Observing and Simulating the Summertime Low-Level Jet in Central Iowa

dc.contributor.author Vanderwende, Brian
dc.contributor.author Lundquist, Julie
dc.contributor.author Rhodes, Michael
dc.contributor.author Takle, Eugene
dc.contributor.author Irvin, Samantha
dc.contributor.department Department of Aerospace Engineering
dc.contributor.department Ames National Laboratory
dc.contributor.department Department of Agronomy
dc.contributor.department Department of the Earth, Atmosphere, and Climate
dc.contributor.department Ames Laboratory
dc.date 2018-02-18T10:11:45.000
dc.date.accessioned 2020-06-29T23:02:45Z
dc.date.available 2020-06-29T23:02:45Z
dc.date.copyright Thu Jan 01 00:00:00 UTC 2015
dc.date.issued 2015-05-01
dc.description.abstract <p>In the U.S. state of Iowa, the increase in wind power production has motivated interest into the impacts of low-level jets on turbine performance. In this study, two commercial lidar systems were used to sample wind profiles in August 2013. Jets were systematically detected and assigned an intensity rating from 0 (weak) to 3 (strong). Many similarities were found between observed jets and the well-studied Great Plains low-level jet in summer, including average jet heights between 300 and 500 m above ground level, a preference for southerly wind directions, and a nighttime bias for stronger jets. Strong vertical wind shear and veer were observed, as well as veering over time associated with the LLJs. Speed, shear, and veer increases extended into the turbine-rotor layer during intense jets. Ramp events, in which winds rapidly increase or decrease in the rotor layer, were also commonly observed during jet formation periods. The lidar data were also used to evaluate various configurations of the Weather Research and Forecasting Model. Jet occurrence exhibited a stronger dependence on the choice of initial and boundary condition data, while reproduction of the strongest jets was influenced more strongly by the choice of planetary boundary layer scheme. A decomposition of mean model winds suggested that the main forcing mechanism for observed jets was the inertial oscillation. These results have implications for wind energy forecasting and site assessment in the Midwest.</p>
dc.description.comments <p>This article is from <em>Monthly Weather Review </em>143 (2015): 2319, doi:<a href="http://dx.doi.org/10.1175/MWR-D-14-00325.1" target="_blank">10.1175/MWR-D-14-00325.1</a>. Posted with permission.</p>
dc.format.mimetype application/pdf
dc.identifier archive/lib.dr.iastate.edu/agron_pubs/128/
dc.identifier.articleid 1124
dc.identifier.contextkey 10139116
dc.identifier.s3bucket isulib-bepress-aws-west
dc.identifier.submissionpath agron_pubs/128
dc.identifier.uri https://dr.lib.iastate.edu/handle/20.500.12876/4453
dc.language.iso en
dc.source.bitstream archive/lib.dr.iastate.edu/agron_pubs/128/2015_Takle_ObservingSimulating.pdf|||Fri Jan 14 19:30:18 UTC 2022
dc.source.uri 10.1175/MWR-D-14-00325.1
dc.subject.disciplines Atmospheric Sciences
dc.subject.disciplines Meteorology
dc.subject.keywords Stability
dc.subject.keywords Wind shear
dc.subject.keywords Boundary layer
dc.subject.keywords Jets
dc.subject.keywords Model evaluation/performance
dc.subject.keywords Renewable energy
dc.title Observing and Simulating the Summertime Low-Level Jet in Central Iowa
dc.type article
dc.type.genre article
dspace.entity.type Publication
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