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  • 2005-2009  (29)
  • 1975-1979  (13)
  • 1970-1974  (2)
  • 1880-1889  (7)
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  • 1
    Publication Date: 2019-07-17
    Description: The isotope (dO18 or dD) variability in ice cores from non-tempered Alpine glaciers might provide long term temperature proxy records at mid-latitudes supplementing respective Polar records. Concerning the last millennium, this exclusively applies to the low accumulation Colle Gnifetti (4450 m asl, Swiss-Italian Alps), though depositional noise challenges reliable temperature reconstruction there. For two ice cores from this drill site a substantial covariation in trends between atmospheric temperature and water isotopes has already been found for the last 250 years- including important exceptions, however. Thus, the decadal isotope variations remain still to be proved as a faithful temperature signal. For Colle Gnifetti, this task is adressed on the basis of the extensive instrumental temperature records provided by the HISTALP network. Here we restrict ourselves as a first step on the last century, where shortcommings in both archives are not yet obstructive- such as ice core dating uncertainties and ambiguities associated with the early instrumental period. Aimed at assessing the temperature related signal embedded in the isotope variability we include isotope time series from four down-to-bedrock ice cores subject to different glaciological regimes. Dedicated time series analysis yields a common signal in the decadal components. For a sound comparsion, a special Colle Gnifetti relevant temperature time series is constructed from the high elevation stations of the HISTALP network. This attempt includes weighting for precipitation and net accumulation, resulting in an ice core relevant temperature record mostly associated with growing seasons. The intercomparison of trends yields a common decadal variability between temperature and ice core isotope data. Thereby the potential of the Colle Gnifetti ice cores in Alpine paleoclimate research is assessed, which may include the early instrumental correction debate.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 2
    Publication Date: 2019-07-17
    Description: The variabilty of water isotopes (delta-O18 or delta-D) preserved in Alpine glaciers may provide mid-latitude temperature records supplementing respective proxy information from other archives. However, concerning long term records (i.e. exceeding 100 years) the limited glacier depth of suitable Alpine drill sites requires a relatively low accumulation rate. As a result, depositional noise is found to strongly challenge the interpretation of these isotope records in terms of net temperature change. Here we present results from our multi core array at the low accumulation Colle Gnifetti (CG) site (4450m asl, Swiss-Italian Alps) dedicated to assess the potential of long term ice core isotope records for paleoclimate reconstruction. To do so, a specific CG relevant temperature time series is synthesized from the high elevation stations of the instrumental HISTALP network considering among others the accumulation bias towards growing seasons. Within the last century (where dating and homogenity problems do not matter) dedicated time series analysis reveals a common signal in the decadal components of the temperature record and isotope records of four ice cores. Throughout the entire 250 year instrumental period, exceptions occur within the early instrumental period, as well as an unexpectedly high isotope-temperature sensitivity. An inter-core correspondence in the temperature related decadal trends can be revealed for two cores throughout the last 500 years. On a tentative basis, we discuss the delta O18-record of a new CG ice core dedicated to last 1000 years in view of constraints arising from varying time resolution, dating uncertainties and systematic glaciological up-stream effects.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , notRev
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Journal of ornithology 30 (1882), S. 178-209 
    ISSN: 1439-0361
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Journal of ornithology 33 (1885), S. 50-61 
    ISSN: 1439-0361
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Journal of ornithology 33 (1885), S. 67-73 
    ISSN: 1439-0361
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Journal of ornithology 33 (1885), S. 35-49 
    ISSN: 1439-0361
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Journal of ornithology 33 (1885), S. 61-67 
    ISSN: 1439-0361
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract The g-factors of the 11/2− states in145, 147, 149Eu were measured by the TDPAD method in metallic Sm-targets. The temperature dependence of the paramagnetism in the system145EuSm follows strictly a Curie-Weiß law Beff=B0[1+¯C/(T-θ)] with C=−50(2)K and θ=−29(5)K. Extrapolation to T→∞ yields g(145Eu)=+1.356(8), g(147Eu)=+1.28(1) and g(149Eu)=+1.27(5). In addition, the quadrupole coupling constantν Q=12.5(5) MHz, and a lower limit for the paramagnetic relaxation time τ = 1 us was determined at room temperature for the 11/2− state of145Eu in Sm. Extensive studies of the anomaly of magnetic moments in the vicinity of the closed neutron shells N=50 and N=126 have unambiguously revealed an anomaly of the proton gl factor of δgl≈0.1 [1]. In the present letter we report on a similar investigation for the closed neutron shell N=82. For this purpose the g-factors of the first excited 11/2− states in the rare earth isotopes145, 147, 149Eu were measured. Due to paramagnetic effects, a measurement of nuclear g-factors in the rare earth region requires the investigation of the paramagnetic behaviour of the probe atoms in the chosen target material. The g-factors in145,147,149Eu were measured by the method of the time differential perturbed angular distribution (TDPAD) of the deexcitationγ-rays. The 11/2− states in145Eu(EX=716 keV, T1/2=0.49 gms) and in149Eu(EX=497 keV, T1/2=2.43 μs) were populated and aligned by the nuclear reaction144,148sm(d,n)145,149Eu with the pulsed deuteron beam (Ed=11 MeV) of the Erlangen tandem accelerator. Enriched metallic Sm targets of 89%144Sm and 95%148Sm were used. The 11/2− state in147Eu(EX=625 keV, T1/2=0.77 μs) was excited by the reaction147Sm(p,n)147Eu with a pulsed proton beam (Ep=10 MeV) using a 93% enriched147Sm target. A detailed description of the experimental set-up and the evaluation procedure for the present TDPAD measurements is given in ref. [2]. The deexcitation γ-rays of the isomeric Eu states were detected by two NaJ(T1) detectors encompassing an angle of Δθ=90°, and placed in a plane perpendicular to the external applied magnetic field direction. The magnetic field was calibrated by measuring the very precisely known g-factor of the isomeric 5/2+ state of19F in a BaF2 target. The Sm targets were mounted either in an oven for the high-temperature measurements or into a copper cooling-rod for temperatures down to liquid nitrogen.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 291 (1979), S. 49-52 
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Theg-factor of the first excited state in the odd-odd nucleus138La (E x=73 keV,I π,T 1/2=116 ns) was measured by the time-differential perturbed angular distribution (TDPAD) method. The result, corrected for Knight shift and diamagnetic shielding, isg=+0.962±0.016. This value can be fairly well reproduced using the additivity relation for magnetic moments, empirical values for the odd-proton and odd-neutrong-factors, and an experimentally deduced wave function for the 3+ state.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    The European physical journal 278 (1976), S. 133-137 
    ISSN: 1434-601X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Theg-factor of the 1,275 keV 2+ state in22Ne has been measured by means of the time-differential recoil-into-vacuum (plunger) technique. An analysis including excited heliumlike electronic configuration was performed. A fit, which includes all these electronic states, provides a value of ¦g¦=0.36±0.03.
    Type of Medium: Electronic Resource
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