Abstract
The article aims to test the sensitivity of high-resolution mesoscale atmospheric model to fairly reproduce atmospheric processes that were present during the Boothbay Harbor meteotsunami on 28 October 2008. The simulations were performed by the Weather and Research Forecasting (WRF) model at 1-km horizontal grid spacing by varying initial conditions (ICs) and lateral boundary conditions (LBCs), nesting strategy, simulation lead time and microphysics and convective parameterizations. It seems that the simulations that used higher-resolution IC and LBC were more successful in reproduction of precipitation zone and surface pressure oscillations caused by internal gravity waves observed during the event. The results were very sensitive to the simulation lead time and to the choice of convective parameterization, while the choice of microphysics parameterization and the type of nesting strategy (one-way or two-way) was less important for reproducibility of the event. The success of the WRF model appears limited to very short-range forecasting, most advanced parameterizations, and very high-resolution grid spacing; therefore, the applicability of present atmospheric mesoscale models to future operational meteotsunami warning systems still has a lot of room for improvements.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
Preview
Unable to display preview. Download preview PDF.
References
Belušić D, Strelec-Mahović N (2009) Detecting and following atmospheric disturbances with a potential to generate meteotsunamis in the Adriatic. Phys Chem Earth 34:918–927
Belušić D, Grisogono B, Klaić ZB (2007) Atmospheric origin of the devastating coupled air–sea event in the east Adriatic. J Geophys Res 112:D17111. doi:10.1029/2006JD008204
Chen F, Dudhia J (2001) Coupling an advanced land surface-hydrology model with the Penn State-NCAR MM5 modeling system. Part I: model implementation and sensitivity. Mon Weather Rev 129:569–585
Dudhia J (1989) Numerical study of convection observed during the winter monsoon experiment using a mesoscale two-dimensional model. J Atmos Sci 46:3077–3107
Ek MB, Mitchell KE, Lin Y, Rogers E, Grunmann P, Koren V, Gayno G, Tarpley JD (2003) Implementation of Noah land surface model advances in the National Centers for Environmental Prediction operational mesoscale Eta model. J Geophys Res 108(D22):8851. doi:10.1029/2002JD003296
Gilland EK, Rowe CM (2012) A comparison of cumulus parameterization schemes in the WRF model. In: 2012 AMS annual meeting, P2.16. https://ams.confex.com/ams/pdfpapers/120591.pdf
Hibiya T, Kajiura K (1982) Origin of the Abiki phenomenon (a kind of seiche) in Nagasaki Bay. J Oceanogr Soc Jpn 38:172–182
Janjić ZI (2001) Nonsingular implementation of the Mellor–Yamada Level 2.5 scheme in the NCEP meso model. NCEP office note no. 437
Jansà A, Monserrat S, Gomis D (2007) The rissaga of 15 June 2006 in Ciutadella (Menorca), a meteorological tsunami. Adv Geosci 12:1–4
Laprise R (1992) The Euler equations of motion with hydrostatic-pressure as an independent variable. Mon Weather Rev 120:197–208
Mapes BE (1997) Equilibrium vs. activation control of large-scale variations of tropical deep convection. In: Smith RK (ed) The physics and parametrization of moist atmospheric convection. Kluwer, Dordrecht, pp 321–358
Mellor GL, Yamada T (1974) Hierarchy of turbulent closure models for planetary boundary-layers. J Atmos Sci 31:1791–1806
Mellor GL, Yamada T (1982) Development of a turbulent closure-model for geophysical fluid problems. Rev Geophys 20:851–875
Mlawer EJ, Taubman SJ, Brown PD, Iacono MJ, Clough SA (1997) Radiative transfer for inhomogeneous atmospheres: RRTM, a validated correlated-k model for the longwave. J Geophys Res 102:16663–16682. doi:10.1029/97JD00237
Monserrat S, Ramis C, Thorpe AJ (1991) Large-amplitude pressure oscillations in the Western Mediterranean. Geophys Res Lett 18:183–186
Monserrat S, Vilibić I, Rabinovich AB (2006) Meteotsunamis: atmospherically induced destructive ocean waves in the tsunami frequency band. Nat Hazards Earth Syst Sci 6:1035–1051
Morrison H, Thompson G, Tatarskii V (2009) Impact of Cloud microphysics on the development of trailing stratiform precipitation in a simulated squall line: comparison of one- and two-moment schemes. Mon Weather Rev 137:991–1007
Orlić M (1980) About a possible occurrence of the Proudman resonance in the Adriatic. Thalassia Jugoslavica 16(1):79–88
Proudman J (1929) The effects on the sea of changes in atmospheric pressure. Geophys Suppl Mon Notices R Astron Soc 2(4):197–209
Rabinovich AB (2009) Seiches and harbour oscillations. In: Kim YC (ed) Handbook of coastal and ocean engineering. World Scientific, Singapore, pp 193–236
Renault L, Vizoso G, Jansá A, Wilkin J, Tintoré J (2011) Toward the predictability of meteotsunamis in the Balearic Sea using regional nested atmosphere and ocean models. Geophys Res Lett 38:L10601. doi:10.1029/2011GL047361
Schroeder G, Schlünzen KH (2009) Numerical dispersion of gravity waves. Mon Weather Rev 137:4344–4354
Šepić J, Vilibić I (2011) The development and implementation of a real-time meteotsunami warning network for the Adriatic Sea. Nat Hazards Earth Syst Sci 11:83–91
Šepić J, Vilibić I, Belušić D (2009) The source of the 2007 Ist meteotsunami (Adriatic Sea). J Geophys Res 114:C03016. doi:10.1029/2008JC005092
Šepić J, Vilibić I, Strelec Mahović N (2012) Northern Adriatic meteorological tsunamis: observations, link to the atmosphere, and predictability. J Geophys Res 117:C02002. doi:10.1029/2011JC007608
Skamarock WC (2004) Evaluating mesoscale NWP models using kinetic energy spectra. Mon Weather Rev 132:3019–3032
Skamarock WC, Klemp JB (2008) A time-split nonhydrostatic atmospheric model for weather research and forecasting applications. J Comput Phys 227:3465–3485
Stensrud DJ (2007) Parametrization schemes: keys to understanding numerical weather prediction models. Cambridge University Press, Cambridge
Tanaka K (2010) Atmospheric pressure-wave bands around a cold front resulted in a meteotsunami in the East China Sea in February 2009. Nat Hazards Earth Syst Sci 10:2599–2610
Vilibić I (2008) Numerical simulations of the Proudman resonance. Cont Shelf Res 28:574–581
Vilibić I, Horvath K, Strelec Mahović N, Monserrat S, Marcos M, Amores Á, Fine I (2014) Atmospheric processes responsible for generation of the 2008 Boothbay meteotsunami. Nat Hazards. doi:10.1007/s11069-013-0811-y. http://link.springer.com/article/10.1007%2Fs11069-013-0811-y
Acknowledgments
We would like to thank NOAA and the Gulf of Maine Research Institute, in particular John Jensenius and Linda Mangum, who provided us with the data observed at GoMOOS/NERACOOS buoys during the event (http://neracoos.org). Croatian Meteorological and Hydrological Service accounted for the provision of computational resources for numerical simulations. This work was performed within the NOAA/NWS project “Towards a meteotsunami warning system along the US coastline (TMEWS)”, Award No. NA11NWS4670005. We are grateful to two anonymous reviewers for comments and suggestions that improved the manuscript.
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2014 Springer Science+Business Media Dordrecht
About this chapter
Cite this chapter
Horvath, K., Vilibić, I. (2014). Atmospheric mesoscale conditions during the Boothbay meteotsunami: a numerical sensitivity study using a high-resolution mesoscale model. In: Vilibić, I., Monserrat, S., Rabinovich, A.B. (eds) Meteorological Tsunamis: The U.S. East Coast and Other Coastal Regions. Springer, Cham. https://doi.org/10.1007/978-3-319-12712-5_4
Download citation
DOI: https://doi.org/10.1007/978-3-319-12712-5_4
Received:
Accepted:
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-319-12711-8
Online ISBN: 978-3-319-12712-5
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)