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  • 1
    ISSN: 1573-093X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract The Pioneer Venus Orbiter (PVO) had on board the electron temperature probe experiment which measured temperature and concentration of electrons in the ionosphere of Venus. When the probe was outside the Venus ionosphere and was in the solar wind, the probe current was entirely due to solar photons striking the probe surface. This probe thus measured integrated solar EUV flux (Ipe) over a 13-year period from January 1979 to December 1991, thereby covering the declining phase of solar cycle 21 and the rising phase of solar cycle 22. In this paper, we examine the behavior of Ipe translated to the solar longitude of Earth (to be called EIpe) during the two solar cycles. We find that total EUV flux changed by about 60% during solar cycle 21 and by about 100% in solar cycle 22. We also compare this flux with other solar activity indicators such as F_10.7 , Lα, and the solar magnetic field. We find that while the daily values of EIpe are highly correlated with F_10.7 (correlation coefficient 0.87), there is a large scatter in EIpe for any value of this Earth-based index. A comparison of EIpe with SME and UARS SOLSTICE Lα measurements taken during the same period shows that EIpe tracks Lα quite faithfully with a correlation coefficient of 0.94. Similar comparison with the solar magnetic field (Bs) shows that EIpe correlates better with Bs than with F_10.7 . We also compare EIpe with total solar irradiance measured during the same period.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2019-07-16
    Description: The Airborne Raman Ozone, Temperature, and Aerosol Lidar (AROTEL) participatedin the recent SAGE III Ozone Loss and Validation Experiment (SOLVE) by providingprofiles of aerosols, polar stratospheric clouds (PSCs), ozone, and temperature with highvertical and horizontal resolution. Temperatures were derived from just above the aircraftto ca. 60 km geometric altitude with a reported vertical resolution of ca. 0.6 km. Thehorizontal footprint varied from 4 to 70 km. This paper explores the measurementuncertainties associated with the temperature retrievals and makes comparisons withindependent, coincident measurements of temperature. Measurement uncertainties rangefrom 0.1 to ca. 4 K depending on altitude and integration time. Comparisons betweenAROTEL and balloon sonde temperatures retrieved under clear sky conditions using bothRayleigh and Raman scattered data showed AROTEL ca. 1 K colder than sonde values.Comparisons between AROTEL and the Meteorological Measurement System (MMS) onNASAs ER-2 show AROTEL being from 2 to 3 K colder for altitudes ranging from 14 to18 km. Temperature comparisons between AROTEL and the UK Met Offices modelshowed differences of ca. 1 K below ca. 25 km and a very strong cold bias of ca. 12 K ataltitudes between 30 and 35 km.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 3
    Publication Date: 2019-07-16
    Description: NASA Goddard Space Flight Centers Airborne Raman Ozone, Temperature, andAerosol Lidar (AROTEL) measured extremely cold temperatures during all threedeployments (116 December 1999, 1429 January 2000, and 27 February to 15 March2000) of the SAGE III Ozone Loss and Validation Experiment (SOLVE). Temperatureswere significantly below values observed in previous years with large regions regularlybelow 191 K and frequent temperature retrievals yielding values at or below 187 K.Temperatures well below the saturation point of type I polar stratospheric clouds (PSCs)were regularly encountered, but their presence was not well correlated with PSCobservations made by NASA Langley Research Centers aerosol lidar colocated withAROTEL. Temperature measurements by meteorological sondes launched within areastraversed by the DC-8 showed minimum temperatures consistent in time and verticalextent with those derived from AROTEL data. Calculations to establish whether PSCscould exist at measured AROTEL temperatures and observed mixing ratios of nitric acidand water vapor showed large areas favorable to PSC formation but that were lackingPSCs. The flight on 12 December 1999 encountered large regions having temperatures upto 10 K below the NAT saturation temperature but only small, localized regions that mightbe identified as PSCs.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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