Zerstörungsfreie Bestimmung von Cholesterol und Collagen in arteriosklerotischen Plaques mittels NIR-Spektroskopie

Eine der häufigsten Todesursachen in den Industrieländern ist nach wie vor der Herzinfarkt infolge sklerotischer Veränderungen der Arterien. Moderne bildgebende Verfahren (Ultraschalltechniken, tomographische Verfahren) ermöglichen die Darstellung der Lumenveränderungen in den Arterien, können jedoch die chemische Zusammensetzung einer arteriosclerotischen Ablagerung (Plaque) nicht wiedergeben. Die Kenntnis der Plaquezusammensetzung wäre jedoch ein wichtiges Kriterium für die Einschätzung der Plaquevulnerabilität und könnte somit therapeutische Entscheidungen unterstützen. Ziel unserer Untersuchungen war es nachzuweisen, ob mittels Nahinfrarot-Spektroskopie die Bestimmung von Komponenten der Arterienwand (Cholesterol, Kollagen) möglich ist. Untersucht wurden 82 verschiedene Arterienareale autoptisch gewonnener humaner Aorten und Modellmischungen. Die NIR-Spektren wurden mit einem FT-Spektrophotometer und drei unterschiedlichen Fasersonden (1.: optisches Fenster d=4mm, 2.: d=1mm, 3.: d=400µm mit rechtwinklig zur Faserrichtung austretendem Meßstrahl) aufgenommen. Die chemische Referenzanalytik erfolgte mittels HPLC, die chemometrische Auswertung mit dem PLS (partial least square) Model. Weiterhin wurde die Eindringtiefe des Meßstrahles in das Gewebe untersucht. Unsere Untersuchungen zeigen, daß die NIR-Spektroskopie ein geeignetes Arbeitsmittel für die quantitative Bestimmung von Arterienwandbestandteilen ist. Für die Realisierung von in-vivo-Untersuchungen mit einem entsprechendem NIR-Katheter müssen jedoch noch viele technische Details geklärt werden

Earth Probe Total Ozone Mapping Spectrometer (TOMS) Data Product User's Guide

Two data products from the Earth Probe Total Ozone Mapping Spectrometer (EP/TOMS) have been archived at the Distributed Active Archive Center, in the form of Hierarchical Data Format files. The EP/ TOMS began taking measurements on July 15, 1996. The instrument measures backscattered Earth radiance and incoming solar irradiance; their ratio is used in ozone retrievals. Changes in the reflectivity of the solar diffuser used for the irradiance measurement are monitored using a carousel of three diffusers, each exposed to the degrading effects of solar irradiation at different rates. The algorithm to retrieve total column ozone compares measured Earth radiances at sets of three wavelengths with radiances calculated for different total ozone values. The initial error in the absolute scale for TOMS total ozone is 3 percent, the one standard deviation random error is 2 percent, and the drift is less than 0.5 percent over the first year of data. The Level-2 product contains the measured radiances, the derived total ozone amount, and reflectivity information for each scan position. The Level-3 product contains daily total ozone and reflectivity in a 1-degree latitude by 1.25 degrees longitude grid. Level-3 files containing estimates of LTVB at the Earth surface and tropospheric aerosol information are also available, Detailed descriptions of both HDF data-files and the CD-ROM product are provided

ADEOS Total Ozone Mapping Spectrometer (TOMS) Data Products User's Guide

Two data products from the Total Ozone Mapping Spectrometer (ADEOS/TOMS) have been archived at the Distributed Active Archive Center, in the form of Hierarchical Data Format files. The ADEOS/ TOMS began taking measurements on September 11, 1996, and ended on June 29, 1997. The instrument measured backscattered Earth radiance and incoming solar irradiance; their ratio was used in ozone retrievals. Changes in the reflectivity of the solar diffuser used for the irradiance measurement were monitored using a carousel of three diffusers, each exposed to the degrading effects of solar irradiation at different rates. The algorithm to retrieve total column ozone compares measured Earth radiances at sets of three wavelengths with radiances calculated for different total ozone values, solar zenith angles, and optical paths. The initial error in the absolute scale for TOMS total ozone is 3 percent, the one standard deviation random error is 2 percent, and the drift is less than 0.5 percent over the 9-month data record. The Level 2 product contains the measured radiances, the derived total ozone amount, and reflectivity information for each scan position. The Level 3 product contains daily total ozone and reflectivity in a 1-degree latitude by 1.25 degrees longitude grid. The Level 3 files containing estimates of UVB at the Earth surface and tropospheric aerosol information will also be available. Detailed descriptions of both HDF data files and the CDROM product are provided

Investigating Zonal Asymmetries in Stratospheric Ozone Trends From Satellite Limb Observations and a Chemical Transport Model

This study investigates the origin of a zonal asymmetry in stratospheric ozone trends at northern high latitudes, identified in satellite limb observations over the past two decades. We use a merged data set consisting of ozone profiles retrieved at the University of Bremen from SCIAMACHY and OMPS-LP measurements to derive ozone trends. We also use TOMCAT chemical transport model (CTM) simulations, forced by ERA5 reanalyses, to investigate the factors that drive the asymmetry observed in the long-term changes. By studying seasonally and longitudinally resolved observation-based ozone trends, we find, especially during spring, a well-pronounced asymmetry at polar latitudes with values up to +6 % per decade over Greenland and −5 % per decade over western Russia. The control CTM simulation agrees well with these observed trends, whereas sensitivity simulations indicate that chemical mechanisms involved in the production and removal of ozone, or their changes, are unlikely to explain the observed behavior. The decomposition of TOMCAT ozone time series and ERA5 geopotential height into the first two wavenumber components shows a clear correlation between the two variables in the middle stratosphere and demonstrates a weakening and a shift in the wavenumber-1 planetary wave activity over the past two decades. Finally, the analysis of the polar vortex position and strength points to a decadal oscillation with a reversal pattern at the beginning of the century. The same is found in the ozone trend asymmetry. This further stresses the link between changes in the polar vortex position and the identified ozone trend pattern

Apo(a) isoforms predict risk for coronary heart disease - A study in six populations

Arteriosclerosis, Thrombosis, and Vascular Biology12101214-1226ATVB