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m, 189-195.
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Rev. de Geojisica, 39.2, 151-164.
Hernandez E, Pacheco J, Garcia R (1983b) Inclusi6n de la liberaci6n de calor latente en las
ecuaciones de un modelo de predicci6n, Communication to the V Asamblea Nacional de
Geojisica y Geodesia, Madrid.
Herring J, Hobbs P (1994) Radiatively driven dynamics of the plume from Kuwait 1991 oil
fires, 1. Geophys. Res., 99 D9, 18809-18826.
Hughes T, Weaver A (1994) Multiple equilibria of an asymmetric two-basin ocean model, 1.
Phys. Ocean., 24-3, 619-637.
Lions J L (1991) "ElplanetaTierra", Espasa Calpe, Madrid.
Liu Z, Pedlosky J (1994) Thermocline forced by annual and decadal surface temperature
variation, 1. Phys. Ocean., 24-3, 587-608.
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Lorenz E (1969) The predictability of a flow which possesses many scales of motion, Tellus,
16(1),289-307.
Lorenz E (1986) On the existence of a slow manifold, 1. Atmos. Sci., 43(15), 1547-1557.
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time solutions, 1. Geophys. Res., 99 D2, 3643-3654.
Nagai T et al. (1992) El Nino-Southern Oscillation simulated in an MRI atmosphere-ocean
coupled general circulation model, 1. of Climate, 5-11, 1202-1233.
Nicolis C (1990) Chaotic dynamics, Markov processes and climate predictability, Tellus 42A,
401-412.
Pedlosky J (1987) Geophysicaljluid dynamics, Springer Verlag, Berlin.
Pelegri J L et al. (1995) These Proceedings.
Pereira C, Mascarenhas A (1994) Numerical simulation of an oceanic front response to an
atmospheric frontal passage, 1. Geophys. Res., 99 C8, 16081-16094.
Sancho P et al. (1992) A five-year climatology of back-trajectories from the Izafia baseline
station, Tenerife, Canary Islands, Almos. Envir., 26 A6, 1081-1096.
Schutz L (1979) Sahara dust transport over the North Atlantic Ocean: Model calculations and
meaurements, in Morales C (ed.) Saharan dust: Mobilization, transport, deposition
(267-278),1. Wiley & Son, New York.
Sellers W (1969) A global climate model based on the energy balance of the earth-atmosphere
system, 1. Appl. Met., 8, 392-400.
Short K (1993) Direct calculation of metric entropy from time series, 1. Comput. Phys., 104,
162-172.
Stephens G et al. (1993) The Earth's radiation budget and its relation to atmospheric hidrology,
1. Geophys. Res., 98 D3, 4931-4950.
Temam R (1995) These Proceedings.
Vannitsem S, Nicolis C (1994) Predictability experiments on a simplified thermal convection
model: The role of spatial scales,J. Geophys. Res., 99 D9, 10377-10386.
Watts R et aI. (1994) Timescales in energy balance climate models 1: The limiting case
solutions, 1. Geophys. Res., 99 D2, 3631-3642.
Weaver A, Hughes T (1994) Rapid interglacial climate fluctuations driven by North Atlantic
ocean circulation, Nature, 367,447-450.
Wiesenfeld K, Moss F (1995) Stochastic resonance and the benefits of noise: from ice ages to
crayfish and SQUIDs, Nature, 373, 33-36.
Zeng X, Pielke R (1993) Error-growth dynamics and the predictability of surface thermally i
nduced atmospheric flow, 1. Almos. Sci, 50-17,2817-2844.
Grassberger P, Procaccia I (1983) Measuring the strangeness of strange attractors, Physica
m, 189-195.
Haltiner J (1970) Numerical Weather Prediction, 1. Wiley & Sons, New York.
Hernandez E, Pacheco J, Garcia R (1987) Evidencias del desarrollo de ondas frontales en las
inundaciones de Levante de 1982, Rev. R. Soc. Ci. EX.Fis.Nat, LXXXI, 2, 299-314.
Hernandez E, Pacheco J, Garcia R (l983a) Metodos numericos en la predicci6n del tiempo,
Rev. de Geojisica, 39.2, 151-164.
Hernandez E, Pacheco J, Garcia R (1983b) Inclusi6n de la liberaci6n de calor latente en las
ecuaciones de un modelo de predicci6n, Communication to the V Asamblea Nacional de
Geojisica y Geodesia, Madrid.
Herring J, Hobbs P (1994) Radiatively driven dynamics of the plume from Kuwait 1991 oil
fires, 1. Geophys. Res., 99 D9, 18809-18826.
Hughes T, Weaver A (1994) Multiple equilibria of an asymmetric two-basin ocean model, 1.
Phys. Ocean., 24-3, 619-637.
Lions J L (1991) "ElplanetaTierra", Espasa Calpe, Madrid.
Liu Z, Pedlosky J (1994) Thermocline forced by annual and decadal surface temperature
variation, 1. Phys. Ocean., 24-3, 587-608.
Liu Z, Yang H (1994) The intergyre chaotic transport, 1. Phys. Ocean., 24-8, 1768-1782.
Lorenz E (1969) The predictability of a flow which possesses many scales of motion, Tellus,
16(1),289-307.
Lorenz E (1986) On the existence of a slow manifold, 1. Atmos. Sci., 43(15), 1547-1557.
Morantine M, Watts R (1994)Timescales in energy balance climate models 2: The intermediate
time solutions, 1. Geophys. Res., 99 D2, 3643-3654.
Nagai T et al. (1992) El Nino-Southern Oscillation simulated in an MRI atmosphere-ocean
coupled general circulation model, 1. of Climate, 5-11, 1202-1233.
Nicolis C (1990) Chaotic dynamics, Markov processes and climate predictability, Tellus 42A,
401-412.
Pedlosky J (1987) Geophysicaljluid dynamics, Springer Verlag, Berlin.
Pelegri J L et al. (1995) These Proceedings.
Pereira C, Mascarenhas A (1994) Numerical simulation of an oceanic front response to an
atmospheric frontal passage, 1. Geophys. Res., 99 C8, 16081-16094.
Sancho P et al. (1992) A five-year climatology of back-trajectories from the Izafia baseline
station, Tenerife, Canary Islands, Almos. Envir., 26 A6, 1081-1096.
Schutz L (1979) Sahara dust transport over the North Atlantic Ocean: Model calculations and
meaurements, in Morales C (ed.) Saharan dust: Mobilization, transport, deposition
(267-278),1. Wiley & Son, New York.
Sellers W (1969) A global climate model based on the energy balance of the earth-atmosphere
system, 1. Appl. Met., 8, 392-400.
Short K (1993) Direct calculation of metric entropy from time series, 1. Comput. Phys., 104,
162-172.
Stephens G et al. (1993) The Earth's radiation budget and its relation to atmospheric hidrology,
1. Geophys. Res., 98 D3, 4931-4950.
Temam R (1995) These Proceedings.
Vannitsem S, Nicolis C (1994) Predictability experiments on a simplified thermal convection
model: The role of spatial scales,J. Geophys. Res., 99 D9, 10377-10386.
Watts R et aI. (1994) Timescales in energy balance climate models 1: The limiting case
solutions, 1. Geophys. Res., 99 D2, 3631-3642.
Weaver A, Hughes T (1994) Rapid interglacial climate fluctuations driven by North Atlantic
ocean circulation, Nature, 367,447-450.
Wiesenfeld K, Moss F (1995) Stochastic resonance and the benefits of noise: from ice ages to
crayfish and SQUIDs, Nature, 373, 33-36.
Zeng X, Pielke R (1993) Error-growth dynamics and the predictability of surface thermally i
nduced atmospheric flow, 1. Almos. Sci, 50-17,2817-2844.