Not exact matches
Dynamical models
of the
interaction between the planet and the belt indicate that the planet's mass is at most three times that
of Jupiter; a higher mass would lead to gravitational disruption
of the belt, matching predictions
of its location.
«This camera has the potential to greatly enhance our understanding
of very fast biological
interactions and chemical processes that will allow us to build better models
of complex,
dynamical systems such as cellular respiration, or to help doctors better deliver and monitor light - based therapies,» says Richard Conroy, Ph.D., program director for Optical Imaging at NIBIB.
«These ultrafast cameras have the potential to greatly enhance our understanding
of very fast biological
interactions and chemical processes and allow us to build better models
of complex,
dynamical systems.»
Recent advances in observational technique allow the detection
of the extremely faint structure around galaxies, such as loops or debris that are likely made by
dynamical interactions with satellite galaxies..
At any given instant it can be argued that the cell is in a «state» defined by its components — their concentrations and locations, the
interactions between components — that are modulated in space and time, and the complex circuitry — that involves a large number
of interacting networks and a snapshot
of the
dynamical processes — such as gene expression, cell cycle, transport
of components, etc..
This is in contrast to the prediction
of the theory that the low binary frequency in the cluster is caused by the disruption
of binaries due to
dynamical interactions.
Some researchers assume that a close system evolves into a wide system over millions
of years due to
dynamical interactions, but others guess that turbulence in a gas cloud fragments the cloud into smaller ones and stars are formed in each small cloud.
The stratosphere is now known to be a region
of intense
interactions among radiative,
dynamical, and chemical processes in which horizontal mixing
of gaseous components proceeds much more rapidly than vertical mixing.
Climate models that include these aerosol - cloud
interactions fail to include a number
of buffering responses, such as rainfall scavenging
of the aerosols and compensating
dynamical effects (which would reduce the magnitude
of the aci cooling effect).
The meeting will mainly cover the following themes, but can include other topics related to understanding and modelling the atmosphere: ● Surface drag and momentum transport: orographic drag, convective momentum transport ● Processes relevant for polar prediction: stable boundary layers, mixed - phase clouds ● Shallow and deep convection: stochasticity, scale - awareness, organization, grey zone issues ● Clouds and circulation feedbacks: boundary - layer clouds, CFMIP, cirrus ● Microphysics and aerosol - cloud
interactions: microphysical observations, parameterization, process studies on aerosol - cloud
interactions ● Radiation: circulation coupling;
interaction between radiation and clouds ● Land - atmosphere
interactions: Role
of land processes (snow, soil moisture, soil temperature, and vegetation) in sub-seasonal to seasonal (S2S) prediction ● Physics - dynamics coupling: numerical methods, scale - separation and grey - zone, thermodynamic consistency ● Next generation model development: the challenge
of exascale,
dynamical core developments, regional refinement, super-parametrization ● High Impact and Extreme Weather: role
of convective scale models; ensembles; relevant challenges for model development
This «statistical coherence» can be regarded as a kind
of organization
of a complicated
dynamical system, and identifying its statistically stable characteristics is similar to the notion
of coherence understood as self - organization
of multicomponent systems that results from chaotic
interactions of their elements (see, e.g., [1]-RRB-.»
Therefore, we suggest that a significant portion
of the wintertime temperature trend is driven by
dynamical interactions between October Eurasian snow cover, which has increased over the last two decades, and the large - scale NH extratropical circulation in the late autumn and winter.
Modes or patterns
of climate variability - Natural variability
of the climate system, in particular on seasonal and longer time scales, predominantly occurs with preferred spatial patterns and time scales, through the
dynamical characteristics
of the atmospheric circulation and through
interactions with the land and ocean surfaces.