JULIE LUNDQUIST

Prof. JULIE LUNDQUIST

orcid

Research Focus & Metrics

Academic Career Length

27Years (2000-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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25 October 2019 in Science
Verified
Journal Article
Open access
PDF file
PVPaul Veers
Paul Veers
KDKatherine Dykes
Katherine Dykes
ELEric Lantz
Eric Lantz
SBStephan Barth
Stephan Barth
CBCarlo L. Bottasso
Carlo L. Bottasso
RWRyan Wiser
Ryan Wiser
A multifaceted future for wind power: Modern wind turbines already represent a tightly optimized confluence of materials science and aerodynamic engineering. Veers et al. review the challenges and opportunities for further expanding this technology, with an emphasis on the need for interdisciplinary collaboration. They highlight the need to better understand atmospheric physics in the regions where taller turbines will operate as well as the materials constraints associated with the scale-up. The mutual interaction of turbine sites with one another and with the evolving features of the overall electricity grid will furthermore necessitate a systems approach to future development. Science , this issue p. eaau2027

1 September 2012 in Monthly Weather Review
Verified
Journal Article
Open access
AFAnna C. Fitch
Anna C. Fitch
JOJoseph B. Olson
Joseph B. Olson
JLJULIE LUNDQUIST
JULIE LUNDQUIST
Jimy DudhiaJimy Dudhia
Jimy Dudhia
AGAlok K. Gupta
Alok K. Gupta
IBIdar Barstad
Idar Barstad
A new wind farm parameterization has been developed for the mesoscale numerical weather prediction model, the Weather Research and Forecasting model (WRF). The effects of wind turbines are represented by imposing a momentum sink on the mean flow; transferring kinetic energy into electricity and turbulent kinetic energy (TKE). The parameterization improves upon previous models, basing the atmospheric drag of turbines on the thrust coefficient of a modern commercial turbine. In addition, the source of TKE varies with wind speed, reflecting the amount of energy extracted from the atmosphere by the turbines that does not produce electrical energy. Analyses of idealized simulations of a large offshore wind farm are presented to highlight the perturbation induced by the wind farm and its interaction with the atmospheric boundary layer (BL). A wind speed deficit extended throughout the depth of the neutral boundary layer, above and downstream from the farm, with a long wake of 60-km e-folding distance. Within the farm the wind speed deficit reached a maximum reduction of 16%. A maximum increase of TKE, by nearly a factor of 7, was located within the farm. The increase in TKE extended to the top of the BL above the farm due to vertical transport and wind shear, significantly enhancing turbulent momentum fluxes. The TKE increased by a factor of 2 near the surface within the farm. Near-surface winds accelerated by up to 11%. These results are consistent with the few results available from observations and large-eddy simulations, indicating this parameterization provides a reasonable means of exploring potential downwind impacts of large wind farms.

1 February 2006 in Boundary-Layer Meteorology
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Journal Article
Closed access
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RBRobert J. Beare
Robert J. Beare
MMMalcolm K. Macvean
Malcolm K. Macvean
AHAlbert A. M. Holtslag
Albert A. M. Holtslag
Joan CuxartJoan Cuxart
Joan Cuxart
IEIgor Esau
Igor Esau
Peter P. SullivanPeter P. Sullivan
Peter P. Sullivan

1 April 2002 in Bulletin of the American Meteorological Society
Verified
Journal Article
Open access
GPGregory S. Poulos
Gregory S. Poulos
WBWilliam Blumen
William Blumen
DFDavid C. Fritts
David C. Fritts
JLJULIE LUNDQUIST
JULIE LUNDQUIST
JSJielun Sun
Jielun Sun
MJMichael Jensen
Michael Jensen
The Cooperative Atmosphere-Surface Exchange Study—1999 (CASES-99) refers to a field experiment carried out in southeast Kansas during October 1999 and the subsequent program of investigation. Comprehensive data, primarily taken during the nighttime but typically including the evening and morning transition, supports data analyses, theoretical studies, and state-of-the-art numerical modeling in a concerted effort by participants to investigate four areas of scientific interest. The choice of these scientific topics is motivated by both the need to delineate physical processes that characterize the stable boundary layer, which are as yet not clearly understood, and the specific scientific goals of the investigators. Each of the scientific goals should be largely achievable with the measurements taken, as is shown with preliminary analysis within the scope of three of the four scientific goals. Underlying this effort is the fundamental motivation to eliminate deficiencies in surface layer and turbul... Abstract The Cooperative Atmosphere-Surface Exchange Study—1999 (CASES-99) refers to a field experiment carried out in southeast Kansas during October 1999 and the subsequent program of investigation. Comprehensive data, primarily taken during the nighttime but typically including the evening and morning transition, supports data analyses, theoretical studies, and state-of-the-art numerical modeling in a concerted effort by participants to investigate four areas of scientific interest. The choice of these scientific topics is motivated by both the need to delineate physical processes that characterize the stable boundary layer, which are as yet not clearly understood, and the specific scientific goals of the investigators. Each of the scientific goals should be largely achievable with the measurements taken, as is shown with preliminary analysis within the scope of three of the four scientific goals. Underlying this effort is the fundamental motivation to eliminate deficiencies in surface layer and turbul...

1 November 2002 in Boundary-Layer Meteorology
Verified
Journal Article
Closed access
PDF file
RBR.M. Banta
R.M. Banta
RNR. K. Newsom
R. K. Newsom
JLJULIE LUNDQUIST
JULIE LUNDQUIST
YPY. L. Pichugina
Y. L. Pichugina
RCR. L. Coulter
R. L. Coulter
LML. Mahrt
L. Mahrt

26 November 2018 in Nature Energy
Verified
Journal Article
Closed access
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JLJULIE LUNDQUIST
JULIE LUNDQUIST
KDK. K. DuVivier
K. K. DuVivier
DKD. Kaffine
D. Kaffine
JTJ. M. Tomaszewski
J. M. Tomaszewski