production downstream, in moderate and high wind speed cases. To isolate the effects of the island, each case study was simulated i) with and without island topography included, and ii) with observed versus spatially uniform sea surface temperature (SST) values, the latter removing the influence of spatial variability in SST, while also enabling examination of how the island effects vary with near-surface thermodynamic stability over the surrounding ocean. Island effects were found to be strongest during daytime heating, which generates convective rolls that redistribute momentum vertically over the island and downstream. Colder SSTs and weaker winds strengthen these rolls and extend their influence. Flow statistics within a representative wind turbine rotor-swept area downstream show that while vertical momentum redistribution enhances near-surface wind speeds, those aloft decrease, resulting in minimal net change to rotor-equivalent wind speed, and slightly reduced vertical shear. Comparisons of mesoscale and LES domains reveal that both capture the roughness-driven near-surface slowdown, but mesoscale models under-estimate vertical momentum transport compared to LES, which explicitly resolve convective rolls. Increasing LES resolution beyond the grid spacing required to begin capturing the largest convective-roll structures ∼ O (100m) yields minimal additional momentum transport but increases resolved turbulence kinetic energy, relevant for stress loading. [ABSTRACT FROM AUTHOR] – Name: AbstractSuppliedCopyright Label: Group: Ab Data: <i>Copyright of Journal of Applied Meteorology & Climatology is the property of American Meteorological Society and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.) |
| PLink | https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&db=egs&AN=194578049 |
| RecordInfo | BibRecord: BibEntity: Identifiers: – Type: doi Value: 10.1175/JAMC-D-25-0182.1 Languages: – Code: eng Text: English PhysicalDescription: Pagination: PageCount: 19 StartPage: 1 Subjects: – SubjectFull: Atmospheric boundary layer Type: general – SubjectFull: Large eddy simulation models Type: general – SubjectFull: Multiscale modeling Type: general – SubjectFull: Atmospheric physics Type: general – SubjectFull: Islands Type: general – SubjectFull: Wind power Type: general – SubjectFull: Atmospheric circulation Type: general – SubjectFull: Ocean temperature Type: general – SubjectFull: Nantucket Island (Mass.) Type: general Titles: – TitleFull: A Multiscale Simulation Study of the Effects of Nantucket Island on Atmospheric Boundary Layer Flow. Type: main BibRelationships: HasContributorRelationships: – PersonEntity: Name: NameFull: Allouche, Mohammad – PersonEntity: Name: NameFull: Mirocha, Jeffrey D. IsPartOfRelationships: – BibEntity: Dates: – D: 01 M: 06 Text: Jun2026 Type: published Y: 2026 Identifiers: – Type: issn-print Value: 15588424 Numbering: – Type: volume Value: 65 – Type: issue Value: 6 Titles: – TitleFull: Journal of Applied Meteorology & Climatology Type: main |
| ResultId | 1 |