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  • 1
    Online Resource
    Online Resource
    Amsterdam :IOS Press, Incorporated,
    Keywords: Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (365 pages)
    Edition: 1st ed.
    ISBN: 9781614992103
    Series Statement: International School of Physics Enrico Fermi Series ; v.124
    Language: English
    Note: Title Page -- Indice -- Preface -- Gruppo fotografico dei partecipanti al Corso -- GROUND-BASED TECHNIQUES -- The measurement of tropospheric trace gases by long-path absorption: OH and ancillary gases -- Introduction -- Experiment description: OH -- Experiment description: white light -- Summary -- The ground-based measurement of stratospheric trace gases using quantitative millimeter wave emission spectroscopy -- Introduction -- The observational challenge -- Specifying the problem -- Atmospheric absorption of stratospheric signals -- Choice of frequencies for observing -- Observing goals -- Instrumental considerations -- Spectral quality -- Functional operation of a millimeter wave spectrometer -- Scale factor accuracy -- Opacity vs. integration time -- Low-opacity observing sites -- Some further comments on recovery of vertical profiles from line shape deconvolution -- Criteria for observability of molecules in the middle atmosphere -- A short history of radar leading to atmospheric profiling -- Introductory remarks -- Earliest analogs to radar -- A brief history of the development of radio -- A brief history of the development of radar -- A brief history of the development of atmosphere radar technology -- Development of generic radar equations for wind profiling -- General comments -- Derivation of the point-to-point < -- < -- range> -- > -- equation -- Derivation ofthe < -- < -- hard-target> -- > -- radar equation -- Derivation of the < -- < -- soft-target> -- > -- radar equation -- Derivation of the Fresnel reflection radar equation -- General comments -- A simple derivation of the first Fresnel zone -- Derivation of the Fresnel scatter radar equation -- Radar wind profiling -- Introductory comments -- What is a profiler? -- What are the basic principles underlying the profiler technology?. , The radio refractive index of the atmosphere -- Volume scattering coefficient for turbulent scatter -- A basic profiler system -- Examples of specific capabilities of wind profilers -- The use of kites for atmospheric research -- Introduction -- Early history of scientific kite flights -- The Christmas Island kite experiment -- Overview -- Data presentation -- Extrapolation of the Christmas Island results to higher, more prolonged flights -- Measurement systems using the kite as a < -- < -- Skyhook> -- > -- -- Types of sensors and weight considerations -- Payload connection -- Sensor power sources -- Concluding remarks -- AIRBORNE MEASUREMENTS -- Sampling of particles and gases from the NASA ER-2 -- Introduction -- Description of the NASA ER-2 -- Sampling requirements and strategies -- Gases -- Aerosol -- Applications of the ER-2 payload -- In situ measurements of stratospheric trace gases from aircraft -- Introduction -- Some properties of the stratosphere that affect in situ measurements -- Guidelines for making meaningful measurements of stratospheric trace gases -- Simultaneous measurements of trace gases -- Simultaneous measurements of a gas that traces atmospheric motion -- Frequency and location of measurements -- Measurements for the NASA ER-2 aircraft -- Instruments on the ER-2 -- Ozone -- Aircraft Laser Infrared Absorption Spectrometer (ALIAS) -- NO and NOy chemiluminescence -- ClO and BrO -- ER-2 instruments as diagnostic tools -- Conclusion -- In situ measurement of tropospheric OH and HO2 by laser-induced fluorescence at low pressure -- Importance of OH and HO2 measurements -- The photochemistry of OH in the troposphere -- Instruments for measuring OH and HO2 -- Instrument design and operation -- Instrument sensitivity -- Minimum detectable OH -- Specificity -- Possible interfering signals -- Calibrations. , Possible chemical loss of OH and HO2 in the instrument -- Detection of H02 -- Detection of tropospheric OH and HO2 -- Design for an aircraft OH/HO2 instrument -- Projected sensitivity for OH and H02 for the aircraft instrument -- Summary -- SPACEBORNE MEASUREMENTS -- UV remote sensing of the Earth's atmosphere -- Introduction -- Background -- Methods for measurement of ozone from space -- Basic physics of UV nadir sounding -- Theoretical UV reflectivity of the Earth's atmosphere -- Single-scattering case -- Multiple scattering -- Ozone profile retrievals -- Total-ozone soundings -- Total-ozone retrieval method -- Two absorber retrievals -- Kerr algorithm -- Satellite data -- Nadir-sounding instrument designs -- BUV-type instruments -- SBUV instruments -- TOMS instruments -- TOMS design requirements -- Satellite characteristics -- Ground resolution -- Optical design -- Wavelength selection -- Spectrometer and detector -- Foreoptics -- Total-ozone calibration -- Sulfur dioxide calibration -- Sulfur dioxide measurement precision -- Sulfur dioxide validation -- Total-ozone results -- Comparison with BUV sampling -- Short-term spatial variations in total ozone -- Long-period variations in ozone -- Ozone trends -- Ozone holes -- Sulfur dioxide results -- Volcano-climate relations -- Satellite occultation measurements of the Earth's atmosphere using SAM II, SAGE and SAGE II -- Introduction -- Solar-occultation technique -- Limb transmission and optical depth -- Instrumentation -- Inversion analysis -- Highlights of SAM II, SAGE and SAGE II observations -- Volcanic aerosols and polar stratospheric clouds -- Ozone hole and ozone trends -- Water vapor and clouds -- Concluding remarks -- Far-infrared remote sensing of the Earth's atmosphere -- Introduction -- The spectrum of the atmosphere -- Instrumentation -- Fourier transform spectroscopy. , Fabry-Perot spectroscopy -- Far-infrared remote sensing -- Balloon-borne observations -- Instrumentation -- Limb sounding -- Minor constituents -- Data analysis -- The forward problem -- The inverse problem -- Laboratory spectroscopy -- Space applications -- THEORY AND ANALYSIS -- Satellite temperature retrievals in the stratosphere and the quality for trend detection -- Introduction -- NOAA satellite temperature retrievals -- Comparisons with ground-based rocktsonde data -- Analysis gridding procedures -- Data quality -- Summary -- Comparisons of satellite and ground-based temperature profiles -- Introduction -- Compatibility between Datasonde adjusted NMC analyses and LIDAR temperatures at OHP and CEL -- Comparison of NMC analyses and temperature lidar observations including consideration of the atmospheric diurnal cycle -- Summary -- Trends of stratospheric ozone and temperature -- Introduction -- Statistical methodology -- Ozonesonde and rawinsonde trend results -- Umkehr aerosol considerations -- Umkehr trend comparisons -- SBUV, SBUV/2 ozone profile trends -- Summary -- Ozone trends from TOMS data -- Introduction -- The TOMS instrument -- Statistics of total-ozone data from TOMS -- Recent trends in total ozone from TOMS -- Summary -- Trajectory modelling -- Introduction -- Trajectory models -- Conservation properties -- Numerical modelling -- Isentropic vs. quasi-isentropic -- Comparison with observations -- Modern uses of trajectory models -- Mixing and transport -- Dynamical modelling -- Chemical modelling -- Trajectory mapping -- Injected pollutants -- Summary -- Gravity waves in the troposphere -- Introduction -- The mathematical model -- Linear theory: plane-wave solution -- Linear theory: large-Rossby-number flow -- General case -- Isothermal and constant-background-wind case -- The Boussinesq approximation. , Linear theory: Rossby number of order-one flow -- Stability analysis -- Wave-turbulence interactions -- The phase-averaging operator and the equations of motions -- Turbulence -- Gravity wave-convection interactions -- Gravity wave generation mechanisms -- Appendix.
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  • 2
    Keywords: Mesosphere. ; Dynamic meteorology. ; Electronic books.
    Description / Table of Contents: Proceedings of the Fourth ESRIN-ESLAB Symposium Held in Frascati, Italy, July 6-10, 1970.
    Type of Medium: Online Resource
    Pages: 1 online resource (308 pages)
    Edition: 1st ed.
    ISBN: 9789401031141
    Series Statement: Astrophysics and Space Science Library ; v.25
    Language: English
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  • 3
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Review of Scientific Instruments 63 (1992), S. 2940-2944 
    ISSN: 1089-7623
    Source: AIP Digital Archive
    Topics: Physics , Electrical Engineering, Measurement and Control Technology
    Notes: A high-resolution Fabry–Perot interferometer was inserted in a feedback loop which, by monitoring elements of the fringe pattern, keeps the position of the transmitting window fixed with respect to a given line, taking into account the instability of the radiation source which would produce a wander of the line itself and the noise affecting the tuning of the receiving interferometer. The system, in this preliminary form, is able to lock itself and maintain its position indefinitely for slow and moderately fast varying disturbances.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 199 (1963), S. 1275-1276 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The optical radar consists of an RCA-designed ruby laser delivering short pulses of approximately 50 nsec, 0.5 joule at λ=6,940 ; of a transmitting refracting telescope of 7.5-cm diameter and 201-cm focal length; of a receiving reflecting telescope of 32-cm diameter and 270-cm focal length, and of ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Physics Letters A 26 (1968), S. 614-615 
    ISSN: 0375-9601
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Pure and applied geophysics 91 (1971), S. 166-170 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Summary In this note we report preliminary measurements of sodium twilight emissions showing the variation of theD 2 /D 1 ratio during twilight at solar depression angles α as low as 3.5°.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 228 (1970), S. 1079-1080 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The graphs in Fig. 1 indicate the average variations of rotational temperature and intensity throughout the night, referred to the hour of sunset and to the local midnight. The graphs were obtained by considering, for each night, the difference in rotational temperature and relative intensity at ...
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract In the period June–July 1992, four Doppler sodars were operated simultaneously in Rome and the surrounding area. The data have been used to investigate the contributions from sea breeze events to the local low-level circulation. Three days in which synoptic-scale pressure gradients were weak have been selected. A number of characteristics of the sea breeze are examined including the onset and cessation of the phenomenon, the behavior of the wind speed, and the depth of the density flow. The time propagation of the events and the influence of orography are obtained from a comparison between the data at different sites. The low-level circulation in the early morning is associated with the land breeze and appears to be enhanced by a mountain wind from the surrounding hills. The observed behavior of the vertical velocity field associated with the sea breeze is consistent with model predictions.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1573-1472
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Convective plume patterns, characteristic of clear sky and light wind daytime boundary layers over land, were observed for two nights with a tri-axial Doppler sodar operated in the central area of Rome during the summer of 1994. An urban heat island effect, combined with a continuation of a breeze from the sea late into night during both days, is believed to be responsible for the observed nocturnal convection. Estimates of the surface heat flux and the vertical velocity scaling parameter are obtained from profiles of vertical velocity variance, and the Raman lidar water vapor measurements are used to obtain the humidity scaling parameter. Convective scaling results for vertical wind and humidity fairly agree with the results of other experiments and models. On the basis of available measurements, it appears that mixed-layer similarity formulations used to characterize the daytime convective boundary layer over horizontally homogeneous surfaces can also be applied to the nocturnal urban boundary layer during periods of reasonable convective activity.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Journal of atmospheric chemistry 23 (1996), S. 5-35 
    ISSN: 1573-0662
    Keywords: polar stratospheric clouds ; computer model ; South Pole ; HNO3 and H2O depletion ; water vapor profiles ; backscattering
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract A 1-D model of the formation and seasonal evolution of Polar Stratospheric Clouds (PSCs) is described. The model considers PSCs of types 1 and 2 in the vertical range from 8 to 30 km and utilizes real temperature data. The micro-physical processes included in the model are the heterogeneous nucleation and condensation (or evaporation), while sedimentation, gas diffusion and vertical wind velocity are the processes responsible for transport. Model simulations have been compared with PSC data obtained by lidar at the South Pole: results for the winter 1990 are discussed. The different contribution of type 1 and type 2 PSCs to the measured backscattering coefficient has been evidenced. In the simulations, layers of NAT particles form when low values of the backscattering coefficient are measured; similarly, ice particles form when sharper and rapidly changeable structures with higher values of the backscattering coefficient are observed. Significant results on the condensation and depletion of HNO3 and H2O are presented. Water vapor profiles measured during winter 1990 are reproduced quite well.
    Type of Medium: Electronic Resource
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