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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
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Icarus 45 (1981), S. 638-652 
    ISSN: 0019-1035
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Physics
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Planetary and Space Science 30 (1982), S. 785-793 
    ISSN: 0032-0633
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 4
    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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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Annales geophysicae 12 (1994), S. 996-1005 
    ISSN: 0992-7689
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract A photochemical-transport two-dimensional model has been used to assess the impact of a projected fleet of high-speed stratospheric aircraft using different emissions scenarios. It is shown that the presence in the background atmosphere of nitric acid trihydrate aerosols is responsible for a lower stratospheric denoxification in addition to that caused by the sulfate aerosol layer. This has the effect of further decreasing the relative role of the odd nitrogen catalytic cycle for ozone destruction, so that the lower stratosphere is primarily controlled by chlorine species. The effect of aircraft injection of nitric oxides is that of decreasing the level of ClO, so that the lower stratospheric ozone (below about 20–25 km altitude) increases. The net effect on global ozone is that of a small increase even at Mach 2.4, and is enhanced by adopting emission scenarios including altitude restriction at 15 or 18 km. Reductions of the emission index (EI) of nitric oxides below relatively small values (about 15) are shown to reduce the aircraft-induced ozone increase, because of the associated smaller decrease of ClO. This conclusion is no more valid when the emission index is raised at the present values (about 45).
    Type of Medium: Electronic Resource
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  • 6
    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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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Human genetics 〈Berlin〉 51 (1979), S. 117-121 
    ISSN: 1432-1203
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Notes: Summary A 46,XY,r(10) karyotype was found in lymphocytes and skin fibroblasts cultured from a 8-month-old male showing multiple malformations and severe mental retardation. A comparison of the clinical features observed in cases in which a 10 ring was identified by means of banding techniques has been also attempted.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1432-0894
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract.  Nested limited-area modelling is one method of down-scaling general circulation model (GCM) climate change simulations. To give credibility to this method the nested limited-area model (LAM) must be shown to simulate local present-day climate conditions fairly accurately. Here seven different European limited-area models driven by observed boundary conditions (operational weather forecast analyses) are validated against observations, and inter-compared for summer and winter months. Relatively large biases are found. In summer large positive surface air temperature biases are found over southeast Europe. The main reason is deficiencies in the surface hydrological schemes causing an unrealistic drying of the soil. In at least one of the models, most likely several of them, an additional factor is an overestimation of incoming solar radiation. Apart from excessive precipitation in mountainous areas in some models they generally show a negative bias due to the drying and decreased advection from the Atlantic. In winter most models have a positive precipitation bias which seems to be caused by an enhancement of advection from the Atlantic and enhanced cyclone activity. Surface air temperature biases are negative probably due to an underestimation of the incoming longwave radiation.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1573-0662
    Keywords: polar stratospheric clouds ; air mass trajectories ; Lagragian model
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract Polar stratospheric clouds (PSC) were observed with the multi-wavelength lidar of the MOANA project (Modelling and Observations of Aerosols in the Northern Atmosphere) during SESAME (Second European Stratospheric Arctic and Mid-latitude Experiment). The physical state, liquid or solid, of the cloud particles can be inferred from the lidar data. Using isentropic back-trajectories to obtain the thermal history of the sampled air masses, it is possible to reconcile most of the observations with current ideas on PSC formation and evolution. When the cloud particles were identified as liquid, changes in the size distribution of the droplets along the trajectory were calculated using a micro-physical box model. Backscatter ratios calculated from the size distributions are in broad agreement with the lidar data, giving confidence in current understanding of the evolution of ternary solution (H2SO4, HNO3 and H2O) droplets. Results from two soundings are shown which bear on the problem of the formation of solid particles. In the first, solid particles were detected. The air mass had cooled to the frost point 12 hours earlier. In the second no solid particles were detected although the air temperature was below the nitric acid trihydrate existence point, and had decreased by 12K in the previous 14 hours.
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2012-12-18
    Description: Background— The role of statins in the prevention of contrast-induced acute kidney injury (CIAKI) is controversial. Methods and Results— First, we investigated the in vivo effects of atorvastatin on CIAKI. Patients with chronic kidney disease enrolled in the Novel Approaches for Preventing or Limiting Events (NAPLES) II trial were randomly assigned to (1) the atorvastatin group (80 mg within 24 hours before contrast media [CM] exposure; n=202) or (2) the control group (n=208). All patients received a high dose of N -acetylcysteine and sodium bicarbonate solution. Second, we investigated the in vitro effects of atorvastatin pretreatment on CM-mediated modifications of intracellular pathways leading to apoptosis or survival in renal tubular cells. CIAKI (ie, an increase 〉10% of serum cystatin C concentration within 24 hours after CM exposure) occurred in 9 of 202 patients in the atorvastatin group (4.5%) and in 37 of 208 patients in the control group (17.8%) ( P =0.005; odds ratio=0.22; 95% confidence interval, 0.07–0.69). CIAKI rate was lower in the atorvastatin group in both diabetics and nondiabetics and in patients with moderate chronic kidney disease (estimated glomerular filtration rate, 31–60 mL/min per 1.73 m 2 ). In the in vitro model, pretreatment with atorvastatin (1) prevented CM-induced renal cell apoptosis by reducing stress kinases activation and (2) restored the survival signals (mediated by Akt and ERK pathways). Conclusions— A single high loading dose of atorvastatin administered within 24 hours before CM exposure is effective in reducing the rate of CIAKI. This beneficial effect is observed only in patients at low to medium risk.
    Keywords: Cardiovascular imaging agents/Techniques, Apoptosis, Angiography
    Electronic ISSN: 1524-4539
    Topics: Medicine
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