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Niklaus Kampfer - One of the best experts on this subject based on the ideXlab platform.
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Short-term stratospheric ozone fluctuations observed by GROMOS microwave radiometer at Bern
'Springer Science and Business Media LLC', 2018Co-Authors: Lorena Moreira, Klemens Hocke, Niklaus KampferAbstract:Abstract The ground-based millimeter wave ozone spectrometer (GROMOS) has been continually measuring middle atmospheric ozone volume mixing ratio profiles above Bern, Switzerland ( $$46.95^{\circ }\hbox {N}$$ 46 . 95 ∘ N , $$7.44^{\circ }\hbox {E}$$ 7 . 44 ∘ E , 577 m), since 1994 in the frame of NDACC. The high temporal resolution of GROMOS (30 min) allows the analysis of short-term fluctuations. The present study analyses the temporal perturbations, ranging from 1 to 8 h, observed in stratospheric ozone from June 2011 to May 2012. The short-term fluctuations of stratospheric ozone are within 5%, and GROMOS appears to have relative amplitudes stable over time smaller than 2% at 10 hPa (32 km). The strongest natural fluctuations of stratospheric ozone (about 1% at 10 hPa) above Bern occur during winter due to displacements and deformations of the polar vortex towards mid-latitudes
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Results from the validation campaign of the ozone radiometer GROMOS-C at the NDACC station of Réunion island
Atmospheric Chemistry and Physics, 2016Co-Authors: Susana Fernandez, Niklaus Kampfer, Rolf Rüfenacht, Thierry Portafaix, Françoise Posny, Guillaume PayenAbstract:Ozone performs a key role in the middle atmosphere and its monitoring is thus necessary. At the Institute of Applied Physics of the University of Bern, Switzerland, we built a new ground-based microwave radiometer, GROMOS-C (GRound based Ozone MOnitoring System for Campaigns). It has a compact design and can be operated remotely with very little maintenance requirements, being therefore suitable for remote deployments. It has been conceived to measure the vertical distribution of ozone in the middle atmosphere, by observing pressure-broadened emission spectra at a frequency of 110.836 GHz. In addition, meridional and zonal wind profiles can be retrieved, based on the Doppler shift of the ozone line measured in the four directions of observation (north, east, south and west). In June 2014 the radiometer was installed at the Maïdo observatory, on Réunion island (21.2 • S, 55.5 • E). High-resolution ozone spectra were recorded continuously over 7 months. Vertical profiles of ozone have been retrieved through an optimal estimation inversion process, using the Atmospheric Radiative Transfer Simulator ARTS2 as the forward model. The validation is performed against ozone profiles from the Microwave Limb Sounder (MLS) on the Aura satellite, the ozone lidar located at the observatory and with ozone profiles from weekly radiosondes. Zonal and merid-ional winds retrieved from GROMOS-C data are validated against another wind radiometer located in situ, WIRA. In addition, we compare both ozone and winds with ECMWF (European Centre for Medium-Range Weather Forecasts) model data. Results show that GROMOS-C provides reliable ozone profiles between 30 and 0.02 hPa. The comparison with lidar profiles shows a very good agreement at all levels. The accordance with the MLS data set is within 5 % for pressure levels between 25 and 0.2 hPa. GROMOS-C's wind profiles are in good agreement with the observations by WIRA and with the model data, differences are below 5 m s −1 for both.
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trend analysis of the 20 year time series of stratospheric ozone profiles observed by the GROMOS microwave radiometer at bern
Atmospheric Chemistry and Physics, 2015Co-Authors: Lorena Moreira, Klemens Hocke, E Eckert, T Von Clarmann, Niklaus KampferAbstract:Abstract. The ozone radiometer GROMOS (GROund-based Millimeter-wave Ozone Spectrometer) has been performing continuous observations of stratospheric ozone profiles since 1994 above Bern, Switzerland (46.95° N, 7.44° E, 577 m). GROMOS is part of the Network for the Detection of Atmospheric Composition Change (NDACC). From November 1994 to October 2011, the ozone line spectra were measured by a filter bench (FB). In July 2009, a fast Fourier transform spectrometer (FFTS) was added as a back end to GROMOS. The new FFTS and the original FB measured in parallel for over 2 years. The ozone profiles retrieved separately from the ozone line spectra of FB and FFTS agree within 5 % at pressure levels from 30 to 0.5 hPa, from October 2009 to August 2011. A careful harmonisation of both time series has been carried out by taking the FFTS as the reference instrument for the FB. This enables us to assess the long-term trend derived from stratospheric ozone observations at Bern. The trend analysis was performed by using a robust multilinear parametric trend model which includes a linear term, the solar variability, the El Nino–Southern Oscillation (ENSO) index, the quasi-biennial oscillation (QBO), the annual and semi-annual oscillation and several harmonics with period lengths between 3 and 24 months. Over the last years, some experimental and modelling trend studies have shown that the stratospheric ozone trend is levelling off or even turning positive. With our observed ozone profiles, we are able to support this statement by reporting a statistically significant trend of +3.14 % decade−1 at 4.36 hPa (37.76 km), covering the period from January 1997 to January 2015, above Bern. Additionally, we have estimated a negative trend over this period of −3.94 % decade−1 at 0.2 hPa (59 km).
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GROMOS c a novel ground based microwave radiometer for ozone measurement campaigns
Atmospheric Measurement Techniques, 2015Co-Authors: Susana Fernandez, Axel Murk, Niklaus KampferAbstract:Abstract. Stratospheric ozone is of major interest as it absorbs most harmful UV radiation from the sun, allowing life on Earth. Ground-based microwave remote sensing is the only method that allows for the measurement of ozone profiles up to the mesopause, over 24 hours and under different weather conditions with high time resolution. In this paper a novel ground-based microwave radiometer is presented. It is called GROMOS-C (GRound based Ozone MOnitoring System for Campaigns), and it has been designed to measure the vertical profile of ozone distribution in the middle atmosphere by observing ozone emission spectra at a frequency of 110.836 GHz. The instrument is designed in a compact way which makes it transportable and suitable for outdoor use in campaigns, an advantageous feature that is lacking in present day ozone radiometers. It is operated through remote control. GROMOS-C is a total power radiometer which uses a pre-amplified heterodyne receiver, and a digital fast Fourier transform spectrometer for the spectral analysis. Among its main new features, the incorporation of different calibration loads stands out; this includes a noise diode and a new type of blackbody target specifically designed for this instrument, based on Peltier elements. The calibration scheme does not depend on the use of liquid nitrogen; therefore GROMOS-C can be operated at remote places with no maintenance requirements. In addition, the instrument can be switched in frequency to observe the CO line at 115 GHz. A description of the main characteristics of GROMOS-C is included in this paper, as well as the results of a first campaign at the High Altitude Research Station at Jungfraujoch (HFSJ), Switzerland. The validation is performed by comparison of the retrieved profiles against equivalent profiles from MLS (Microwave Limb Sounding) satellite data, ECMWF (European Centre for Medium-Range Weather Forecast) model data, as well as our nearby NDACC (Network for the Detection of Atmospheric Composition Change) ozone radiometer measuring at Bern.
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a climatology of the diurnal variations in stratospheric and mesospheric ozone over bern switzerland
Atmospheric Chemistry and Physics, 2014Co-Authors: Simone Studer, Klemens Hocke, Ansgar Ulrich Schanz, Hauke Schmidt, Niklaus KampferAbstract:Abstract. The ground-based radiometer GROMOS, stationed in Bern (47.95° N, 7.44° E), Switzerland, has a unique data set: it obtains ozone profiles from November 1994 to present with a time resolution of 30 min and equivalent quality during night- and daytime. Here, we derive a monthly climatology of the daily ozone cycle from 17 years of GROMOS observation. We present the diurnal ozone variation of the stratosphere and mesosphere. Characterizing the diurnal cycle of stratospheric ozone is important for correct trend estimates of the ozone layer derived from satellite observations. The diurnal ozone cycle from GROMOS is compared to two models: the Whole Atmosphere Community Climate Model (WACCM) and the Hamburg Model of Neutral and Ionized Atmosphere (HAMMONIA). Generally, observation and models show a good agreement: in the lower mesosphere, daytime ozone is for both GROMOS and models around 25% less than midnight ozone. In the stratosphere, ozone reaches its maximum in the afternoon showing values several percent larger than the midnight value. Further, GROMOS and models indicate a seasonal behaviour of the diurnal ozone variations in the stratosphere with a larger afternoon maximum during daytime in summer than in winter. Using the 17 years of ozone profiles from GROMOS, we find strong interannual variations in the diurnal ozone cycle for both the stratosphere and the mesosphere. Interannual variability in temperature, atmospheric circulation and composition may explain the observed interannual variability of the diurnal ozone cycle above Bern.
Wilfred F Van Gunsteren - One of the best experts on this subject based on the ideXlab platform.
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interfacing the GROMOS bio molecular simulation software to quantum chemical program packages
Journal of Computational Chemistry, 2012Co-Authors: Katharina Meier, Nathan Schmid, Wilfred F Van GunsterenAbstract:The newly implemented quantum-chemical/molecular-mechanical (QM/MM) functionality of the Groningen molecular simulation (GROMOS) software for (bio)molecular simulation is described. The implementation scheme is based on direct coupling of the GROMOS C++ software to executables of the quantum-chemical program packages MNDO and TURBOMOLE, allowing for an independent further development of these packages. The new functions are validated for different test systems using program and model testing techniques. The effect of truncating the QM/MM electrostatic interactions at various QM/MM cutoff radii is discussed and the application of semiempirical versus density-functional Hamiltonians for a solute molecule in aqueous solution is compared. © 2012 Wiley Periodicals, Inc.
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architecture implementation and parallelisation of the GROMOS software for biomolecular simulation
Computer Physics Communications, 2012Co-Authors: Nathan Schmid, Clara D Christ, Markus Christen, Andreas P Eichenberger, Wilfred F Van GunsterenAbstract:Abstract In this work the design of the latest version of the GROMOS software for biomolecular simulation, GROMOS11 is discussed. Detailed organisation and class descriptions of the MD++ simulation program and the GROMOS++ analysis package are given. It is shown how the code was documented, how it can be easily modified and extended, how debugging of it is carried out. Additional efficiency and parallelisation concepts are presented and benchmarked.
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force field evaluation for biomolecular simulation free enthalpies of solvation of polar and apolar compounds in various solvents
ChemPhysChem, 2006Co-Authors: Daan P Geerke, Wilfred F Van GunsterenAbstract:Recently, the GROMOS biomolecular force field parameter set 53A6—which has been parametrized to reproduce experimentally determined free enthalpies of hydration and solvation in cyclohexane of amino acid side-chain analogs—was presented. To investigate the transferability of the new parameter set, we calculated free enthalpies of solvation of a range of polar and apolar compounds in different solvents (methanol, dimethyl sulfoxide (DMSO), acetonitrile, and acetone) from molecular dynamics simulations using the GROMOS 53A6 force field. For methanol and DMSO, parameters were used that are available in the 53A6 parameter set. For acetonitrile, a recently developed model was taken and for acetone, two models available in literature were used. We found that trends in and values for the solvation free enthalpies are in satisfactory agreement with experiment, except for the solvation in acetone for which deviations from experiment can be explained in terms of the properties of the models used.
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amine hydration a united atom force field solution
ChemPhysChem, 2005Co-Authors: Chris Oostenbrink, Daniel Juchli, Wilfred F Van GunsterenAbstract:The free energies of hydration for ammonia and mono-, di-, and trimethylated amines experimentally show an unexpected trend that has, in the past, been difficult to reproduce computationally. Absolute and relative free energies of hydration of these compounds were calculated using the OPLS all-atom and the united-atom GROMOS force fields. Both force fields reproduce the relative free energy of hydration, but the absolute free energies of hydration were only reproduced within k B T when using the recently developed GROMOS parameter set 53A6. Relative free energies of solvation in chloroform could also be reproduced indicating a proper partitioning of the compounds between polar and apolar media. Overall we conclude that it is possible to resolve the amine hydration problem using a simple united-atom force field.
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a biomolecular force field based on the free enthalpy of hydration and solvation the GROMOS force field parameter sets 53a5 and 53a6
Journal of Computational Chemistry, 2004Co-Authors: Chris Oostenbrink, Alessandra Villa, Alan E Mark, Wilfred F Van GunsterenAbstract:Successive parameterizations of the GROMOS force field have been used successfully to simulate biomolecular systems over a long period of time. The continuing expansion of computational power with time makes it possible to compute ever more properties for an increasing variety of molecular systems with greater precision. This has led to recurrent parameterizations of the GROMOS force field all aimed at achieving better agreement with experimental data. Here we report the results of the latest, extensive reparameterization of the GROMOS force field. In contrast to the parameterization of other biomolecular force fields, this parameterization of the GROMOS force field is based primarily on reproducing the free enthalpies of hydration and apolar solvation for a range of compounds. This approach was chosen because the relative free enthalpy of solvation between polar and apolar environments is a key property in many biomolecular processes of interest, such as protein folding, biomolecular association, membrane formation, and transport over membranes. The newest parameter sets, 53A5 and 53A6, were optimized by first fitting to reproduce the thermodynamic properties of pure liquids of a range of small polar molecules and the solvation free enthalpies of amino acid analogs in cyclohexane (53A5). The partial charges were then adjusted to reproduce the hydration free enthalpies in water (53A6). Both parameter sets are fully documented, and the differences between these and previous parameter sets are discussed.
Chris Oostenbrink - One of the best experts on this subject based on the ideXlab platform.
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The Impact of Using Single Atomistic Long-Range Cutoff Schemes with the GROMOS 54A7 Force Field
2018Co-Authors: Tomás F. D. Silva, Chris Oostenbrink, Diogo Vila-viçosa, Pedro B. P. S. Reis, Bruno L. Victor, Matthias Diem, Miguel MachuqueiroAbstract:With the recent increase in computing power, the molecular modeling community is now more focused on improving the accuracy and overall quality of biomolecular simulations. For the available simulation packages, force fields, and all other associated methods used, this relates to how well they describe the conformational space and thermodynamic properties of a biomolecular system. The parameter sets of GROMOS force fields have been parametrized and validated with the reaction field (RF) method using charge groups and a twin-range cutoff scheme (0.8/1.4 nm). However, the most recent versions of GROMACS (since v.2016) discontinued the support for charge groups. To take full advantage of the newer and faster versions of this software package with GROMOS 54A7 and RF, we need to evaluate the impact of using a single cutoff scheme (vs twin-range) and of using the Verlet list update method (which is atomistic) compared to the group-based cutoff scheme. Our results show that the GROMOS 54A7 force field seems consistent with a single cutoff, since the resulting conformation and protonation ensembles were indistinguishable. The GROMOS parametrization procedure was also reproduced using an atomistic cutoff scheme, and we have observed that the hydration free energy values of small amino acid side-chain analogues were similar to the ones obtained with the group-based protocol. We do observe a small impact of the atomistic cutoff scheme in the conformational space of the model systems studied (G1-PAMAM and DMPC). However, since the structural properties of these systems are well converged for the cutoff range used (1.4–2.0 nm), unlike with the group-based cutoff schemes, we are confident that the atomistic cutoff can be adopted with RF for MD and constant-pH MD biomolecular simulations using the GROMOS 54A7 force field
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Testing of the GROMOS Force-Field Parameter Set 54A8: Structural Properties of Electrolyte Solutions, Lipid Bilayers, and Proteins
2016Co-Authors: Maria M. Reif, Moritz Winger, Chris OostenbrinkAbstract:Chem. Theory Comput. 2012, 8, 3705−3723] is the first of its kind to contain nonbonded parameters for charged amino acid side chains that are derived in a rigorously thermodynamic fashion, namely a calibration against single-ion hydration free energies. Considering charged moieties in solution, the most decisive signature of the GROMOS 54A8 force field in comparison to its predecessor 54A7 can probably be found in the thermodynamic equilibrium between salt-bridged ion pair formation and hydration. Possible shifts in this equilibrium might crucially affect the properties of electrolyte solutions or/and the stability of (bio)molecules. It is therefore important to investigate the consequences of the altered description of charged oligoatomic species in the GROMOS 54A8 force field. The present study focuses on examining the ability of the GROMOS 54A8 force field to accurately model the structural properties of electrolyte solutions, lipid bilayers, and proteins. It is found that (i) aqueous electrolytes involving oligoatomic species (sodium acetate, methylammonium chloride, guanidinium chloride) reproduce experimental salt activity derivatives for concentrations up to 1.0 m (1.0-molal) very well, and good agreement between simulated and experimental data is also reached for sodium acetate and methylammonium chloride at 2.0 m concentration, while not even qualitative agreement is found for sodium chloride throughout the whole range of examined concentrations, indicating a failure of the GROMOS 54A7 and 54A8 force-fiel
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an automated force field topology builder atb and repository version 1 0
Journal of Chemical Theory and Computation, 2011Co-Authors: Alpeshkumar K Malde, Chris Oostenbrink, Le Zuo, Matthew Breeze, Martin Stroet, David Poger, Pramod C Nair, Alan E MarkAbstract:The Automated force field Topology Builder (ATB, http://compbio.biosci.uq.edu.au/atb) is a Web-accessible server that can provide topologies and parameters for a wide range of molecules appropriate for use in molecular simulations, computational drug design, and X-ray refinement. The ATB has three primary functions: (1) to act as a repository for molecules that have been parametrized as part of the GROMOS family of force fields, (2) to act as a repository for pre-equilibrated systems for use as starting configurations in molecular dynamics simulations (solvent mixtures, lipid systems pre-equilibrated to adopt a specific phase, etc.), and (3) to generate force field descriptions of novel molecules compatible with the GROMOS family of force fields in a variety of formats (GROMOS, GROMACS, and CNS). Force field descriptions of novel molecules are derived using a multistep process in which results from quantum mechanical (QM) calculations are combined with a knowledge-based approach to ensure compatibility (a...
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amine hydration a united atom force field solution
ChemPhysChem, 2005Co-Authors: Chris Oostenbrink, Daniel Juchli, Wilfred F Van GunsterenAbstract:The free energies of hydration for ammonia and mono-, di-, and trimethylated amines experimentally show an unexpected trend that has, in the past, been difficult to reproduce computationally. Absolute and relative free energies of hydration of these compounds were calculated using the OPLS all-atom and the united-atom GROMOS force fields. Both force fields reproduce the relative free energy of hydration, but the absolute free energies of hydration were only reproduced within k B T when using the recently developed GROMOS parameter set 53A6. Relative free energies of solvation in chloroform could also be reproduced indicating a proper partitioning of the compounds between polar and apolar media. Overall we conclude that it is possible to resolve the amine hydration problem using a simple united-atom force field.
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Validation of the 53A6 GROMOS force field
European Biophysics Journal, 2005Co-Authors: Chris Oostenbrink, Thereza A. Soares, Nico F. A. Vegt, Wilfred F. GunsterenAbstract:The quality of biomolecular dynamics simulations relies critically on the force field that is used to describe the interactions between particles in the system. Force fields, which are generally parameterized using experimental data on small molecules, can only prove themselves in realistic simulations of relevant biomolecular systems. In this work, we begin the validation of the new 53A6 GROMOS parameter set by examining three test cases. Simulations of the well-studied 129 residue protein hen egg-white lysozyme, of the DNA dodecamer d(CGCGAATTCGCG)_2, and a proteinogenic β^3-dodecapeptide were performed and analysed. It was found that the new parameter set performs as well as the previous parameter sets in terms of protein (45A3) and DNA (45A4) stability and that it is better at describing the folding–unfolding balance of the peptide. The latter is a property that is directly associated with the free enthalpy of hydration, to which the 53A6 parameter set was parameterized.
Wilfred F. Gunsteren - One of the best experts on this subject based on the ideXlab platform.
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Biomolecular structure refinement using the GROMOS simulation software
Journal of Biomolecular NMR, 2011Co-Authors: Nathan Schmid, Andreas P Eichenberger, Jane R. Allison, Jožica Dolenc, Anna-pitschna E. Kunz, Wilfred F. GunsterenAbstract:For the understanding of cellular processes the molecular structure of biomolecules has to be accurately determined. Initial models can be significantly improved by structure refinement techniques. Here, we present the refinement methods and analysis techniques implemented in the GROMOS software for biomolecular simulation. The methodology and some implementation details of the computation of NMR NOE data, ^3 J -couplings and residual dipolar couplings, X-ray scattering intensities from crystals and solutions and neutron scattering intensities used in GROMOS is described and refinement strategies and concepts are discussed using example applications. The GROMOS software allows structure refinement combining different types of experimental data with different types of restraining functions, while using a variety of methods to enhance conformational searching and sampling and the thermodynamically calibrated GROMOS force field for biomolecular simulation.
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Validation of the 53A6 GROMOS force field
European Biophysics Journal, 2005Co-Authors: Chris Oostenbrink, Thereza A. Soares, Nico F. A. Vegt, Wilfred F. GunsterenAbstract:The quality of biomolecular dynamics simulations relies critically on the force field that is used to describe the interactions between particles in the system. Force fields, which are generally parameterized using experimental data on small molecules, can only prove themselves in realistic simulations of relevant biomolecular systems. In this work, we begin the validation of the new 53A6 GROMOS parameter set by examining three test cases. Simulations of the well-studied 129 residue protein hen egg-white lysozyme, of the DNA dodecamer d(CGCGAATTCGCG)_2, and a proteinogenic β^3-dodecapeptide were performed and analysed. It was found that the new parameter set performs as well as the previous parameter sets in terms of protein (45A3) and DNA (45A4) stability and that it is better at describing the folding–unfolding balance of the peptide. The latter is a property that is directly associated with the free enthalpy of hydration, to which the 53A6 parameter set was parameterized.
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a biomolecular force field based on the free enthalpy of hydration and solvation the GROMOS force field parameter sets 53a5 and 53a6
Journal of Computational Chemistry, 2004Co-Authors: Chris Oostenbrink, Alessandra Villa, Alan E Mark, Wilfred F. GunsterenAbstract:Successive parameterizations of the GROMOS force field have been used successfully to simulate biomolecular systems over a long period of time. The continuing expansion of computational power with time makes it possible to compute ever more properties for an increasing variety of molecular systems with greater precision. This has led to recurrent parameterizations of the GROMOS force field all aimed at achieving better agreement with experimental data. Here we report the results of the latest, extensive reparameterization of the GROMOS force field. In contrast to the parameterization of other biomolecular force fields, this parameterization of the GROMOS force field is based primarily on reproducing the free enthalpies of hydration and apolar solvation for a range of compounds. This approach was chosen because the relative free enthalpy of solvation between polar and apolar environments is a key property in many biomolecular processes of interest, such as protein folding, biomolecular association, membrane formation, and transport over membranes. The newest parameter sets, 53A5 and 53A6, were optimized by first fitting to reproduce the thermodynamic properties of pure liquids of a range of small polar molecules and the solvation free enthalpies of amino acid analogs in cyclohexane (53A5). The partial charges were then adjusted to reproduce the hydration free enthalpies in water (53A6). Both parameter sets are fully documented, and the differences between these and previous parameter sets are discussed. (C) 2004 Wiley Periodicals, Inc.
Susana Fernandez - One of the best experts on this subject based on the ideXlab platform.
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Results from the validation campaign of the ozone radiometer GROMOS-C at the NDACC station of Réunion island
Atmospheric Chemistry and Physics, 2016Co-Authors: Susana Fernandez, Niklaus Kampfer, Rolf Rüfenacht, Thierry Portafaix, Françoise Posny, Guillaume PayenAbstract:Ozone performs a key role in the middle atmosphere and its monitoring is thus necessary. At the Institute of Applied Physics of the University of Bern, Switzerland, we built a new ground-based microwave radiometer, GROMOS-C (GRound based Ozone MOnitoring System for Campaigns). It has a compact design and can be operated remotely with very little maintenance requirements, being therefore suitable for remote deployments. It has been conceived to measure the vertical distribution of ozone in the middle atmosphere, by observing pressure-broadened emission spectra at a frequency of 110.836 GHz. In addition, meridional and zonal wind profiles can be retrieved, based on the Doppler shift of the ozone line measured in the four directions of observation (north, east, south and west). In June 2014 the radiometer was installed at the Maïdo observatory, on Réunion island (21.2 • S, 55.5 • E). High-resolution ozone spectra were recorded continuously over 7 months. Vertical profiles of ozone have been retrieved through an optimal estimation inversion process, using the Atmospheric Radiative Transfer Simulator ARTS2 as the forward model. The validation is performed against ozone profiles from the Microwave Limb Sounder (MLS) on the Aura satellite, the ozone lidar located at the observatory and with ozone profiles from weekly radiosondes. Zonal and merid-ional winds retrieved from GROMOS-C data are validated against another wind radiometer located in situ, WIRA. In addition, we compare both ozone and winds with ECMWF (European Centre for Medium-Range Weather Forecasts) model data. Results show that GROMOS-C provides reliable ozone profiles between 30 and 0.02 hPa. The comparison with lidar profiles shows a very good agreement at all levels. The accordance with the MLS data set is within 5 % for pressure levels between 25 and 0.2 hPa. GROMOS-C's wind profiles are in good agreement with the observations by WIRA and with the model data, differences are below 5 m s −1 for both.
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GROMOS c a novel ground based microwave radiometer for ozone measurement campaigns
Atmospheric Measurement Techniques, 2015Co-Authors: Susana Fernandez, Axel Murk, Niklaus KampferAbstract:Abstract. Stratospheric ozone is of major interest as it absorbs most harmful UV radiation from the sun, allowing life on Earth. Ground-based microwave remote sensing is the only method that allows for the measurement of ozone profiles up to the mesopause, over 24 hours and under different weather conditions with high time resolution. In this paper a novel ground-based microwave radiometer is presented. It is called GROMOS-C (GRound based Ozone MOnitoring System for Campaigns), and it has been designed to measure the vertical profile of ozone distribution in the middle atmosphere by observing ozone emission spectra at a frequency of 110.836 GHz. The instrument is designed in a compact way which makes it transportable and suitable for outdoor use in campaigns, an advantageous feature that is lacking in present day ozone radiometers. It is operated through remote control. GROMOS-C is a total power radiometer which uses a pre-amplified heterodyne receiver, and a digital fast Fourier transform spectrometer for the spectral analysis. Among its main new features, the incorporation of different calibration loads stands out; this includes a noise diode and a new type of blackbody target specifically designed for this instrument, based on Peltier elements. The calibration scheme does not depend on the use of liquid nitrogen; therefore GROMOS-C can be operated at remote places with no maintenance requirements. In addition, the instrument can be switched in frequency to observe the CO line at 115 GHz. A description of the main characteristics of GROMOS-C is included in this paper, as well as the results of a first campaign at the High Altitude Research Station at Jungfraujoch (HFSJ), Switzerland. The validation is performed by comparison of the retrieved profiles against equivalent profiles from MLS (Microwave Limb Sounding) satellite data, ECMWF (European Centre for Medium-Range Weather Forecast) model data, as well as our nearby NDACC (Network for the Detection of Atmospheric Composition Change) ozone radiometer measuring at Bern.
