Articles | Volume 15, issue 7
https://doi.org/10.5194/acp-15-3785-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-3785-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
High-resolution observations of the near-surface wind field over an isolated mountain and in a steep river canyon
B. W. Butler
CORRESPONDING AUTHOR
US Forest Service, Rocky Mountain Research Station, Missoula Fire Sciences Laboratory, 5775 Hwy 10 Missoula, MT 59808, USA
N. S. Wagenbrenner
US Forest Service, Rocky Mountain Research Station, Missoula Fire Sciences Laboratory, 5775 Hwy 10 Missoula, MT 59808, USA
Washington State University, Laboratory for Atmospheric Research Pullman, WA 99164-2910, USA
J. M. Forthofer
US Forest Service, Rocky Mountain Research Station, Missoula Fire Sciences Laboratory, 5775 Hwy 10 Missoula, MT 59808, USA
B. K. Lamb
Washington State University, Laboratory for Atmospheric Research Pullman, WA 99164-2910, USA
K. S. Shannon
US Forest Service, Rocky Mountain Research Station, Missoula Fire Sciences Laboratory, 5775 Hwy 10 Missoula, MT 59808, USA
D. Finn
NOAA Air Resources Laboratory, Field Research Division 1750 Foote Dr. Idaho Falls, ID 83402, USA
R. M. Eckman
NOAA Air Resources Laboratory, Field Research Division 1750 Foote Dr. Idaho Falls, ID 83402, USA
K. Clawson
NOAA Air Resources Laboratory, Field Research Division 1750 Foote Dr. Idaho Falls, ID 83402, USA
L. Bradshaw
US Forest Service, Rocky Mountain Research Station, Missoula Fire Sciences Laboratory, 5775 Hwy 10 Missoula, MT 59808, USA
P. Sopko
US Forest Service, Rocky Mountain Research Station, Missoula Fire Sciences Laboratory, 5775 Hwy 10 Missoula, MT 59808, USA
S. Beard
NOAA Air Resources Laboratory, Field Research Division 1750 Foote Dr. Idaho Falls, ID 83402, USA
D. Jimenez
US Forest Service, Rocky Mountain Research Station, Missoula Fire Sciences Laboratory, 5775 Hwy 10 Missoula, MT 59808, USA
C. Wold
US Forest Service, Rocky Mountain Research Station, Missoula Fire Sciences Laboratory, 5775 Hwy 10 Missoula, MT 59808, USA
M. Vosburgh
US Forest Service, Rocky Mountain Research Station, Missoula Fire Sciences Laboratory, 5775 Hwy 10 Missoula, MT 59808, USA
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Revised manuscript not accepted
Related subject area
Subject: Dynamics | Research Activity: Field Measurements | Altitude Range: Mesosphere | Science Focus: Physics (physical properties and processes)
Variations in global zonal wind from 18 to 100 km due to solar activity and the quasi-biennial oscillation and El Niño–Southern Oscillation during 2002–2019
Radar observations of winds, waves and tides in the mesosphere and lower thermosphere over South Georgia island (54° S, 36° W) and comparison with WACCM simulations
Simultaneous in situ measurements of small-scale structures in neutral, plasma, and atomic oxygen densities during the WADIS sounding rocket project
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On the origin of the mesospheric quasi-stationary planetary waves in the unusual Arctic winter 2015/2016
Influence of geomagnetic activity on mesopause temperature over Yakutia
Quasi-12 h inertia–gravity waves in the lower mesosphere observed by the PANSY radar at Syowa Station (39.6° E, 69.0° S)
Change in turbopause altitude at 52 and 70° N
Characteristics and sources of gravity waves observed in noctilucent cloud over Norway
Observation of a mesospheric front in a thermal-doppler duct over King George Island, Antarctica
The role of the QBO in the inter-hemispheric coupling of summer mesospheric temperatures
Xiao Liu, Jiyao Xu, Jia Yue, and Vania F. Andrioli
Atmos. Chem. Phys., 23, 6145–6167, https://doi.org/10.5194/acp-23-6145-2023, https://doi.org/10.5194/acp-23-6145-2023, 2023
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Winds are important in characterizing atmospheric dynamics and coupling. However, it is difficult to directly measure the global winds from the stratosphere to the lower thermosphere. We developed a global zonal wind dataset according to the gradient wind theory and SABER and meteor radar observations. Using the dataset, we studied the intra-annual, inter-annual, and long-term variations. This is helpful to understand the variations and coupling of the stratosphere to the lower thermosphere.
Neil P. Hindley, Nicholas J. Mitchell, Neil Cobbett, Anne K. Smith, Dave C. Fritts, Diego Janches, Corwin J. Wright, and Tracy Moffat-Griffin
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T. D. Demissie, P. J. Espy, N. H. Kleinknecht, M. Hatlen, N. Kaifler, and G. Baumgarten
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J. V. Bageston, C. M. Wrasse, P. P. Batista, R. E. Hibbins, D. C Fritts, D. Gobbi, and V. F. Andrioli
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P. J. Espy, S. Ochoa Fernández, P. Forkman, D. Murtagh, and J. Stegman
Atmos. Chem. Phys., 11, 495–502, https://doi.org/10.5194/acp-11-495-2011, https://doi.org/10.5194/acp-11-495-2011, 2011
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Short summary
Interest in numerical wind models continues to increase, especially for models that can simulate winds at relatively high spatial resolution (~100m). However, limited observational data exist for evaluation of model predictive performance. This study presents high-resolution surface wind data sets collected from an isolated mountain and a steep river canyon. The data are available to the public at http://www.firemodels.org/index.php/windninja-introduction/windninja-publications.
Interest in numerical wind models continues to increase, especially for models that can simulate...
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