scholarly journals Transition of meteorological variables while downburst occurrence by a high density ground surface observation network

2019 ◽  
Vol 184 ◽  
pp. 153-161 ◽  
Author(s):  
Hisato Iwashita ◽  
Fumiaki Kobayashi
2020 ◽  
Vol 38 (2) ◽  
pp. 53-66
Author(s):  
Hisato Iwashita ◽  
Toshiaki Morita ◽  
Koji Shibata ◽  
Fumiaki Kobayashi

2019 ◽  
Vol 38 (1) ◽  
pp. 23-35 ◽  
Author(s):  
Hisato Iwashita ◽  
Toshiaki Morita ◽  
Koji Shibata ◽  
Fumiaki Kobayashi

2019 ◽  
Vol 12 (11) ◽  
pp. 4661-4679 ◽  
Author(s):  
Bin Cao ◽  
Xiaojing Quan ◽  
Nicholas Brown ◽  
Emilie Stewart-Jones ◽  
Stephan Gruber

Abstract. Simulations of land-surface processes and phenomena often require driving time series of meteorological variables. Corresponding observations, however, are unavailable in most locations, even more so, when considering the duration, continuity and data quality required. Atmospheric reanalyses provide global coverage of relevant meteorological variables, but their use is largely restricted to grid-based studies. This is because technical challenges limit the ease with which reanalysis data can be applied to models at the site scale. We present the software toolkit GlobSim, which automates the downloading, interpolation and scaling of different reanalyses – currently ERA5, ERA-Interim, JRA-55 and MERRA-2 – to produce meteorological time series for user-defined point locations. The resulting data have consistent structure and units to efficiently support ensemble simulation. The utility of GlobSim is demonstrated using an application in permafrost research. We perform ensemble simulations of ground-surface temperature for 10 terrain types in a remote tundra area in northern Canada and compare the results with observations. Simulation results reproduced seasonal cycles and variation between terrain types well, demonstrating that GlobSim can support efficient land-surface simulations. Ensemble means often yielded better accuracy than individual simulations and ensemble ranges additionally provide indications of uncertainty arising from uncertain input. By improving the usability of reanalyses for research requiring time series of climate variables for point locations, GlobSim can enable a wide range of simulation studies and model evaluations that previously were impeded by technical hurdles in obtaining suitable data.


2019 ◽  
Author(s):  
Bin Cao ◽  
Xiaojing Quan ◽  
Nicholas Brown ◽  
Emilie Stewart-Jones ◽  
Stephan Gruber

Abstract. Simulations of land-surface processes and phenomena often require driving time series of meteorological variables. Corresponding observations, however, are unavailable in most locations, even more so, when considering the duration, continuity and data quality required. Atmospheric reanalyses provide global coverage of relevant meteorological variables, but their use is largely restricted to grid-based studies. This is because technical challenges limit the ease with which reanalysis data can be applied to models at the site scale. We present the software toolkit GlobSim, which automates the downloading, interpolation and scaling of different reanalyses – currently ERA-5, ERA-Interim, JRA-55 and MERRA-2 – to produce meteorological time series for user-defined point locations. The resulting data have consistent structure and units to efficiently support ensemble simulation. The utility of GlobSim is demonstrated using an application in permafrost research. We perform ensemble simulations of ground-surface temperature for ten terrain types in a remote tundra area in northern Canada and compare the results with observations. Simulation results reproduced seasonal cycles and variation between terrain types well, demonstrating that GlobSim can support efficient land-surface simulations. Ensemble means often yielded better accuracy than individual simulation and ensemble ranges additionally provide indications of uncertainty arising from uncertain input. By improving the usability of reanalyses for research requiring time-series of climate variables for point locations, GlobSim can enable a wide range of simulation studies and model evaluations that previously were impeded by technical hurdles in obtaining suitable data.


2004 ◽  
Vol 13 (2) ◽  
pp. 109-121 ◽  
Author(s):  
Christian Häberli ◽  
Inga Groehn ◽  
Reinhold Steinacker ◽  
Wolfgang Pöttschacher ◽  
Manfred Dorninger

2011 ◽  
Vol 261-263 ◽  
pp. 1379-1385
Author(s):  
Chang Hong Li ◽  
Yan Cheng ◽  
Lei Zhang

According to the study of electrical properties of geological bodies crust, different instruments electric field is measured through the case, then the distribution of the electric field is studied in order to understand the situation of deep underground geological principles. The unknown bodies underground, cave, mined-out areas, ground water detection of two typical survey lines are detected with AGI high-density resistivity measurement system, which the three selected acquisition mode are selected, the sectional drawing of two-dimensional inversion is obtained by data collected processing; the coupling analysis is detected in exploration information and strata Information according to the corresponding geological profile, both high resistance and low resistivity anomalies of the underground and the character of the corresponding space area are accessed; the possibility and ease of the ground surface collapse of different anomalies is pointed out according to the surface geological information and the situation of surface subsidence.


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