Non-Negative Filter Using Arcsine Transformation for Tracer Advection with Semi-Lagrangian Scheme
Author:
Affiliation:
1. Institute of Space and Astronautical Science
2. Disaster Prevention Research Institute, Kyoto University
3. Center for Planetary Science, Kobe University
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/sola/9/0/9_2013-028/_pdf
Reference16 articles.
1. Bermejo, B., and A. Staniforth, 1992: The conversion of semi-Lagrangian advection schemes to quasi-monotone schemes. Mon. Wea. Rev., 120, 2622-2632.
2. Enomoto, T., 2008: Bicubic interpolation with spectral derivatives. SOLA, 4, 5-8.
3. Laprise, R., 1988: Representation of water vapour in a spectral GCM. Research activities in atmospheric and oceanic modelling, CAS/JSC Working Group on Numerical Experimentation, 11, 3.18-3.21.
4. Mahlman, J. D., and W. J. Moxim, 1978: Tracer simulation using a global general circulation model: results from a midlatitude instantaneous source experiment. J. Atmos. Sci., 35, 1340-1374.
5. Moorthi, S., 1997: NWP experiments with a gridpoint semi-Lagrangian semi-implicit global model at NCEP. Mon. Wea. Rev., 125, 74-98.
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