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Unified multifractal atmospheric dynamics tested in the tropics:part II,vertical scaling and generalized scale invariance
multifractal atmospheric dynamics vertical scaling generalized scale invariance
2009/11/16
We empirically investigate the scaling behaviour of the horizontal wind along the vertical direction using 287 radiosonde soundings with a resolution of 50 m. We compare the results obtained with thos...
Some Features of the Microclimate of a Luxuriant Turnip Rape Field on a Clear Day.Part II
Features Microclimate Luxuriant Turnip Rape Field
2009/6/18
Some Features of the Microclimate of a Luxuriant Turnip Rape Field on a Clear Day.Part II.
Investigation of the Forecasting Error of a Simple Barotropic Model with the Aid of Empirical Orthogonal Functions. Part II
meteorology Forecasting Error Functions
2009/6/18
Investigation of the Forecasting Error of a Simple Barotropic Model with the Aid of Empirical Orthogonal Functions. Part II.
The Interaction of the Monthly Mean Flow and Large-Scale Transient Eddies in two Different Circulation Types. Part II
Interaction Transient Circulation
2009/6/16
The Interaction of the Monthly Mean Flow and Large-Scale Transient Eddies in two Different Circulation Types. Part II
Atmospheric impact of the 1783–1784 Laki Eruption: Part II Climatic effect of sulphate aerosol
Atmospheric impact Laki Eruption Climatic effect of sulphate aerosol
2009/3/11
The long 1783-1784 eruption of Laki in southern Iceland, was one of the first eruptions to have been linked to an observed climate anomaly, having been held responsible for cold temperatures over much...
Systematic reduction of complex tropospheric chemical mechanisms, Part II: Lumping using a time-scale based approach
complex tropospheric chemical mechanisms Lumping time-scale
2009/3/6
This paper presents a formal method of species lumping that can be applied automatically to intermediate compounds within detailed and complex tropospheric chemical reaction schemes. The method is bas...
A review of biomass burning emissions part II: intensive physical properties of biomass burning particles
biomass burning emissions intensive physical properties biomass burning particles
2009/2/7
The last decade has seen tremendous advances in atmospheric aerosol particle research that is often performed in the context of climate and global change science. Biomass burning, one of the largest s...
Simulating aerosol microphysics with the ECHAM4/MADE GCM – Part II: Results from a first multiannual simulation of the submicrometer aerosol
Simulating aerosol microphysics ECHAM4/MADE GCM multiannual simulation submicrometer aerosol
2009/1/21
First results of a multiannual integration with the new global aerosol model system ECHAM4/MADE are presented. This model system enables simulations of the particle number concentration and size-distr...
Modeling of biomass smoke injection into the lower stratosphere by a large forest fire（Part II）: sensitivity studies
biomass smoke lower stratosphere forest fire sensitivity studies
2009/1/20
The Chisholm forest fire that burned in Alberta, Canada, in May 2001 resulted in injection of substantial amounts of smoke into the lower stratosphere. We used the cloud-resolving plume model ATHAM (A...
The total ozone field separated into meteorological regimes – Part II: Northern Hemisphere mid-latitude total ozone trends
total ozone field meteorological regimes Northern Hemisphere mid-latitude ozone trends
2009/1/19
Previous studies have presented clear evidence that the Northern Hemisphere total ozone field can be separated into distinct regimes (tropical, midlatitude, polar, and arctic) the boundaries of which ...
Implementation of a Markov Chain Monte Carlo method to inorganic aerosol modeling of observations from the MCMA-2003 campaign – Part II: Model application to the CENICA, Pedregal and Santa Ana sites
Markov Chain Monte Carlo method inorganic aerosol CENICA Pedregal Santa Ana sites
2009/1/16
A Markov Chain Monte Carlo model for integrating the observations of inorganic species with a thermodynamic equilibrium model was presented in Part I of this series. Using observations taken at three ...
Columnar modelling of nucleation burst evolution in the convective boundary layer – first results from a feasibility study Part II: Meteorological characterisation
nucleation burst convective boundary layer feasibility study Meteorological characterisation
2009/1/15
While in Paper I of four papers a revised columnar high-order modelling approach to investigate gas-aerosol-turbulence interactions in the convective boundary layer (CBL) was deduced, in the present P...
Homogeneous nucleation rates of nitric acid dihydrate (NAD) at simulated stratospheric conditions – Part II: Modelling
Homogeneous nucleation rates nitric acid dihydrate NAD
2009/1/13
Activation energies ΔGact for the nucleation of nitric acid dihydrate (NAD) in supercooled binary HNO3/H2O solution droplets were calculated from volume-based nucleation rate measurements using the AI...
Water activity and activation diameters from hygroscopicity data - Part II: Application to organic species
Water activity activation diameters hygroscopicity data organic species
2009/1/4
A method has been developed for using particle hygroscopicity measurements made with a humidified tandem differential mobility analyzer (HTDMA) to determine water activity as a function of solute wei...
Evaluation and modeling of the size fractionated aerosol particle number concentration measurements nearby a major road in Helsinki – Part II: Aerosol measurements within the SAPPHIRE project
size fractionated aerosol particle Helsinki SAPPHIRE project
2008/12/16
This study presents an evaluation and modeling exercise of the size fractionated aerosol particle number concentrations measured nearby a major road in Helsinki during 23 August–19 September 2003 and ...