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91.
The Sardinia Radio Telescope (SRT) is a challeging scientific project managed by the National Institute for Astrophysics (INAF),
it is being developed at 30 km North of the city of Cagliari, Italy. The goal of the SRT project is to build a general purpose,
fully steerable, 64 m diameter radio telescope, capable of operating with high efficiency in the centimeter and millimeter
frequency range (0.3–100 GHz). In portions of this frequency range, especially towards the high end, astronomical observations
can be heavily deteriorated by non-optimal atmospheric conditions, especially by water vapor content. The water molecule permanent
electric dipole in fact, leads to pressure broadened rotational transitions around the 22.23 GHz spectral line. Furthermore,
water vapor’s continuum absorption and emission may influence higher frequency observations too. To a lower degree, cloud
liquid black body radiation can also affect centimeter and millimeter observations. In addition to this, inhomogeneities in
water vapor distributions can cause signal phase errors which introduce a great amount of uncertainty to VLBI mode observations.
The Astronomical Observatory of Cagliari (OA-CA) has obtained historical timeseries of radiosonde profiles conducted at the
airport of Cagliari. Through the radiosonde measurements and an appropriate radiative transfer model, we have performed a
statistical analysis of the SRT site’s atmosphere which accounts for atmospheric opacity at different frequencies, integrated
water vapor (IWV), integrated liquid water (ILW) and cloud cover distributions during the year. This will help to investigate
in which period of the year astronomical observations at different frequencies should be performed preferably. The results
show that, at the SRT site, K-band astronomical observations are possible all year round, the median opacity at 22.23 GHz
is 0.10 Np in the winter (Dec-Jan-Feb) and 0.16 Np in the summer (Jun-Jul-Aug). Integrated water vapor during winter months
ranges, on average, between 7 and 15 mm. Cloud cover is usually not present for more than 36% of the time during the year.
The atmospheric opacity study indicates that observations at higher frequencies (50–100 GHz) may be performed usefully: the
median opacity at 100 GHz is usually below or equal to 0.2 Np in the period that ranges from January to April. 相似文献
92.
Alec Thornton Tony Binns Maria Talaitupu Kerslake 《Singapore journal of tropical geography》2013,34(3):357-372
This paper presents findings from a study about the relationships between social change and settlement change in Samoa, where a form of landlessness is emerging in low income areas of the main town, Apia. It examines changing reciprocal kinship arrangements with respect to customary rural village plantation land and changes in both individual and household relationships with the church. Although these relationships are typically closely bound in Pacific island societies, recent field‐based research has revealed the expansion of landless urban settlements with households that are alienated from rural village‐based kin and, by extension, customary land. 相似文献
93.
94.
The concept of vulnerability is increasingly important in engineering and the socio-economic planning sciences, particularly given the enormous costs associated with addressing it. The ability to identify and mitigate vulnerabilities is extremely challenging because it is influenced by a complex and dynamic set of interacting factors that can compromise social, economic and infrastructure systems. Where the latter is concerned, the ability to assess infrastructure vulnerability involves the consideration of a range of physical, operational, geographical and socio-economic characteristics. In this paper, significant elements of infrastructure vulnerability are identified and discussed with a focus on their intrinsic spatial nature and their propensity to interact across space. Further, the developed typology of vulnerability outlined in this paper emphasizes the need to ensure that policy, planning and disaster mitigation efforts are strongly integrated at global, regional and local levels. 相似文献
95.
This special issue of GeoJournal is centered on geographic approaches to vulnerability analysis. Six papers addressing several core areas of active research in vulnerability analysis are included in this volume of work. In particular, network analysis methods, geographic data acquisition and use, measurement of vulnerability, evaluation of spatial and temporal variability in vulnerability, as well as related theoretical and policy issues are examined in detail. 相似文献
96.
97.
Hydrodynamic, suspension and bed-form measurements were made 2 km off the Dutch coast near Noordwijk aan Zee in ∼14 m water depth for a period of 32 days in 2003. Tidal currents were just able to suspend sand at the bed at peak spring tide but most suspension and transport occurred as a result of the combination of waves and currents. Burst-average (17 min) sand concentration profiles (C¯-profiles) from an acoustic backscatter instrument were used to define the (varying) location of the sea-bed, following the method used by Green et al. [Green, M.O., Dolphin, T.J., Swales, A., Vincent, C.E., 1999. Transport of mixed-size sediments in a tidal channel. Coastal Sediments ‘99, edited by N.C. Kraus, and W.G. McDougal, ASCE, Long Island, New York, pp. 644–658]. Reference concentrations at the sea-bed (C0) and at 1 cm (C1) were examined in relation to both the hydrodynamic conditions and the type of bed forms present. The C0 predictive equations of Green and Black [Green, M.O., Black, K.P., Suspended sediment reference concentration under waves: field measurements and critical analysis of two predictive models, Coastal Engineering, 38, 115–141, 1999](short-wave ripples) and Nielsen [Nielsen, P., Suspended sediment concentrations under waves, Coastal Engineering, 10, 23–31, 1986](all bed forms; includes ripple steepness), both of which require knowledge of the bed-form type, were not as successful in explaining the variance in our C0 data as a regression of C0 against the skin-friction Shields parameter θ′cw that ignored bed-form type (73% of variance explained). The values of the reference concentration C1 were compared with the Lee et al. [Lee, G.-H., Dade, W.B., Friedrichs, C.T., Vincent, C.E., Examination of Reference Concentration Under Waves and Currents on the Inner Shelf., Journal of Geophysical Research, 109, 1–10, 2004] equation which predicts C1 from the product of the Shields parameter and the inverse Rouse parameter; 51% of the variance in C1 was explained. 相似文献
98.
Richard J. Bathurst Tony M. Allen Yoshihisa Miyata Sina Javankhoshdel Nezam Bozorgzadeh 《Georisk: Assessment and Management of Risk for Engineered Systems and Geohazards》2019,13(3):214-225
ABSTRACTMechanically stabilized earth (MSE) walls must be designed with adequate margins of safety against internal stability failure described by tensile strength and pullout limit states. Probabilities of failure (or reliability index) will vary strongly with the accuracy of the underlying models that appear in limit state performance functions. In this paper, prior work by the authors and co-workers on this topic is reviewed. Relative performance is explored in the context of the reliability (or probability of failure) of steel and polymeric reinforcing elements in MSE walls using limit state performance functions with load and resistance models having different accuracy. 相似文献
99.
Omar A. Alharbi Michael R. Phillips Allan T. Williams Tony Thomas Mohammed Hakami Jehad Kerbe Abdoul Jelil Niang ElSayed Hermas Khalid Al-Ghamdi 《Arabian Journal of Geosciences》2017,10(16):360
Jizan is one of the Saudi Arabian coastal cities endowed with diverse natural settings, which includes Ash Shuqayq in the north, Turfah in the centre and Jizan in the South. This work analysed specific environmental characteristics, such as spits, sabkhas and wadis. Assessments used Landsat imagery to examine coastal change between 1973 and 2011. The cumulative temporal change identified regression trends given by coefficients of determination that explained a significant percentage of data variation for Jizan (R 2 = 69%) and Turfah (R 2 = 72%), while Ash Shuqayq was insignificant (R 2 = 14%). Inter-survey results predicted future change, although trends were not significant, i.e. Jizan (R 2 = 22%), Turfah (R 2 = 14%) and Ash Shuqayq (R 2 = 3 and 61% with outlying value removed). Aerial photos showed regional coastal changes, which included a maximum accretion of 36.4 m and maximum erosion of 12.9 m. These are scientifically effective techniques to monitor regional coastal change, i.e. erosion and accretion and identified rates of 0.59, 1.80 and 3.53 myr?1 for Ash Shuqayq, Turfah and Jizan. Changes were linked to infrastructure developments, e.g. tourism, port development and natural causes, e.g. spit formations and wadi outfalls. 相似文献
100.