L. Osterloh, C. Böckmann, R. Mamouri, A. Papayannis
{"title":"An Adaptive Base Point Algorithm for the Retrieval of Aerosol Microphysical Properties","authors":"L. Osterloh, C. Böckmann, R. Mamouri, A. Papayannis","doi":"10.2174/1874282301105010061","DOIUrl":"https://doi.org/10.2174/1874282301105010061","url":null,"abstract":"We propose a new iterative algorithm for the retrieval of the microphysical properties of stratospheric and tropospheric aerosols from multiwavelength lidar data. We consider the basic equation as an ill-posed problem and solve the system derived from spline collocation via a Pade iteration. The algorithm takes special care of the fact that the reconstruction of the distribution via spline collocation is very sensitive to the choice of base points of the chosen spline basis. The algorithm makes use of this fact by changing the base points used for the spline collocation at certain iteration steps. In addition, the effects of projection to ensure a nonnegative solution are examined. We tested how well this and other algorithms are suitable for retrieving the complex refractive index of the particles as well. We also examine whether the algorithm is capable of distinguishing between different, very small imaginary parts of the refractive index, which is often a main problem in practice. Finally, the algorithm is applied to real multiwavelength Raman lidar data and our results are partially validated by the thermodynamic chemical model Isorropia II.","PeriodicalId":122982,"journal":{"name":"The Open Atmospheric Science Journal","volume":"198 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2011-04-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"125731462","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
G. Jandieri, A. Ishimaru, V. Gavrilenko, A. Surmava, A. Gvelesiani
{"title":"On the Features of Magnetogradient Planetary Waves in the Approximation of the Spherical Symmetry of the Ionosphere","authors":"G. Jandieri, A. Ishimaru, V. Gavrilenko, A. Surmava, A. Gvelesiani","doi":"10.2174/1874282301105010033","DOIUrl":"https://doi.org/10.2174/1874282301105010033","url":null,"abstract":"A problem of propagation of very long planetary waves in the upper atmosphere of the Earth is investigated. A new exact solution of the magnetohydrodynamics equations of the ionosphere in the spherical coordinate system is found taking into account the Earth’s rotation and geomagnetic field. The general dispersion equation for the planetary waves in the E and F regions of the ionosphere is derived and propagation of these waves in weakly ionized ionospheric plasma are studied.","PeriodicalId":122982,"journal":{"name":"The Open Atmospheric Science Journal","volume":"93 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2011-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122970796","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Multi-Frequency HF Observations of Farley-Buneman Phase Velocities","authors":"D. Moorcroft, L. Kagan, R. S. Kissack","doi":"10.2174/1874282301105010050","DOIUrl":"https://doi.org/10.2174/1874282301105010050","url":null,"abstract":"With the potential use of SuperDARN radars in mind and to test the theoretical predictions for dependence of the phase velocity of Farley-Buneman waves on radar frequencies in the HF range, a statistical analysis was made of over 11,000 specifically selected spectra from multi-frequency observations by the SuperDARN ykkvibaer radar in September-October 2000. Good qualitative agreement was found between the observed and predicted frequency dependence for slightly disturbed magnetic conditions. Assuming that increased magnetic activity (higher Kp) manifests itself via enhanced electron temperature and applying the algorithm of the control parameters of Kagan & Kissack [1], it was shown that in agreement with observations, the dependence of the FB waves phase velocity on the irregularity wave number (radar frequency) should decrease with increasing electron temperature (Kp). The results make it clear that specially designed multi-frequency SuperDARN experiments would be a valuable tool in studying the HF FarleyBuneman waves at high latitudes.","PeriodicalId":122982,"journal":{"name":"The Open Atmospheric Science Journal","volume":"22 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2011-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122808638","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Detecting a Large-Scale Upper-Atmospheric Plasma Inhomogeneity Using the Method of Multifrequency Radio Sounding in the Decametric Wavelength Range","authors":"N. T. Afanasiev, A. Afanasiev, V. Markov","doi":"10.2174/1874282301105010043","DOIUrl":"https://doi.org/10.2174/1874282301105010043","url":null,"abstract":"We examine the problem of transionospheric sounding with satellite radio signals at frequencies that are close to the edge of the radio transparency frequency range of the ionosphere. We derive asymptotic formulas for the group delay time of the transionospheric radio signal and present an example of how they are implemented if there is a localized large-scale electron density inhomogeneity in the ionosphere. Finally, we suggest techniques for detecting large-scale ionospheric inhomogeneities, which are based on numerical-asymptotic synthesis of disturbed distance-frequency characteristics of decametric signals radiated from a low-orbiting or geostationary satellite.","PeriodicalId":122982,"journal":{"name":"The Open Atmospheric Science Journal","volume":"29 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2011-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127240478","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Editorial: Waves Propagation in the Upper Atmosphere","authors":"G. Jandieri","doi":"10.2174/1874282301105010032","DOIUrl":"https://doi.org/10.2174/1874282301105010032","url":null,"abstract":"","PeriodicalId":122982,"journal":{"name":"The Open Atmospheric Science Journal","volume":"18 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2011-04-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127446994","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Detection of Tornado Frequency Trend Over Ontario, Canada","authors":"Z. Cao, Huaqing Cai","doi":"10.2174/1874282301105010027","DOIUrl":"https://doi.org/10.2174/1874282301105010027","url":null,"abstract":"An upward trend in Ontario tornado frequency (about 1.6 tornadoes/decade with the statistically significant level at least at 95%) is identified using three independent approaches. The first method is the conventional linear regression method that had no disturbance to the original tornado time series. The second approach is to employ the Mann-Kendall test with consideration of removing a lag one autoregressive process. The trend is further firmed up using the Monte Carlo simulation. The robustness of the detected tornado frequency trend presented in this work offers an example for tornado frequency trend analysis over other regions of the world. It is shown in this study that the Ontario tornado frequency is linked to ENSO (El Nino/Southern Oscillation) signals with a statistically significant level at 99%.","PeriodicalId":122982,"journal":{"name":"The Open Atmospheric Science Journal","volume":"278 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2011-03-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"115422124","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"On the Stability of Three-Dimensional Disturbances in Stratified Flow with Lateral and Vertical Shear","authors":"I. Panayotova, J. McHugh","doi":"10.2174/1874282301105010023","DOIUrl":"https://doi.org/10.2174/1874282301105010023","url":null,"abstract":"Howard's semi-circle theorem is generalized for three-dimensional disturbances in a non-Boussinesq stratified fluid with a mean flow varying horizontally and vertically. In case of Boussinesq approximation Howard's and Rayleigh's theorem are extended for three-dimensional disturbances in a fluid with a mean flow varying only with respect to the latitude.","PeriodicalId":122982,"journal":{"name":"The Open Atmospheric Science Journal","volume":"5 1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2011-02-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127083773","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Long-Term Dependencies of Annual and Semiannual Components of NmF2 Over Concepción","authors":"M. Bravo, A. Foppiano, R. A. Rio","doi":"10.2174/1874282301105010002","DOIUrl":"https://doi.org/10.2174/1874282301105010002","url":null,"abstract":"In this work an attempt is made to determine whether the annual and semiannual components of the NmF2 observed over Concepcion (36.8°S; 73.0°W), Chile, exhibit long-term trends. Monthly median hourly values of NmF2 determined from ionosonde observations are analyzed. Although the assessed trends for NmF2 and for the semiannual and annual components of NmF2, are hardly significant by any statistical test, they exhibit a systematic diurnal evolution. NmF2 trends are almost null during night time and negative from around noon to the early evening. The same can be said for trends of the amplitudes of the semiannual component. On the contrary, trends for the annual component are always positive and exhibit a rather irregular diurnal pattern. It seems reasonable then to particularly look for an explanation of the semiannual component long-term changes when concerned with long-term changes of NmF2. The semiannual variation is linked to composition and thermospheric wind effects, and solar zenith angle changes which may be connected to changes of the strength of the global circulation. But, more study is needed to envisage the changes on the semiannual component of NmF2 which may arise from eventual long-term changes of the global circulation.","PeriodicalId":122982,"journal":{"name":"The Open Atmospheric Science Journal","volume":"6 1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2011-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122701087","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Stratospheric Temperature Trends Between 10 and 70 hPa During the Period 1948-2009","authors":"M. M. Z. Artigas, P. Campra","doi":"10.2174/1874282301105010016","DOIUrl":"https://doi.org/10.2174/1874282301105010016","url":null,"abstract":"Trends in zonal mean temperatures between 10 and 70 hPa have been assessed for the period 1948-2009 using zonal monthly mean temperature from the NCEP/NCAR reanalysis dataset. Monthly temperature linear trends were calculated for the Northern and Southern Hemisphere at a 5o step in latitude. The observed trend pattern agrees with a general cooling for every month. The area of negative trends, in the latitude-month grid, increases as we go down in the stratosphere. Positive trends are also observed, mainly at 10 hPa for equatorial zones and summer northern and southern latitudes, and also at southern high-latitudes during the months July-February for every height analyzed. The positive trends observed at 10 hPa at equatorial and mid-latitudes are due to a warming from the beginning of the record until the beginning of 1980s, coincident with the El Chichon eruption. In the case of high latitudes, also at 10 hPa, there seems to be a \"step\" in 1979. For lower altitudes the positive trends are smoother. In the case of 10 hPa we suggest as a hint, that the temperature behavior for the \"warming\" cases follows the 11-year running mean of the total solar irradiance.","PeriodicalId":122982,"journal":{"name":"The Open Atmospheric Science Journal","volume":"11 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2011-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128930005","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
{"title":"Possible Sources of Long-Term Variations in the Mid-Latitude Ionosphere","authors":"A. Elias","doi":"10.2174/1874282301105010009","DOIUrl":"https://doi.org/10.2174/1874282301105010009","url":null,"abstract":"Trends in the upper atmosphere, together with the global warming of the lower atmosphere, are part of the global change of the Earth system. In the present work, which is focused in the upper atmosphere, long-term variations of the critical frequency of the ionospheric F2 layer, foF2, are studied in terms of the following possible causes: (1) long- term variations of the solar EUV radiation shown by the solar cycle length (SCL), (2) long-term variations in geomagnetic activity measured by the aa index, (3) the increasing greenhouse gases concentration in the lower atmosphere which would be producing a temperature decrease in the upper atmosphere, and (4) the Earth's main magnetic field secular variation, which implies changes in the dip angle (I) affecting the thermospheric neutral winds that move the conducting plasma of the ionosphere. For this purpose, foF2 time series of four mid-latitude stations were processed. After filtering the solar activity effect, the long-term variability of these time series and that of the mentioned possible trend sources, were analyzed. The study of trends in the upper atmosphere is an important contribution to one of the present focus of climate science that is the determination of the extent to which human activities are altering the planetary energy balance through the emission of greenhouse gases and pollutants.","PeriodicalId":122982,"journal":{"name":"The Open Atmospheric Science Journal","volume":"103 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2011-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"117308119","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}