Last edited by Mezikinos
Friday, May 8, 2020 | History

2 edition of Poker Flat MST radar data bases found in the catalog.

Poker Flat MST radar data bases

Poker Flat MST radar data bases

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  • 18 Currently reading

Published by U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Aeronomy Laboratory, For sale by the National Technical Information Service in Boulder, Colo, Springfield, Va .
Written in English

    Subjects:
  • Winds aloft -- Observations -- Databases.,
  • Automatic meteorological stations.

  • Edition Notes

    StatementA.C. Riddle ... [et al.].
    SeriesNOAA technical memorandum ERL AL -- 11.
    ContributionsRiddle, Anthony C., Aeronomy Laboratory (U.S.)
    The Physical Object
    FormatMicroform
    Paginationiv, 137 p.
    Number of Pages137
    ID Numbers
    Open LibraryOL17674881M

    The semidiurnal tide also exhibits phase fluctuations indicating the possible presence of a transient S(,2,3) mode. A post-processing selection algorithm is used to determine the meteor echoes detected on the Poker Flat, Alaska, MST radar from a composite database consisting of . Entrance to Poker Flat Research Range The Poker Flat Research Range (PFRR) is a launch facility and rocket range for sounding rockets in the U.S. state of Alaska. The world's largest land-based rocket range, it is on a 5,acre ( km 2) site about 30 miles (50 km) northeast of Fairbanks and degrees south of the Arctic Circle.

    We examine the seasonal, day-to-day, and diurnal fluctuations of Cn2 using data from the mesosphere, stratosphere, troposphere (MST) radar at Poker Flat, Alaska. The radar has been operated in a nearly continuous mode since early , with profiles recorded every 2 to 4 by: Documents:Data Volume. From CedarWiki. Jump to: CEDAR DATABASE VOLUME BY INSTRUMENT Mass store archive summary for public copy volumes in '/ISRADAR' as of May 26 Particle Flux PKF Poker Flat AK Scanning Imaging F-P Spec PKR Poker Flat Alaska MST Radar PLA Platteville Colorado ST (MEDAC) Radar PLR

    (, The Poker Flat MST radar system: Current status and capabilities, 20th Conference on Radar Meteorology, Nov. 30 - Dec. 3. Bowhill, S. A. and P. E. Mayes (, Proposal for engineering and cost study of a phased array antenna for Urbana coherent scatter radar, Aeron. Lab., Dep. Elec. Eng. Balsley, B. B., and R. Garello (), The kinetic energy density in the troposphere, stratosphere and mesosphere: A preliminary study using the Poker Flat radar in Alaska, Radio Sci. 20, – CrossRef Google ScholarCited by:


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Poker Flat MST radar data bases Download PDF EPUB FB2

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With some limitations the system will be capable of measuring winds, waves, and turbulence throughout the 1‐ to ‐km height range. Data obtained from the portion of the Poker Flat system already in operation are presented and by: With some limitations the system will be capable of measuring winds, waves, and turbulence throughout the 1- to km height range.

Data obtained from Poker Flat MST radar data bases book portion of the Poker Flat system already in operation are presented and discussed. PRELIMINARY RESULTS system at a later time involves phase coding of POKER FLAT PPELIMIMARY MST RADAR DATA RECEIUER â ¢1 The partially completed Poker Flat MST radar was put into operation on Februand has continued to operate during the construction phaseof the full portion of the system usesone quarter of the completeantenna and only one transmitter.

Meteor echoes received on the mesosphere‐stratosphere‐troposphere radar at Poker Flat, Alaska, have been tested for their usefulness in studying the large‐scale dynamics of the upper mesosphere and Cited by: Observations with the Poker Flat, Alaska, MST radar during and after solar proton events in and suggest that winds in the altitude range of.

Poker Flat Research Range has five major launch pads. Pads 1 and 2 each have a K launcher, pads 3 and 4 each contain 20K MRL launchers, and pad 5 contains a 4K twinboom launcher.

Pads 1 and 2 each have a K launcher, pads 3 and 4 each contain 20K MRL. The paper describes the initial results obtained during the first 60 days of continuous operation of the MST radar under construction at Poker Flat, Alaska.

A comparison is made between tropospheric wind profiles obtained by the radar and concurrent windsonde profiles. Journal of Atmospheric and Terrestrial Physics, Vol. 55, No. 9, pp. Printed in Great Britain. /93 S+ Pergamon Press Ltd Poker Flat MST radar observations of high latitude neutral winds at the mesopause during and after solar proton events R.

JOHNSON* and J. LUHMANN+ * Space Physics Research Laboratory, University of Michigan, Ann Arbor, MIU Cited by: Rottger (). MST Radars can be utilized for observing wind, waves and turbulence (Gage and Balsley, ). Balsley and Garello () analysed the short period wind fluctuations over poker Flat, Alaska using the Poker Flat MST Radar.

The vertical velocity power spectra was studied by Ecklund et al. () using poker flat MST Size: 1MB. MST radar is a high-resolution atmospheric detecting radar with three operational modes: low mode (3 to 10 km), middle mode (10 to 25 km), and high mode (60 to 90 km) with all-weather and.

MF radar wind measurements in the mesosphere and lower thermosphere over Poker Flat, Alaska (° N, ° W) are used to study the features of mean winds and solar tides. We describe initial results obtained during the first 60 days of continuous operation of the MST radar under construction at Poker Flat, Alaska.

Tropospheric‐stratospheric wind profiles obtained by the radar are compared with concurrent windsonde profiles. Mesospheric echoes between 57‐72 km are observed during daytime periods of ionospheric absorption.

Mesospheric winds obtained following. Poker Flat MST radar data bases. Personal Author: Riddle, Anthony C. Corporate Authors: Aeronomy Laboratory (U.S.) Published Date: Series: NOAA technical memorandum ERL AL ; 11 File Type: [PDF - MB] A tropical cyclone data tape for the eastern and central North Pacific basins, contents, limitations, and uses Cited by: 1.

Poker Flat MST radar data bases. Personal Author: Riddle, Anthony C. Corporate Authors: Aeronomy Laboratory (U.S.) Published Date: Series: NOAA technical memorandum ERL AL ; 11 File Type: [PDF - MB] Geodetic glossary.

Corporate Authors: National Geodetic Survey (U.S.). Cited by: 4. Kishore et al.: MF radar observations of mean winds and tides over Poker Flat, Alaska Fig. Time-height cross section of the mean zonal wind component (bot-tom) observed at Poker Flat from Octo-ber to December HWM93 (Hedin et al., ) model contours for Poker Flat are given in the top panel.

Shaded regions represent the. Zonal and meridional wind measurements made with the Poker Flat MST radar over a day period are used to calculate the frequency power spectra at heights between and km.

The winds used in the analysis are 1 h averages of samples taken every 4 by: MF radar wind measurements in the mesosphere and lower thermosphere over Poker Flat, Alaska (° N, ° W) are used to study the features of mean winds and solar tides. Continuous observation with the newly installed radar is in progress and in the present study we have analyzed a database of the first 27 months (October –December.

The basic form arises from theoretical considerations of radar noise; the final form includes empirical modifications based on radar observations. While SNR min was originally developed using data from the MHz profiler at Poker Flat, Alaska, it works well with data collected from a wide range of locations, frequencies, and parameter settings Cited by: Poker Flat Mesosphere, Stratosphere, Troposphere (MST) Radar on the Poker Flat Rocket Range near Fairbanks, Alaska.

The MST Radar, operating at a frequency of 50 MHz, profiled the three vector components of wind velocity with a 2 kilometer vertical resolution and a 2 to kilometer vertical range.

Scientists from the. A post processing selection algorithm is used to determine the meteor echoes detected on the Poker Flat, Alaska, MST radar from a composite database consisting of meteor and turbulence echoes.

The echo distributions depend on the geometry of the antenna beams, the presence of strong turbulence echoes, average power transmitted, and the number Author: David Tetenbaum.Observation of upper-mesospheric neutral winds made during two energetic Solar Proton Events (SPEs) by the Poker Flat, MST radar are presented.

These results allow the low-altitude limits of magnetospheric coupling to the neutral atmosphere to be determined.Cambridge Core - Atmospheric Science and Meteorology - Atmospheric Radar - by Wayne K.

Hocking Characterization of atmospheric structures observed by a VHF MST-type radar in the troposphere over Santa Cruz, Costa Rica. Earth, Planets and Space, Vol. 71, Issue.

1, View all Google Scholar citations for this by: 7.