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  • English  (6)
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  • 1
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    In:  Protokoll über das 27. Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung : Breklum, 25.-29. September 2017
    Publication Date: 2020-02-12
    Description: The MT data used in this survey was acquired in a Hot-Dry-Rock survey of the Chinese Geological Survey in 2016, and the AMT data was acquired in another geological resource survey in 2015. The main purpose of the MT and AMT exploration is to investigate the geological structure, structural characteristics of rock mass, fissure development characteristics, and the contact relationship between rock mass and cover.
    Language: English
    Type: info:eu-repo/semantics/conferenceObject
    Format: application/pdf
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  • 2
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    In:  4th Mini Conference on Noble Gases in the Hydrosphere and in Natural Gas Reservoirs
    Publication Date: 2020-02-12
    Language: English
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  • 3
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-06-08
    Description: In 2017, the Chinese government announced the development of another metropolis called Xiong'an New Area (XNA) to relieve the population and service pressures affecting Beijing. By the programs of the Chinese governments, the largest natural freshwater wetland of the XNA, Lake Baiyangdian (BYD), will provide the key ecosystem services for the region. However, whether the hydrological conditions of BYD can support this booming metropolis is still unclear. To maintain the ecosystem function of BYD and provide ecological services for the XNA, the annual ecological water demands of BYD ranged from 3.10×10〈sup〉8〈/sup〉 m〈sup〉3〈/sup〉 to 6.35 ×10〈sup〉8〈/sup〉 m〈sup〉3〈/sup〉 under different water exchange scenarios. Due to the insufficient water resources within the watershed, under the scenario of a 1.0 time yr〈sup〉-1〈/sup〉 frequency of lake water exchange, in wet years, normal flow years and dry years 1.32×10〈sup〉8〈/sup〉 m〈sup〉3〈/sup〉, 2.10×10〈sup〉8〈/sup〉 m〈sup〉3〈/sup〉 and 3.38×10〈sup〉8〈/sup〉 m〈sup〉3 〈/sup〉of external water from the Yellow and Yangtze Rivers must be transferred into BYD to satisfy the ecological restoration of the XNA, and the costs may be as much as 77~277 million RMB (11.0~39.57 million USD) per year. The predicted results show that the external water demands may decrease slightly by 0.58×10〈sup〉8〈/sup〉~0.95×10〈sup〉8〈/sup〉 m〈sup〉3〈/sup〉 yr〈sup〉-1〈/sup〉 and 1.02×10〈sup〉8〈/sup〉~1.18×10〈sup〉8〈/sup〉 m〈sup〉3〈/sup〉 yr〈sup〉-1〈/sup〉 in the 2030s and 2050s, respectively. Agricultural water consumption reduction, inflow water quality improvement and the intelligent use and management of urban reclaimed water are necessary for maintaining the ecosystem function of BYD, and externally transferred water may be a potential factor needed to support the growing XNA.
    Language: English
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  • 4
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-07-28
    Description: Whether active fractures are thermal anomalies is a cutting-edge scientific issue in geothermics. Geothermal measurements of the San Andreas Fault reveal no heat flow anomaly, and then the "heat flow paradox" was proposed. The Tan Lu Fault Zone (TLFZ) is the most important fault in eastern Asia and is still active currently. We have carried out extensive geothermal measurements in the south-central TLFZ: the heat flow in the southern TLFZ is concentrated in the range 55-65 mW/m〈sup〉2〈/sup〉; the highest heat flow site LZSD (93 mW/m〈sup〉2〈/sup〉) is determined by the high heat production rocks, so the southern TLFZ is not a thermal anomaly. In contrast, the heat flow value in the middle section of the TLFZ is over 80 mW/m〈sup〉2〈/sup〉, which is likely to be a thermal anomaly zone. Simulations and calculations show that the heat generated by the fault activity is not significant (1-6 mW/m〈sup〉2〈/sup〉). Detailed two-dimensional temperature field simulation work also confirms these conclusions. The differences in the present-day thermal state of the TLFZ are the result of differences in the influence of tectono-thermal events in different regions, with the "Craton destruction event" at the late Early Cretaceous having altered the property of lithosphere in East China (Lower Yangtze Craton and the north part of the eastern North China Craton), while the south part of the eastern has only undergone the lithospheric thinning process. The difference in paleo-lithosphere thickness is likely the main reason for the different thermal state of the TLFZ.
    Language: English
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  • 5
    Publication Date: 2023-06-06
    Description: Analyzing the spatiotemporal characteristics and evolution of meteorological and hydrological droughts can reproduce the process of drought propagation. This study focuses on drought propagation between meteorological and hydrological drought in Yunnan province, Southwest China, using Global Navigation Satellite Systems (GNSS) observations and precipitation data. We identify 7 meteorological and 7 hydrological droughts between January 2011 and May 2021 and find that the meteorological droughts are concentrated in northern Yunnan and last 1-11 months, while hydrological droughts are more severe and larger, lasting 2-16 months. The drought propagation time varies between 2-7 months and is short in the southwest but long in the northeast. We also find that water vapor, precipitation, and water storage have an uneven spatiotemporal distribution with the red river fault (RRF) as the boundary and that the RRF influences the spatial variation of water resources and drought propagation. The results of this study provide valuable insights into the spatiotemporal characteristics and evolution of meteorological and hydrological droughts, which can be used to improve water resources management and mitigate the impact of droughts.
    Language: English
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  • 6
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    In:  XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
    Publication Date: 2023-07-31
    Description: Radiative transfer models are widely applied in climate models to simulate vertical temperature perturbations caused by external radiative forcings. A large part of radiative transfer models is the infrared gaseous spectral transmittance scheme, which quantifies the longwave atmospheric absorption. A rapid infrared gaseous spectral transmittance scheme, called the optimized alternate mapping correlated K-distribution model (OMCKD), is introduced in this paper. To improve the accuracy of our scheme without increasing pseudo-monochromatic calculations, we introduce the optimal iteration method to automatically tune the equivalent absorption coefficients in the cumulative probability subspace. In addition, a new expression weighted by black-body radiation is introduced to calculate the equivalent absorption coefficient. The OMCKD simulates heating rate and radiation flux with errors of less than 0.12 K d-1 and 0.35 W m-2, respectively, below stratopause for standard atmospheric profiles. The OMCKD is also evaluated and compared with the rapid radiative transfer model for general circulation models (RRTMG) in realistic atmospheric profiles. We found that OMCKD can accurately produce heating rates and generally captures radiative forcings associated with large perturbations to the concentrations of main greenhouse gases. Furthermore, the number of pseudo-monochromatic calculations in OMCKD is 11.4% less than that in RRTMG, which indicates less computational cost.
    Language: English
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