scholarly journals Global Transmission of COVID-19 for Classifications of Community-Acquired Outbreaks: Machine Learning and Statistical Model Analysis

Author(s):  
Wei-Chun Wang ◽  
Ting-Yu Lin ◽  
Sherry Yueh-Hsia Chiu ◽  
Chiung-Nien Chen ◽  
Pongdech Sarakarn ◽  
...  
2007 ◽  
Vol 16 (07n08) ◽  
pp. 1783-1789 ◽  
Author(s):  
GIORGIO TORRIERI

We briefly describe two statistical hadronization models, based respectively on the presence and absence of light quark chemical equilibrium, used to analyze particle yields in heavy ion collisions. We then try to distinguish between these models using K/π fluctuations data. We find that while the non-equilibrium model provides an acceptable description of fluctuations at top SPS and RHIC energies, both models considerably under-estimate fluctuations at low SPS energies.


2007 ◽  
Vol 33 (2) ◽  
pp. 214-225 ◽  
Author(s):  
B. V. Robouch ◽  
A. Marcelli ◽  
M. Cestelli Guidi ◽  
A. Kisiel ◽  
E. M. Sheregii ◽  
...  

2016 ◽  
Vol 109 ◽  
pp. 05004
Author(s):  
G. Khuukhenkhuu ◽  
M. Odsuren ◽  
Y. M. Gledenov ◽  
G. H. Zhang ◽  
M. V. Sedysheva ◽  
...  

2017 ◽  
Author(s):  
Yuanqiao Wu ◽  
Ed Chan ◽  
Joe R. Melton ◽  
Diana L. Verseghy

Abstract. Peatlands store large amounts of soil carbon and constitute an important component of the global carbon cycle. Accurate information on the global extent and distribution of peatlands is presently lacking but it important for earth system models (ESMs) to be able to simulate the effects of climate change on the global carbon balance. The most comprehensive peatland map produced to date is a qualitative presence/absence product. Here, we present a spatially continuous global map of peatland fractional coverage using the extremely randomized tree machine learning method suitable for use as a prescribed geophysical field in an ESM. Inputs to our statistical model include spatially distributed climate data, soil data and topographical slopes. Available maps of peatland fractional coverage for Canada and West Siberia were used along with a proxy for non-peatland areas to train and test the statistical model. Regions where the peatland fraction is expected to be zero were estimated from a map of topsoil organic carbon content below a threshold value of 13 kg/m2. The modelled coverage of peatlands yields a root mean square error of 4 % and a coefficient of determination of 0.91 for the 10,978 tested 0.5 degree grid cells. We then generated a complete global peatland fractional coverage map. In comparison with earlier qualitative estimates, our global modelled peatland map is able to reproduce peatland distributions in places remote from the training areas and capture peatland hot spots in both boreal and tropical regions, as well as in the southern hemisphere. Additionally we demonstrate that our machine-learning method has greater skill than solely setting peatland areas based on histosols from a soil database.


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