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Kramers-Kronig relations in optical materials research
Electrodynamic Properties of a General Physical System.- General Properties of the Linear Optical Response.- Kramers-Kronig Relations and Sum Rules in Linear Optics.- General Properties of the
Extremes and Recurrence in Dynamical Systems
This book provides a comprehensive introduction for the study of extreme events in the context of dynamical systems. The introduction provides a broad overview of the interdisciplinary research area
ENERGETICS OF CLIMATE MODELS: NET ENERGY BALANCE AND MERIDIONAL ENTHALPY TRANSPORT
We analyze the publicly released outputs of the simulations performed by climate models (CMs) in preindustrial (PI) and Special Report on Emissions Scenarios A1B (SRESA1B) conditions. In the PI
Prevailing climatic trends and runoff response from Hindukush-Karakoram-Himalaya, upper Indus basin
We analyze trends in maximum, minimum and mean temperatures (Tx, Tn, and Tavg, respectively), diurnal temperature range (DTR) and precipitation from 18 stations (1250-4500 m asl) for their
Numerical Bifurcation Methods and their Application to Fluid Dynamics: Analysis beyond Simulation
We provide an overview of current techniques and typical applications of numerical bifurcation analysis in fluid dynamical problems. Many of these problems are characterized by high-dimensional
Stochastic Parameterization: Towards a new view of Weather and Climate Models
AbstractThe last decade has seen the success of stochastic parameterizations in short-term, medium-range, and seasonal forecasts: operational weather centers now routinely use stochastic
Hydrological cycle over South and Southeast Asian river basins as simulated by PCMDI/CMIP3 experiments
Abstract. We investigate how the climate models contributing to the PCMDI/CMIP3 dataset describe the hydrological cycle over four major South and Southeast Asian river basins (Indus, Ganges,
The physics of climate variability and climate change
The climate system is a forced, dissipative, nonlinear, complex and heterogeneous system that is out of thermodynamic equilibrium. The system exhibits natural variability on many scales of motion, in
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