메뉴 건너뛰기




Volumn 136, Issue 647, 2010, Pages 497-506

Treatment of vector equations in deep-atmosphere, semi-lagrangian models. I: Momentum equation

Author keywords

Non euclidean effects; Orthogonal curvilinear systems; Rotation matrix; Shallow atmosphere approximation; Spheroidal coordinates

Indexed keywords

ATMOSPHERE MODELS; EULERIAN; EXPLICIT FORM; GREAT CIRCLE; IDENTITY MATRICES; MERIDIONAL PLANES; MOMENTUM EQUATION; NON-EUCLIDEAN; ROTATION MATRICES; SEMI-LAGRANGIAN; SEMI-LAGRANGIAN METHODS; SEMI-LAGRANGIAN MODELS; SPHERICAL COORDINATES; SPHEROIDAL COORDINATES; TIME STEP; UNIT VECTORS; VECTOR COMPONENTS; VECTOR EQUATION; VECTOR MOMENTUM EQUATION;

EID: 77949390977     PISSN: 00359009     EISSN: 1477870X     Source Type: Journal    
DOI: 10.1002/qj.562     Document Type: Article
Times cited : (16)

References (22)
  • 3
    • 0025591039 scopus 로고
    • Integration of the shallow- water equations on the sphere using a vector semi-Lagrangian scheme with a multigrid solver
    • Bates JR, Semazzi FHM, Higgins RW. 1990. Integration of the shallow- water equations on the sphere using a vector semi-Lagrangian scheme with a multigrid solver. Mon. Weather Rev. 118: 1615-1627.
    • (1990) Mon. Weather Rev , vol.118 , pp. 1615-1627
    • Bates, J.R.1    Semazzi, F.H.M.2    Higgins, R.W.3
  • 4
    • 0000397713 scopus 로고
    • A Lagrange multiplierapproach for the metrictermsof semi-Lagrangian models on the sphere
    • Côté J. 1988. A Lagrange multiplierapproach for the metrictermsof semi-Lagrangian models on the sphere. Q. J. R. Meteorol. Soc. 114: 1347-1352.
    • (1988) Q. J. R. Meteorol. Soc , vol.114 , pp. 1347-1352
    • Côté, J.1
  • 6
    • 8744240174 scopus 로고    scopus 로고
    • Derivation of the equations of atmospheric motion in oblate spheroidal coordinates
    • Gates WL. 2004. Derivation of the equations of atmospheric motion in oblate spheroidal coordinates. J. Atmos. Sci. 61: 2478-2487.
    • (2004) J. Atmos. Sci , vol.61 , pp. 2478-2487
    • Gates, W.L.1
  • 7
    • 0003437218 scopus 로고
    • Addison-Wesley: Palo Alto, California, USA
    • Goldstein H. 1950. Classical mechanics. Addison-Wesley: Palo Alto, California, USA.
    • (1950) Classical Mechanics
    • Goldstein, H.1
  • 11
    • 5244262503 scopus 로고
    • Angular-momentum budget of shallow waters on a rotating sphere
    • Müller D. 1992. Angular-momentum budget of shallow waters on a rotating sphere. Phys. Rev. A 45: 5545-5555.
    • (1992) Phys. Rev. A , vol.45 , pp. 5545-5555
    • Müller, D.1
  • 12
    • 77949382123 scopus 로고    scopus 로고
    • MüllerP, CambridgeUniversity Press: Cambridge, UK
    • MüllerP.2006.Theequationsofoceanicmotions.CambridgeUniversity Press: Cambridge, UK.
    • (2006) Theequationsofoceanicmotions
  • 14
    • 0000050506 scopus 로고
    • Application of the semi-Lagrangian method to a spectral model of the shallow-water equations
    • Ritchie H. 1988. Application of the semi-Lagrangian method to a spectral model of the shallow-water equations. Mon. Weather Rev. 122: 366-376.
    • (1988) Mon. Weather Rev , vol.122 , pp. 366-376
    • Ritchie, H.1
  • 15
    • 0028578362 scopus 로고
    • Spurious resonant response of semi-Lagrangian discretizations to orographic forcing: Diagnosis and solution
    • Rivest C, Staniforth A, Robert A. 1994. Spurious resonant response of semi-Lagrangian discretizations to orographic forcing: Diagnosis and solution. Mon. Weather Rev. 122: 366-376.
    • (1994) Mon. Weather Rev , vol.122 , pp. 366-376
    • Rivest, C.1    Staniforth, A.2    Robert, A.3
  • 16
    • 0026291228 scopus 로고
    • Semi-Lagrangian integration schemes for atmospheric models - A review
    • Staniforth A, Côté J. 1991. Semi-Lagrangian integration schemes for atmospheric models - A review. Mon. Weather Rev. 119: 2206-2223.
    • (1991) Mon. Weather Rev , vol.119 , pp. 2206-2223
    • Staniforth, A.1    Côté, J.2
  • 18
    • 0028973721 scopus 로고
    • Dynamically consistent, quasi-hydrostatic equations for global models with a complete representation of the Coriolis force
    • White AA, Bromley RA. 1995. Dynamically consistent, quasi-hydrostatic equations for global models with a complete representation of the Coriolis force. Q. J. R. Meteorol. Soc. 121: 399-418.
    • (1995) Q. J. R. Meteorol. Soc , vol.121 , pp. 399-418
    • White, A.A.1    Bromley, R.A.2
  • 19
    • 27644541433 scopus 로고    scopus 로고
    • Consistent approximate models of the global atmosphere: Shallow, deep, hydrostatic, quasi-hydrostatic and non-hydrostatic
    • White AA, Hoskins BJ, Roulstone I, Staniforth A. 2005. Consistent approximate models of the global atmosphere: Shallow, deep, hydrostatic, quasi-hydrostatic and non-hydrostatic. Q. J. R. Meteorol. Soc. 131: 2081-2107.
    • (2005) Q. J. R. Meteorol. Soc , vol.131 , pp. 2081-2107
    • White, A.A.1    Hoskins, B.J.2    Roulstone, I.3    Staniforth, A.4
  • 20
    • 41949088988 scopus 로고    scopus 로고
    • Spheroidal coordinate systems formodellingglobalatmospheres
    • White AA, Staniforth A, Wood N. 2008. Spheroidal coordinate systems formodellingglobalatmospheres.Q.J.R.Meteorol.Soc.134:261-270.
    • (2008) Q.j.r.meteorol.soc , vol.134 , pp. 261-270
    • White, A.A.1    Staniforth, A.2    Wood, N.3
  • 21
    • 77949387084 scopus 로고    scopus 로고
    • Treatmentofvectorequationsin deep-atmosphere, semi-Lagrangian models. II: Kinematic equation
    • in press. DOI:10.1002/qj.565
    • Wood N, White AA, Staniforth A. 2009. Treatmentofvectorequationsin deep-atmosphere, semi-Lagrangian models. II: Kinematic equation. Q. J. R. Meteorol. Soc. in press. DOI:10.1002/qj.565.
    • (2009) Q. J. R. Meteorol. Soc
    • Wood, N.1    White, A.A.2    Staniforth, A.3


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.