Numerical study of the spatial distribution of the M2 internal tide in the Pacific Ocean

By Yoshihiro Niwa, T. Hibiya. 2001

221 citations recorded by the source corpus.

Subfields: Atmospheric Science, Geology, Oceanography

View Paper: https://www.semanticscholar.org/paper/25531fc3e2e9c9fb64e8e0f658372c292ea86e12

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. K. Polzin
2. Y. Lvov
3. J. MacKinnon
4. J. Klymak
5. R. Pinkel
6. Robert Hallberg
7. M. Alford
8. G. Carter

In Geology

1. K. Polzin
2. Y. Lvov
3. Jonas Nycander

In Oceanography

1. S. Jayne
2. J. MacKinnon
3. Jonas Nycander
4. K. Polzin
5. Raffaele Ferrari
6. Y. Lvov
7. Sonya Legg
8. J. Klymak

Citations in the corpus

• Sensitivity of the Ocean State to the Vertical Distribution of Internal-Tide-Driven Mixing (2013, background): “…topography in the stratified ocean, leading to, respectively, the generation of internal lee waves (e.g., Nikurashin and Ferrari 2011) and baroclinic tides (internal waves at the tidal frequency, also called internal tides, e.g., Egbert and Ray 2000; Niwa and Hibiya 2001; Garrett and Kunze 2007).”
• Generation of internal waves in the deep ocean by tides (2005, background): “[6] Niwa and Hibiya [2001] have simulated the M2 tide in the Pacific with a three-dimensional primitive equation model with a horizontal resolution of 1/16� , averaging depth data within a radius of 10 km at each grid point.”
• Internal waves across the Pacific (2007, background): “…be generated both at the surface by surface wind forcing and below the surface by extracting energy from the internal tide through parametric subharmonic instability (PSI) [Niwa and Hibiya, 2001; Nagasawa et al., 2002; Hibiya and Nagasawa, 2004; Rainville and Pinkel, 2006; Carter and Gregg, 2006].”
• Model-predicted distribution of wind-induced internal wave energy in the world's oceans (2008, unknown): “[3] The global energy conversion rate from the surface to internal tide was estimated to be $0.9 TW on the basis of the altimetric observations [Egbert and Ray, 2000] and numerical experiments [Niwa and Hibiya, 2001; Simmons et al., 2004].”
• Energetics of M2 Barotropic-to-Baroclinic Tidal Conversion at the Hawaiian Islands (2008, methodology): “, Holloway and Merrifield 1999; Johnston and Merrifield 2003) and realistic (e.g., Cummins and Oey 1997; Merrifield et al. 2001; Niwa and Hibiya 2001; Merrifield and Holloway 2002; Johnston et al. 2003) topography.”
• TOWARD REGIONAL CHARACTERIZATIONS OF THE OCEANIC INTERNAL WAVEFIELD (2010, methodology): “[1982, 1984] tackle this starting from the Lagrangian of Olbers [1976] and carrying forward their calculations in the context of the direct interaction approximation (DIA).”
• Tidally driven mixing in a numerical model of the ocean general circulation (2003, unknown): “Previously, the global distribution of energy flux into the internal tides has been examined using observations and tidal models (Egbert and Ray, 2000, 2001; Jayne and St. Laurent, 2001; Niwa and Hibiya, 2001).”
• The accuracy of surface elevations in forward global barotropic and baroclinic tide models (2004, background): “…Holloway (1996), Cummins and Oey (1997), Kantha and Tierney (1997), Holloway and Merrifield (1999), Kang et al. (2000), Merrifield et al. (2001), Niwa and Hibiya (2001), Balmforth et al. (2002), St. Laurent and Garrett (2002), Llewellyn Smith and Young (2002, 2003), Khatiwala (2003), St.…”
• Propagation of Low-Mode Internal Waves through the Ocean (2006, background): “Low-mode internal tides rapidly fill the ocean interior in barotropically forced numerical models (Niwa and Hibiya 2001; Simmons et al. 2004).”