Articles | Volume 14, issue 1
Geosci. Model Dev., 14, 91–106, 2021
https://doi.org/10.5194/gmd-14-91-2021
Geosci. Model Dev., 14, 91–106, 2021
https://doi.org/10.5194/gmd-14-91-2021

Model description paper 07 Jan 2021

Model description paper | 07 Jan 2021

An N-dimensional Fortran interpolation programme (NterGeo.v2020a) for geophysics sciences – application to a back-trajectory programme (Backplumes.v2020r1) using CHIMERE or WRF outputs

Bertrand Bessagnet et al.

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Cited articles

Bessagnet, B.: A N-dimensional Fortran Interpolation Program (NterGeo) for Geophysics Sciences (Version 2020v1), Zenodo, https://doi.org/10.5281/zenodo.3733278, 2020. a
Donner, L. J., Wyman, B. L., Hemler, R. S., Horowitz, L. W., Ming, Y., Zhao, M., Golaz, J.-C., Ginoux, P., Lin, S.-J., Schwarzkopf, M. D., Austin, J., Alaka, G., Cooke, W. F., Delworth, T. L., Freidenreich, S. M., Gordon, C. T., Griffies, S. M., Held, I. M., Hurlin, W. J., Klein, S. A., Knutson, T. R., Langenhorst, A. R., Lee, H.-C., Lin, Y., Magi, B. I., Malyshev, S. L., Milly, P. C. D., Naik, V., Nath, M. J., Pincus, R., Ploshay, J. J., Ramaswamy, V., Seman, C. J., Shevliakova, E., Sirutis, J. J., Stern, W. F., Stouffer, R. J., Wilson, R. J., Winton, M., Wittenberg, A. T., and Zeng, F.: The Dynamical Core, Physical Parameterizations, and Basic Simulation Characteristics of the Atmospheric Component AM3 of the GFDL Global Coupled Model CM3, J. Climate, 24, 3484–3519, https://doi.org/10.1175/2011JCLI3955.1, 2011. a
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Hardy, R.: Theory and applications of the multiquadric-biharmonic method 20 years of discovery 1968–1988, Computers and Mathematics with Applications, 19, 163–208, https://doi.org/10.1016/0898-1221(90)90272-L, 1990. a
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Short summary
This paper presents a new interpolator useful for geophysics applications. It can explore N-dimensional meshes, grids or look-up tables. The code accepts irregular but structured grids. Written in Fortran, it is easy to implement in existing codes and very fast and portable. We have compared it with a Python library. Python is convenient but suffers from portability and is sometimes not optimized enough. As an application case, this method is applied to atmospheric sciences.