Zobrazeno 1 - 10
of 17
pro vyhledávání: '"J. M. Warnock"'
Publikováno v:
Journal of Geophysical Research: Atmospheres. 103:13689-13701
A primary objective of the 1995 and 1996 Flatland boundary layer experiments, known as Flatland95 and Flatland96, was to measure and characterize entrainment at the top of the convective boundary layer. The experiments took place in the area near the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28c7d03edbd4b10f072b4431df6fb7e9
https://doi.org/10.1029/98jd01150
https://doi.org/10.1029/98jd01150
Publikováno v:
Journal of Geophysical Research: Atmospheres. 102:6685-6701
We spectrally analyzed high-resolution balloon measurements of vertical profiles of temperature and horizontal wind in the troposphere and lower stratosphere over very flat terrain in Illinois. This paper is principally concerned with spectra in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::734167bfb26ceff9c7e4a4bf7c5834a6
https://doi.org/10.1029/96jd03784
https://doi.org/10.1029/96jd03784
Autor:
G. D. Nastrom, W. L. Clark, T. E. VanZandt, Patricia M. Pauley, K. S. Gage, J. M. Warnock, R. Creasey
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 11:14-21
The hypothesis that temporal averages of vertical motions over a single radar station are representative of weather systems large enough to be resolved by the radiosonde network is tested using data from the Flatland VHF radar, located in the very fl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::539e5b714d7089f4613d5111880287dd
https://doi.org/10.1175/1520-0426(1994)011<0014:csotvv>2.0.co
https://doi.org/10.1175/1520-0426(1994)011<0014:csotvv>2.0.co
Autor:
J. M. Warnock, T. E. VanZandt, H. S. Kim, W. L. Clark, Steven J. Franke, Paul E. Johnston, G. D. Nastrom
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 11:5-13
An experimental field campaign to measure synoptic-scale vertical velocities was conducted from 5 to 11 January 1991 in the Urbana-Champaign, Illinois, region, which is in very flat terrain far from mountains. Both the Flatland and the Urbana wind-pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba006b56e8c70b0a0f882cbd81ce540f
https://doi.org/10.1175/1520-0426(1994)011<0005:mossvv>2.0.co
https://doi.org/10.1175/1520-0426(1994)011<0005:mossvv>2.0.co
Autor:
J. M. Warnock, G. D. Nastrom
Publikováno v:
Journal of Applied Meteorology. 33:65-73
The so-called adiabatic method for estimating vertical air motions under isentropic flow conditions can be used with wind and temperature data from a single station. With the advent of radio acoustic sounding systems, wind and temperature measurement
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e5d4558539c89bee6233d3e0e0e150f
https://doi.org/10.1175/1520-0450(1994)033<0065:vmeudf>2.0.co
https://doi.org/10.1175/1520-0450(1994)033<0065:vmeudf>2.0.co
Publikováno v:
International Geoscience and Remote Sensing Symposium, 'Remote Sensing: Moving Toward the 21st Century'..
A knowledge of vertical air velocities associated with synoptic scale meteorological phenomena is important to practical weather prediction as well a:; to an understanding of these systems. At present, these vertical velocities a re inferred from a g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::036f9579cdf0d2e066e08c53f2c1bbf2
https://doi.org/10.1109/igarss.1988.570197
https://doi.org/10.1109/igarss.1988.570197
Publikováno v:
10th Annual International Symposium on Geoscience and Remote Sensing.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b35d662efcff6c694795ae0788a54cf9
https://doi.org/10.1109/igarss.1990.688540
https://doi.org/10.1109/igarss.1990.688540
Publikováno v:
Geophysical Research Letters. 15:269-272
A new VHF clear-air Doppler radar has been constructed in very flat terrain near Urbana, Illinois. This radar, called the Flatland radar, as presently configured measures a profile of the vertical component of the wind velocity every 2.5 minutes. It
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c3d160894bca165631e61d335b59b22
https://doi.org/10.1029/gl015i003p00269
https://doi.org/10.1029/gl015i003p00269
Publikováno v:
Radio Science. 20:1207-1213
During the last decade, great progress has been made in the use of sensitive VHF and UHF Doppler radars (often called MST, ST, or wind profiler radars) to study the dynamics of the clear air in the troposphere and middle atmosphere. Currently used tw
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e04d66bd5a2715564ddc237310bd55a1
https://doi.org/10.1029/rs020i006p01207
https://doi.org/10.1029/rs020i006p01207
Publikováno v:
Geophysical Research Letters. 5:109-112
Sensitive Doppler radars can measure the Doppler spectrum of echoes from refractive index irregularities in the clear air. In this paper horizontal winds estimated from the mean Doppler shift measured by the Sunset VHF Radar, near Boulder, CO, are co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2452541cfa5423aa8805f58aa6571145
https://doi.org/10.1029/gl005i002p00109
https://doi.org/10.1029/gl005i002p00109