Bild des Monats

Average global distribution of diffuse attenuation coefficient at the excitation wavelength region 390 to 426 nm (Kd(λext)) from Feb until Dec 2007. The diffuse attenuation coefficient is a measure of how deep the sunlight penetrates the ocean. It helps characterizing the underwater light field which is important for estimating the heat budget and primary production in the global oceans. The diffuse attenuation coefficient was derived from three atmospheric satellite sensors SCIAMACHY, GOME-2, and OMI by retrieving vibrational Raman scattering fit factors using Differential Optical Absorption Spectroscopy and converting these to Kd(λext) via Look-up-Tables based on radiative transfer modeling. The standard diffuse attenuation product OC-CCI (Kd490) as obtained from multispectral ocean color satellites was converted to the excitation wavelength region and is shown in comparison. Figure adapted from Oelker et al. (2019).

Recent work at the Institute of Environmental Physics exploits the potential of TROPOMI for ocean applications in a project funded by ESA and led by the Alfred-Wegener-Institute in Bremerhaven (S5POC, https://eo4society.esa.int/projects/sentinel-5pinnovation/). TROPOMI is a satellite sensor on board Sentinel-5P, a recent atmospheric satellite mission launched in October 2017 dedicated for detecting atmospheric trace gases such as ozone and nitrogen dioxide. The possibility to derive diffuse attenuation in the blue and additionally in the ultraviolet region ofthe solar spectrum, as well as the quantification of different phytoplankton groups and the fluorescence signal of phytoplankton will be explored.

Reference:Julia Oelker, Andreas Richter, Tilman Dinter, Vladimir V. Rozanov, John P. Burrows, and Astrid Bracher, "Global diffuse attenuation derived from vibrational Raman scattering detected in hyperspectral backscattered satellite spectra," Opt. Express 27, A829-A855 (2019).

Forschungsmeile 2019

Am 21. und 22. September war es wieder soweit: Im Rahmen der Maritimen Woche 2019 fand an der Weserpromenade „Schlachte“ erneut eine „Forschungsmeile“ statt, natürlich auch diesmal mit IUP-Beteiligung. Die Arbeitsgruppen Physik und Chemie der Atmosphäre und Fernerkundung präsentierten der Öffentlichkeit aktuelle Forschungsergebnisse u.a. zur Beobachtung von Meereis, Luftverschmutzung und Klimagasen durch Satelliten. Neben dem beliebten „Eiswürfelexperiment“ (Wo schmilzt ein Eiswürfel schneller, ins Süßwasser oder Meerwasser?) konnten die Besucher diesmal auch vor Ort die CO2 und Methan-Konzentrationen in ihrem Atem messen. Das herrliche Wetter sorgte für zahlreiche Interessierte, so dass die diesjährige Forschungsmeile für alle Beteiligten als Erfolg gewertet werden kann.

Kontakt: Stefan Noël (stefan.noel@iup.physik.uni-bremen.de)

The September picture of the month shows the modelling of methane dispersion using FLEXPART-WRF.

Methane is an important greenhouse gas. Getting extended knowledge about the sinks and sources is therefore an important task. Modelling the transport of emissions can help a) to plan future measurement campaigns and, b) in combination with measurements, to validate the given emission estimates.

The Upper Silesian Coal Basin is a coal basin in Silesia (Poland, Czech Republic). It contains numerous mines exploiting its large coal reservoirs. When the coal is extracted from the earth, considerable amounts of methane are released, which is extracted from the underground mines and released into the atmosphere through venting shafts. The methane emitted from the Upper Silesian Coal Basin constitutes a regionally significant source.

The fact that the emission takes place at a limited number of well-known locations allows for detailed simulation of the dispersion of the emitted methane in the atmosphere. The latter, combined with measurements of the atmospheric methane concentration,can yield important insight into the emitted quantities.

FLEXPART-WRF is a Lagrangian atmospheric transport model which uses meteorological data (e.g., wind fields) from simulations using the Weather Research and Forecast model WRF. Practically, this means that it allows the simulation of atmospheric transport processes at very small spatial scales of on the order of ~100m.

Figures a) – b) show the simulated methane column enhancement (i.e., ignoring the high methane background of the atmosphere) emitted in Upper Silesia on the morning of 29 May 2018. For Image a) wind fields at a spatial resolution of 1km per grid box were used while b) uses wind fields ata spatial resolution of 200m.

One can see considerably finer structured plumes when using the higher spatial resolution. Even if the general shape of the plumes is comparable in both figures, when taking a closer look one can see that at 1km resolution, the detailed shape of the plume is different (it starts turning northwards earlier, i.e., closer to the emission sources, at 200m resolution).

These high-resolution simulations allow better analysis of methane measurements executed by the airborne MaMap instrument during the CoMet campaign in spring 2018 (ongoing work)

Acknowledgements: All simulations were conducted on the Aether HPC cluster at University of Bremen, financed by DFG within the scope of the Excellence Initiative.

Erste Auswertungen von CMIP6 Modellen mit dem ESMValTool: CO2 im Vergleich zu Beobachtungsdaten

Die Abbildung zeigt die CO2und XCO2 (Säulenmittel des Stoffmengenanteils von CO2 in trockener Luft) Zeitserien von 2003 bis 2014 aus Satellitenbeobachtungen, Stationsdaten und dem Mittel zweier Erdsystemmodelle, die am Coupled Model Intercomparison Project Phase 6 (CMIP6) (Eyring et al. 2016a) teilgenommen haben. Der Satellitendatensatz wurde aus Messungen von SCIAMACHY („SCanning Imaging Absorption Spectrometer for Atmospheric ChartographY“) auf Envisat und TANSO-FTS („Thermal And Near infrared Sensor for carbon Observation - Fourier Transform Spectrometer“) auf GOSAT („Greenhouse gases Observing SATellite“) zusammengesetzt. Die Stationsdaten gehören zum NOAA/ESRL (“National Oceanic and Atmospheric Administration/Earth System Research Laboratory”) Datensatz.

Alle Daten wurden mit dem „Earth System Model Evaluation Tool“, (ESMValTool, Eyring et al. (2016c)) prozessiert. Zur Zeit wird die Veröffentlichung einer neuen Version (v2.0) des ESMValTools vorbereitet, die entwickelt wurde um CMIP6 Daten zu analysieren sobald sie im CMIP6 Archiv veröffentlicht sind. Das ESMValTool enthält eine große Sammlung von Diagnosen und Performance-Tests für Variablen aus Atmosphäre, Ozeans und Land anwendbar auf deren Mittel, Trends und Variabilität. Für die Abbildung wurde mit Hilfe des ESMValTools XCO2 (von den Satellitenbeobachtungen angegebene Messgröße) aus den Modellergebnissen berechnet und ihr Sampling wurde den Beobachtungsdaten entsprechend angepasst. Für einen besseren Vergleich des Jahresganges wurden die Modellergebnisse auf einen Offset zu den Satellitendaten korrigiert.

Modelle und Beobachtungen zeigen den erwarteten Anstieg im CO2-Gehalt der Atmosphäre und den charakteristischen Jahresgang. Dieser ist in der Nordhemisphäre am stärksten ausgeprägt, mit niedrigeren Werten im Sommer, wenn durch die verstärkte Photosynthese CO2 absorbiert wird und hohen Werten im Winter, wenn die Photosynthese zum Erliegen kommt und die Vegetation ihre Kohlenstoffspeicher wieder freisetzt. Die Amplitude des Jahresgangs ist bei Modellen und Beobachtungsdaten unterschiedlich. Gründe für diesen Unterschied und mögliche Änderungen des Jahresgangs in der Zukunft werden im Rahmen des durch die Helmholtz Gesellschaft finanzierten Projektes „Advanced Earth System Model Evaluation for CMIP“ (EVal4CMIP) evaluiert. Änderungen im Jahresgang werden wegen des Effekts der CO2-Düngung erwartet (Wenzel et al. 2016). Zur CO2-Düngung und anderen Wechselwirkungen zwischen CO2-Gehalt und Klima werden im Projekt “Climate-Carbon Interactions in the Coming Century” (CCiCC), finanziert durch das EU Horizon 2020 Program neue „Emergent Constraints“ (Eyring et al. 2019) entwickelt. Zusätzlich umfasst dieses Projekt die Analyse neuer Datensätze sowie Empfehlungen für Modellverbesserungen und Beobachtungsstrategien.

Projekte:

Advanced Earth System Model Evaluation for CMIP (EVal4CMIP)

Climate-Carbon Interactions in the Coming Century (CCiCC)

Coupled Model Intercomparison Project (CMIP)

Publikationen:

Buchwitz, M., Reuter, M., Schneising, O., Noel, S., Gier, B., Bovensmann, H., Burrows, J.P., Boesch, H., Anand, J., Parker, R.J., Somkuti, P., Detmers, R.G., Hasekamp, O.P., Aben, I., Butz, A., Kuze, A., Suto, H., Yoshida, Y., Crisp, D., & O'Dell, C. (2018). Computation and analysis of atmospheric carbon dioxide annual mean growth rates from satellite observations during 2003-2016. Atmospheric Chemistry and Physics, 18

Eyring, V., Bony, S., Meehl, G.A., Senior, C.A., Stevens, B., Stouffer, R.J., & Taylor, K.E. (2016a). Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization. Geoscientific Model Development, 9, 1937-1958

Eyring, V., Cox, P.M., Flato, G.M., Gleckler, P.J., Abramowitz, G., Caldwell, P., Collins, W.D., Gier, B.K., Hall, A.D., Hoffman, F.M., Hurtt, G.C., Jahn, A., Jones, C.D., Klein, S.A., Krasting, J.P., Kwiatkowski, L., Lorenz, R., Maloney, E., Meehl, G.A., Pendergrass, A.G., Pincus, R., Ruane, A.C., Russell, J.L., Sanderson, B.M., Santer, B.D., Sherwood, S.C., Simpson, I.R., Stouffer, R.J., & Williamson, M.S. (2019). Taking climate model evaluation to the next level. Nature Climate Change, 9, 102-110

Eyring, V., Gleckler, P.J., Heinze, C., Stouffer, R.J., Taylor, K.E., Balaji, V., Guilyardi, E., Joussaume, S., Kindermann, S., Lawrence, B.N., Meehl, G.A., Righi, M., & Williams, D.N. (2016b). Towards improved and more routine Earth system model evaluation in CMIP. Earth System Dynamics, 7, 813-830

Eyring, V., Righi, M., Lauer, A., Evaldsson, M., Wenzel, S., Jones, C., Anav, A., Andrews, O., Cionni, I., Davin, E.L., Deser, C., Ehbrecht, C., Friedlingstein, P., Gleckler, P., Gottschaldt, K.D., Hagemann, S., Juckes, M., Kindermann, S., Krasting, J., Kunert, D., Levine, R., Loew, A., Makela, J., Martin, G., Mason, E., Phillips, A.S., Read, S., Rio, C., Roehrig, R., Senftleben, D., Sterl, A., van Ulft, L.H., Walton, J., Wang, S.Y., & Williams, K.D. (2016c). ESMValTool (v1.0) - a community diagnostic and performance metrics tool for routine evaluation of Earth system models in CMIP. Geoscientific Model Development, 9, 1747-1802

Wenzel, S., Cox, P.M., Eyring, V., & Friedlingstein, P. (2016). Projected land photosynthesis constrained by changes in the seasonal cycle of atmospheric CO2. Nature, 538, 499-501

Midlatitude total ozone means were high in 2018, while the tropical values were low compared to the annual means observed in the recent decade as seen in Fig. 1, which shows the annual mean total ozone time series from various merged datasets (five satellite datasets and one based upon groundbased instruments) for the near-global (60°N–60°S) average, tropics, extratropics, and selected months in the polar regions.

For all latitude bands, except the tropics, the average total ozone levels have not yet recovered to the values of the 1970s, a time when ozone losses due to ozone-depleting substances (ODSs) were still very small (WMO 2018). Total ozone is defined as the vertical column amount or in other words the number of ozone molecules above a unit area. Typical units are Dobson units (DU) and the global average column amount is about 300 DU. The lower the ozone column, the higher is the amount of harmful UV radiation reaching the surface that can damage plant cells as well as cause skin cancer.

A recent study by us (Weber et al. 2018a) indicates that total ozone trends since the late 1990s are positive (<1% decade−1) but at most latitudes the trends do not reach statistical significance. Still, the small increase in global total ozone following the significant decline before the 1990s provides proof that the Montreal Protocol and its later Amendments, responsible for phasing out ozone-depleting substances, has been successful. The observed changes in total ozone are reproduced well by state-of-the-art chemistry-transport model calculations that account for changes in transport and for changes in the ozone-depleting substances regulated by the Montreal Protocol (Chipperfield et al. 2018).

In Figure 1 one of the satellite merged data were produced in our institute (GSG dataset) that combines various European sensors (GOME, SCIAMACHY, GOME-2A) that were retrieved with the WFDOAS (weighting function differential absorption spectroscopy) retrievals (Coldewey-Egbers et al., 2005). The European time series started in 1995 and in 2017 and 2018 two new sensors were launched, TROPOMI and GOME-2C, respectively. Both instruments will continue long-term ozone monitoring. In particular TROPOMI provides measurements at an unprecedented spatial resolution corresponding to a foot print of 3.5 km by 7 km at the surface.

Figure 2 shows the total ozone distribution above Antarctica from 1stOctober 2018. In early October the ozone hole reaches its largest extent. In 2018 the size of the ozone hole (defined by values below 220 DU) was higher than the average from recent years. However, the extent of the ozone hole varies from year-to-year depending on the polar meteorology (colder stratospheric winters produce larger ozone holes) as seen in panel e of Fig. 1. Nevertheless, there are signs that spring time total ozone above Antarctica is beginning to recover (Weber et al., 2018, WMO 2018).


References:

Chipperfield, M. P., Dhomse, S., Hossaini, R., Feng, W., Santee, M. L., Weber, M., Burrows, J. P., Wild, J. D., Loyola, D., Coldewey-Egbers, M, 2018: On the Cause of Recent Variations in Lower Stratospheric Ozone. Geophys. Res. Lett., 45, 5718-5726, https://doi.org/10.1029/2018GL078071.

Coldewey-Egbers, M., M. Weber, L. N. Lamsal, R. de Beek, M. Buchwitz, J. P. Burrows, 2005: Total ozone retrieval from GOME UV spectral data using the weighting function DOAS approach.Atmos. Chem. Phys. 5, 5015-5025, https://doi.org/10.5194/acp-5-1015-2005.

Weber, M., Coldewey-Egbers, M., Fioletov, V. E., Frith, S. M., Wild, J. D., Burrows, J. P., Long, C.
S., and Loyola, D., 2018a: Total ozone trends from 1979 to 2016 derived from five merged
observational datasets – the emergence into ozone recovery. Atmos. Chem. Phys., 18, 2097-2117,
https://doi.org/10.5194/acp-18-2097-2018.

Weber, M., Steinbrecht, W., van der A, R., Frith, S. M., Anderson, J., Coldewey-Egbers, M., Davis, S,
Degenstein, D., Fioletov, V., Froidevaux, L., Hubert, D., de Laat, J., Long, C. S., Loyola, D., Sofieva,
V., Tourpali, K., Roth, C., Wang, R., and Wild, J.D., 2018b: Stratospheric ozone [in "State of the
Climate in 2017"], Bull. Amer. Meteor. Soc., 99, S51-S54,
https://doi.org/10.1175/2018BAMSStateoftheClimate.1.

WMO, 2018: World Meteorological Organization/United Nations of Environmental Protection,
Scientific assessment of ozone depletion, 2018. Global Ozone Research and Monitoring Project–
Report No. 58, Geneva, Switzerland, available at https://www.esrl.noaa.gov/csd/assessments/ozone/.

Die Ausdehnung des Meereises um den antarktischen Kontinent herum hat einen ausgeprägten Jahreszyklus: Das Maximum wird normalerweise im September erreicht (am Ende des Südwinters) und das Minimum gegen Ende Februar (am Ende des Südsommers). Das diesjährige Minimum wurde in der letzten Februarwoche erreicht. Nach den Meereisdaten, die am IUP aus Satellitendaten berechnet werden (vom Mikrowellenradiometer AMSR2 auf dem japanischen Satelliten GCOM-W2), war der niedrigste Tageswert der Meereisausdehnung 2,54 Mio. km2 am 23. Februar 2019. Mit Meereisausdehnung meint man die Gesamtfläche aller Satellitenpixel, die mindestens 15% Meereisbedeckung haben.

Der größte Teil des verbleibenden Eises befindet sich, wie gewöhnlich, im Weddellmeer, wo es von der dort vorherrschenden Meeresströmung gegen die Antarktische Halbinsel gedrückt wird (Bild in der Mitte). Das kann man vergleichen mit dem letztjährigen Meereismaximum vom 30. September 2018 (Bild oben). Der jahreszeitliche Unterschied beträgt mehr als 15 Mio km2, das ist 1,5 Mal die Fläche von Europa. Ein Vergleich mit den anderen antarktischen Meereisminima seit Beginn der Satellitenbeobachtungen 1978 (Bild unten) zeigt, dass das diesjährige Minimum zwar niedrig, aber kein Rekord war. Das absolute Minimum, das bisher beobachtet wurde, war 2017. Dennoch: Nach einem im allgemeinen leicht zunehmenden Trend des antarktischen Meereises bis ca. 2013 zeigen die letzten Jahre eine deutliche Abnahme im Sommer wie im Winter.

Publikationen:

Spreen, G., L. Kaleschke, and G.Heygster (2008), Sea ice remote sensing using AMSR-E 89 GHz channels ,vol. 113, C02S03, doi:10.1029/2005JC003384.

AMSR2 ASI sea ice concentration data, Antarctic, version 5.4 (NetCDF) (July 2012 - December 2018). , https://doi.pangaea.de/10.1594/PANGAEA.898400

Projekte:

Sea ice type distribution in the Antarctic from microwave satellite observations (SITAnt), (https://seaice.uni-bremen.de/sitant/)

Ground based Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) observations are a frequently used method to determine atmospheric column amounts of reactive gases such as ozone, nitrogen dioxide or formaldehyde. By probing the atmosphere at different elevation angles, information on the vertical distribution of these absorbers can be determined, as well as on aerosol extinction. In order to extract the profile information from the observations taken at different elevation angles, inversion algorithms are needed which combine a priori information with the information from the measurements.

The Bremen Optimal estimation REtrieval for Aerosols and trace gaseS (BOREAS) is a new, flexible profiling algorithm which combines a non-linear aerosol retrieval module with a trace gas retrieval part. Both Optimal Estimation and Levenberg Marquardt approaches are implemented, and many options for a priori selection and pre-scaling, smoothing constraints, and retrieval modes are implemented. Results from BOREAS have been compared to those from other state of the art retrievals in an extensive study using synthetic data (Frieß et al., 2018) and using measurements during the CINDI-2 campaign (Tirpitz et al., manuscript in preparation) demonstrating the good performance of the algorithm. More details on BOREAS and its validation can be found in Bösch et al., 2018.

References:

Bösch, T., Rozanov, V., Richter, A., Peters, E., Rozanov, A., Wittrock, F., Merlaud, A., Lampel, J., Schmitt, S., de Haij, M., Berkhout, S., Henzing, B., Apituley, A., den Hoed, M., Vonk, J., Tiefengraber, M., Müller, M., and Burrows, J. P.: BOREAS – a new MAX-DOAS profile retrieval algorithm for aerosols and trace gases, Atmos. Meas. Tech., 11, 6833-6859, https://doi.org/10.5194/amt-11-6833-2018, 2018.

Frieß, U., Beirle, S., Alvarado Bonilla, L., Bösch, T., Friedrich, M. M., Hendrick, F., Piters, A., Richter, A., van Roozendael, M., Rozanov, V. V., Spinei, E., Tirpitz, J.-L., Vlemmix, T., Wagner, T., and Wang, Y.: Intercomparison of MAX-DOAS Vertical Profile Retrieval Algorithms: Studies using Synthetic Data, Atmos. Meach. Teech. Discuss., https://doi.org/10.5194/amt-2018-423, in review, 2018.

BLUES - Das Bremer Luftüberwachungssystem https://www.bauumwelt.bremen.de/umwelt/luft/luftqualitaet-24505

Erste Schätzung des CO2-Anstiegs in 2018 mittels Satellitendaten

Kohlenstoffdioxid (CO2) ist ein wichtiges Treibhausgas und steigende atmosphärische Konzentrationen führen zu Erderwärmung. Das IUP der Universität Bremen entwickelt Methoden, um die atmosphärische CO2-Verteilung vom Weltraum aus zu messen.

Das Bild zeigt (a) eine Zeitreihe des vertikal gemittelten CO2-Mischungsverhältnisses („XCO2“) mit vorläufigen Werten für 2018. Wie man sieht, steigt das CO2 nahezu linear an. Grund hierfür ist primär die Verbrennung fossiler Brennstoffe. Die jahreszeitlichen Schwankungen kommen primär durch die Aufnahme und Abgabe von CO2 durch Pflanzen. Die Zeitreihe wurde berechnet aus der von den Satelliten gemessenen räumlichen Verteilung des XCO2 (siehe Karten in (c)). Die Einheit des XCO2 ist ppm (parts per million). 400 ppm bedeutet, dass die Atmosphäre im Mittel 400 CO2 Moleküle pro eine Millionen Luftmoleküle enthält.

Das Bild zeigt in (b) die jährliche Rate des CO2-Anstiegs. Diese schwankt etwas von Jahr zu Jahr. Ein Grund hierfür sind Schwankungen der Stärke natürlicher CO2-Senken, wie z.B. Wälder, oder eine Zunahme der Quellen, wie z.B. Brände. Die gezeigte erste vorläufige Schätzung für 2018 ist 2,5 ppm/Jahr (Unsicherheitsbereich +/- 0,8 ppm/Jahr). Dies ist etwas weniger als in den Jahren 2015 und 2016 (zwei Jahre mit schwächeren Senken und vielen Bränden, teilweise verursacht durch das natürliche Klimaphänomen El Niῆo) aber etwas mehr als in 2017. Zukünftige verfeinerte Analysen werden zeigen, in wie weit sich diese vorläufige Schätzung bestätigt.

Presse:

Copernicus (7-Jan-2019): Pressemitteilung: “Last four years have been the warmest on record – and CO2 continues to rise” URL: https://climate.copernicus.eu/last-four-years-have-been-warmest-record-and-co2-continues-rise

EuroNews (14-Dez-2018): Video: “CO2-Konzentration rekordverdächtig hoch” URL: https://de.euronews.com/2018/12/14/co2-konzentration-rekordverdachtig-hoch

Publikationen:

Buchwitz, M., Reuter, M., Schneising, O., Noel, S., Gier, B., Bovensmann, H., Burrows, J. P., Boesch, H., Anand, J., Parker, R. J., Somkuti, P., Detmers, R. G., Hasekamp, O. P., Aben, I., Butz, A., Kuze, A., Suto, H., Yoshida, Y., Crisp, D., and O'Dell, C., Computation and analysis of atmospheric carbon dioxide annual mean growth rates from satellite observations during 2003-2016, Atmos. Chem. Phys., 18, 17355-17370, https://doi.org/10.5194/acp-18-17355-2018, 2018. URL: https://www.atmos-chem-phys.net/18/17355/2018/

Heymann, J., M. Reuter, M. Buchwitz, O. Schneising, H. Bovensmann, J. P. Burrows, S. Massart, J. W. Kaiser, D. Crisp, CO2 emission of Indonesian fires in 2015 estimated from satellite-derived atmospheric CO2 concentrations, Geophys. Res. Lett., DOI: 10.1002/2016GL072042, pp. 18, 2017. URL: http://onlinelibrary.wiley.com/doi/10.1002/2016GL072042/full

Der linke Teil der Abbildung zeigt die mittlere (2003-2016) saisonale Amplitude vom Säulenmittel des Stoffmengenanteils von CO2in trockener Luft (XCO2) von Satellitenmessungen im Vergleich zu einem multi-Modell Mittel aus 10 gekoppelten Kohlenstoff-Klima Modellen, die am Coupled Model Intercomparison Project Phase 5 (CMIP5) teilgenommen haben. Die Modelldaten wurden entsprechend der Abdeckung der Beobachtungsdaten ausgewählt. Der Satellitendatensatz wurde aus Messungen von SCIAMACHY („SCanning Imaging Absorption Spectrometer for Atmospheric ChartographY“) auf Envisat und TANSO-FTS („Thermal And Near infrared Sensor for carbon Observation - Fourier Transform Spectrometer“) auf GOSAT („Greenhouse gases Observing SATellite“) zusammengesetzt (Buchwitz et al., 2018). Die mittlere saisonale Amplitude ist als Differenz zwischen Minimum und Maximum eines Kalenderjahres der enttrendeten Zeitserie definiert.

Sowohl Modelle als auch Beobachtungsdaten zeigen charakteristische saisonale Zyklen: Im Sommer, wenn die Pflanzen durch Photosynthese Kohlenstoff speichern, ist der CO2-Gehalt in der Atmosphäre geringer. Im Winter kommt die Photosynthese zum Stillstand und beim Verfall von Blättern und Pflanzen setzt die Vegetation ihre Kohlenstoffspeicher wieder frei. Daraus folgt, dass die Schwankung der CO2-Konzentration innerhalb eines Jahres abhängig ist von der Stärke der Photosynthese im Sommer und von der Dauer der Wachstumsphasen der Pflanzen. Diese Schwankungen sind in der Nordhemisphäre größer als in der Südhemisphäre. Eine neue Studie im Journal Nature zeigt: Bei einer Verdopplung des CO2-Gehalts in der Atmosphäre, nimmt die Effektivität der Pflanzen Kohlenstoff über Photosynthese aufzunehmen um etwa ein Drittel zu (Wenzel et al., 2016).

Der rechte Teil der Abbildung basiert auf einer Analyse von Schneising et al. (2014) und zeigt den Einfluss der Temperaturanomalie der Vegetationsperiode auf die saisonale Amplitude für die mittleren Breiten der Nordhemisphäre (30-60°N) für Beobachtungsdaten und das multi-Modell Mittel. Die Temperaturanomalie der Vegetationsperiode ist als Anomalie zur monatlichen Klimatologie gemittelt über die Vegetationsperiode (April – September in der Nordhemisphäre) definiert. Es wurden dabei nur Vegetationsflächen genutzt, die durch die MODIS-Klassifizierung für Bodenbedeckung gekennzeichnet sind. Das multi-Modell Mittel kann sowohl die Korrelation, als auch den negativen Trend der saisonalen Amplitude reproduzieren, den die Beobachtungsdaten zeigen.

Die Analyse der Daten ist Teil des „Advanced Earth System Model Evaluation for CMIP“ (EVal4CMIP) Projektes, finanziert durch die Helmholtz Gesellschaft. Die Daten wurden mit dem Earth System Model Evaluation Tool (ESMValTool, Eyring et al. (2016)) prozessiert und analysiert, ein als open-source Software entwickeltes Diagnose- und Performance-Tool zur systematischen Evaluation von Erdsystemmodellen mit Messdaten.

Projekte:

Advanced Earth System Model Evaluation for CMIP (EVal4CMIP)
Coupled Model Intercomparison Project (CMIP)

Publikationen:

Buchwitz, M., Reuter, M., Schneising, O., Noël, S., Gier, B., Bovensmann, H., Burrows, J.P., Boesch, H.,
Anand, J., Parker, R.J., Somkuti, P., Detmers, R.G., Hasekamp, O.P., Aben, I., Butz, A., Kuze, A., Suto, H., Yoshida, Y., Crosp, D., O'Dell, C.Computation and analysis of atmospheric carbon dioxide annual mean growth rates from satellite observations during 2003-2016. Atmospheric Chemistry and Physics
Discussions, 1-22, doi:10.5194/acp-2018-158, 2018.


Eyring, V., Bony, S., Meehl, G. A., Senior, C. A., Stevens, B., Stouffer, R. J., and Taylor, K. E.: Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization ,
Geosci. Model Dev., 9, 1937-1958, doi:10.5194/gmd-9-1937-2016, 2016a.

Eyring, V., Righi, M., Lauer, A., Evaldsson, M., Wenzel, S., Jones, C., Anav, A., Andrews, O., Cionni, I.,
Davin, E. L., Deser, C., Ehbrecht, C., Friedlingstein, P., Gleckler, P., Gottschaldt, K.-D., Hagemann, S.,
Juckes, M., Kindermann, S., Krasting, J., Kunert, D., Levine, R., Loew, A., Mäkelä, J., Martin, G., Mason,
E., Phillips, A. S., Read, S., Rio, C., Roehrig, R., Senftleben, D., Sterl, A., van Ulft, L. H., Walton, J., Wang, S., and Williams, K. D.: ESMValTool (v1.0) – a community diagnostic and performance metrics tool forroutine evaluation of Earth system models in CMIP , Geosci. Model Dev., 9, 1747-1802, doi:10.5194/gmd-9-1747-2016, 2016b.

Eyring, V., Gleckler, P. J., Heinze, C., Stouffer, R. J., Taylor, K. E., Balaji, V., Guilyardi, E., Joussaume, S., Kindermann, S., Lawrence, B. N., Meehl, G. A., Righi, M., and Williams, D. N.: Towards improved andmore routine Earth system model evaluation in CMIP, Earth Syst. Dynam., 7, 813-830,
doi:10.5194/esd-7-813-2016, 2016c.

Schneising, O., Reuter, M., Buchwitz, M., Heymann, J., Bovensmann, H., and Burrows, J. P., Terrestrial
carbon sink observed from space: variation of growth rates and seasonal cycle amplitudes in
response to interannual surface temperature variability, Atmospheric Chemistry and Physics, 14(1),
133-141, doi:10.5194/acp-14-133-2014, 2014.

Wenzel, S., Cox, P. M., Eyring, V ., and Friedlingstein, P.: Projected land photosynthesis constrained bychanges in the seasonal cycle of atmospheric CO2, Nature, doi: 10.1038/nature19772, 2016.


Text von Veronika Eyring, Bettina Gier und Katja Weigel
Grafik von Bettina Gier

Text: Dr. Nikos Daskalakis and Prof. Mihalis Vrekoussis (LAMOS/IUP)

Image:

a) Easter Island map (a), ozone sonde data and back trajectories:Laura Gallardo, Adolfo HenrÍquez, Anne M. Thompson, Roberto Rondanelli, Jorge Carrasco, Andrea Orfanoz-Cheuquelaf & Patricio Velásquez (2016). The first twenty years (1994–2014) of ozone soundings from Rapa Nui (27°S, 109°W, 51 m a.s.l.), Tellus B: Chemical and Physical Meteorology, 68:1,DOI: 10.3402/tellusb.v68.29484

b) Moai picture (b): Matías Morel [CC BY-SA 4.0 (https://creativecommons.org/licenses/by-sa/4.0)], from Wikimedia Commons

c) Plots (c), (d) and (e): Dr. Nikos Daskalakis (IUP) from original data.

Modelling of the ozone vertical distribution

Introduction-Motivation: Modelling of ozone is a difficult task, since there are no direct ozone emissions. It is a purely secondary pollutant, chemically produced in the atmosphere. The main removal processes consist of chemical transformation and dry deposition. To simulate the vertical distribution of ozone in the troposphere, we need to properly account for both precursor species amounts (CO, NOx etc) and production/removal processes.

For this work, we used the highly documented TM4-ECPL model (Daskalakis et al., ACP, 2016 and references therein). TM4-ECPL is a Chemistry and Transport Model (CTM) with an analytical chemical scheme consisting of ~280 reactions involving 120 tracers (Myriokefalitakis et al., ACP, 2008, 2011). The model is driven by the ERA-Interim meteorology from ECMWF (Dee et al., GMD, 2011) and uses a variety of emissions covering all different sources (anthropogenic, biomass burning, biogenic, marine and soil).

Here we compare the simulated TM4-ECPL ozone concentrationsover the Easter Island (Rapa Nui) to the collocated time series of ozone sondes. Easter Island is chosen as a representative background site of the Southern Pacific region; making such a comparison extremely important for the understanding of the modeled processes. Such a remote location has minimal local anthropogenic impact on ozone precursor levels. This is supported by back trajectories of the region, which show that the air masses reaching the island come mainly from the west, being influenced mostly by the vast ocean (Gallardo et al., Tellus B, 2016).

The model-measurements comparison revealed that the model simulates correctly the seasonality of ozone levels. However, at the same time the comparison also pointed to model’s inability to simulate the tropopause height (panel (e)). The model simulates a higher tropopause affecting this way the mixing of the atmosphere. It manages to capture stratospheric ozone intrusions events that we see from the measurements with higher ozone values well below the tropopause, down to almost 10 km altitude (13 km altitude in the model). To further explain the ozone levels, the impact of long-range transport, wildfires and the El Niño-Southern Oscillation (ENSO) needs to be addressed.

Energie Flüsse interner Wellen südlich der Azoren

Interne Schwerewellen werden im Ozean durch Gezeiten, Wind, und die Wechselwirkung von Meeresströmungen mit der Topographie des Meeresbodens angeregt. Modellrechnungen zeigen einen Eintrag von 0.7–1.3 TW Energie in das interne Wellenfeld durch die Umwandlung von barotropen zu baroklinen Gezeiten an Rücken und untermeerischen Bergen. Der Wind trägt weitere 0.3–1.5 TW Energie in den Ozean ein, von denen der größte Teil allerdings in der oberflächennahen Deckschicht verbleibt, und der Beitrag von wechselwirkenden Strömungen beläuft sich auf 0.2 TW. Global werden 1–2 TW Energie benötigt, um die Schichtung des Ozeans aufrecht zu erhalten. Dies geschieht durch Vermischung durch das Brechen der internen Wellen. Beobachtungen zeigen, dass die Energie für diese Vermischung über Tausende von Kilometern hinweg von niedrig-modigen Internen Wellen nahe der Inertialfrequenz transportiert werden. Hochauflösende globale Ozeanmodelle sind zwar inzwischen teilweise in der Lage, die Energiequellen zu Quantifizieren und die Ausbreitung der niedrig-modigsten Wellen zu berechnen, die Variabilität entlang der Ausbreitungspfade und die Dissipation der Energie muss jedoch parametrisiert werden.

Das Bild zeigt Ergebnisse eines Experiments südlich der Azoren, wo an einer untermeerischen Gebirgskette große Mengen interner Wellen erzeugt werden. Die Wellen verlassen die Erzeugungsregion in einem engen sogenannten 'Gezeitenstrahl', was die Beobachtung der Prozesse an den Wellen erleichtert. Das Schemabild zeigt die Bathymetrie der Erzeugungsregion auf der rechten Seite, sowie in rot/blau die Amplitude der Gezeitenwellen aus Satellitenbeobachtungen. Die Messinstrumente, die wir für die Beobachtung der Energieflüsse verwenden, sind das CTD/LADCP System, das vom Schiff aus verwendet wird, um Zeitreihen Stationen durchzuführen, und eine verankerte Messkette, die Langzeitmessungen von Strömungen und Temperatur aufzeichnet. Die gezeigten Daten sind (unten) ein Ausschnitt aus den Flüssen an der Verankerung, zerlegt in Moden, im Vergleich zu vom Modell vorhergesagten Gezeiten, und (rechts oben) die Signale Interner Wellen in Geschwindigkeit (oben) und Schichtung (unten), jeweils ungefiltert (links), und nach M2 Gezeitenfrequenz gefiltert (rechts).

Projekt:

TRR181 Energy Transfers in Atmosphere and Ocean (https://www.trr-energytransfers.de), Subproject W2: 'Energy transfer through low mode internal waves' Monika Rhein (MARUM/IUP, University of Bremen), Jin-Song von Storch (MPI for Meteorology, Hamburg) DFG

Carbon Dioxide Emissions from Southeast Asian Rivers

How much carbon dioxide (CO2) is released from Southeast Asian rivers? At the Institute of Environmental Physics (IUP), we have investigated this question in close collaboration with the Leibniz Center for Tropical Marine Research (ZMT), Bremen, and with the Swinburne University of Technology in Kuching, Malaysia. Our recent work, supported by the Central Development Research Fund of the University of Bremen, focused on the Rajang River, the longest river in Malaysia on the island of Borneo. It flows through mountainous terrain, tropical rainforests, oil palm plantations and peatlands. Southeast Asian peatlands store large amounts of organic carbon. It is expected that this carbon is released to the adjacent rivers, converted to CO2 and released to the atmosphere from the water surface. However, due to the proximity of the peatlands to the coast, the material is swiftly transported to the ocean, and CO2 emissions from Southeast Asian rivers are actually much lower than predicted. This was confirmed by our research at the Rajang River.

The left images are photographs of our scientists and students at work. The right image displays the measured partial pressure of CO2 (pCO2, in µatm) in the Rajang River. Peat areas are shown in dark colors. It can be seen that pCO2 increases as the river flows through the peat area, but soon decreases towards the river mouth due to mixing with seawater.

Our current knowledge of Southeast Asian river systems is mainly based on these kind of sampling campaigns. They can be realized in short term at relatively low cost and allow to resolve spatial patterns of carbon dynamics in a river. In order to better constrain the temporal variability of carbon fluxes in peat-draining rivers, it would be desirable to have additional long-term monitoring data. A new project, funded by the German Research Foundation (Deutsche Forschungsgemeinschaft, DFG), will look into the use of satellites to monitor the amount of riverine dissolved organic carbon (DOC), which is one of the most important drivers of CO2 emissions.

Related Projects:

‘Integrating field measurements and numerical modeling in order to understand carbon dynamics in Southeast Asian rivers’, awarded to Denise Müller-Dum (IUP), CDRF (Uni Bremen)
‘Studying dissolved organic carbon in tropical rivers of Malaysia using in-situ and satellite observations’, awarded to Justus Notholt (IUP), Thorsten Warneke (IUP), Tim Rixen (ZMT), DFG

Text and Images: Denise Müller-Dum (IUP) and Moritz Müller (Swinburne University of
Technology, Malaysia)

The left panel shows long-term changes in zonal monthly mean ozone in the stratosphere over the 2003-2017 period as a function of altitude and latitude. Values are reported in % per decade and shaded areas indicate non-significant trends. The right panel shows the longitudinally resolved long-term changes at an altitude of 38 km, displaying a remarkable variability. These plots confirm a significant increase of ozone concentration at mid latitudes in the upper stratosphere, whereas, in the middle stratosphere down to 20 km the long-term changesare generally not significant.

The observed increase of ozone concentration around 35-45 km is attributed by recent studies to two main causes; the first one is the decreasing concentration of ozone depleting substances after the production and use of CFCs have been regulated by the Montreal Protocol and its amendments. The second explanation is related to the increasing concentration of greenhouse gases responsible for the recorded global tropospheric warming. Due to radiative processes, this leads to a stratospheric cooling that in turn impacts on the ozone chemistry, increasing its production efficiency at these altitudes. Changes in the stratospheric circulation also have a strong influence on the latitudinal and vertical distribution of ozone and its trends.

In order to obtain a long term record of ozone profiles and study the long-term changes, SCIAMACHY and OMPS Limb Profiler stratospheric ozone data sets have been retrieved and merged at the University of Bremen. Since the overlap of the two satellite missions is only 3 months at the beginning of 2012, a reference time series for the merging has been used. Data from the NASA Aura-MLS instrument have been chosen for this purpose, as the instrument performs limb observations with a broad latitude coverage and it is considered stable and reliable.

Trends have been computed using a multilinear regression model, accounting for all phenomena having a strong impact on stratospheric ozone on different temporal and spatial scale: the solar activity, the quasi-biennial oscillation, El Nino and seasonal terms with a period of 6 and 12 months.

Atmospheric CO2 reaches new high-water mark

Satellite data show that northern hemispheric CO2 has exceeded 410 parts per million (ppm) in April 2018. Globally approximately 407.6 ppm has been reached. These are the highest atmospheric CO2 concentrations since at least 800000 years.

The figure presents time series of atmospheric CO2 mixing ratios for the entire world (black and grey lines), for the northern hemisphere (red) and for the southern hemisphere (green). Shown are monthly mean column-averaged molecular mixing ratios of CO2 (“XCO2”) as retrieved from satellite measurements.

The lines shown in pale colours (recent years) correspond to preliminary time series generated in Near-Real-Time (NRT) whereas the bright colours show a high-quality Climate Data Record (CDR) currently covering the time period 2003-2016.

All curves show an increasing trend due to increasing concentrations of atmospheric CO2 originating primarily from the burning of fossil fuels (coal, oil, gas). The seasonal variations within each year are primarily due to uptake and release of CO2 by vegetation (photosynthesis, respiration, decay of organic matter). As can be seen, the largest variations are over the northern hemisphere (red line), where most of the terrestrial vegetation is located. The northern hemispheric CO2 maximum is typically reached in May. After that CO2 concentrations will decrease because the growing plants will take up large amounts of CO2 from the atmosphere.

The satellite-derived CO2 time series have been generated at the Institute of Environmental Physics (IUP) of the University of Bremen, Germany. They have been derived from spectroscopic measurements of the European satellite instrument SCIAMACHY on Envisat (2002-2012) and from TANSO-FTS onboard the Japanese GOSAT satellite (since 2009).

The underlying retrieval algorithms and corresponding CO2 data products have been generated in the framework of three European projects: the GHG-CCI project of ESA’s Climate Change Initiative and the EU projects Copernicus Climate Change Service (C3S) and Copernicus Atmosphere Monitoring Service (CAMS).

The CAMS data product (pale colours, recent years) is generated in quasi near-real-time at University of Bremen for the European Centre for Medium-Range Weather Forecasts (ECMWF) for CO2 forecasting and other applications within CAMS.

The bright colours show a Climate Data Record (2003-2016) generated at University of Bremen for C3S, which will be extended each year by one additional year. This data product is based on merging several high-quality data products generated in Europe (by University of Bremen, SRON and University of Leicester), in Japan (by the National Institute for Environmental Studies (NIES)) and in the USA (by NASA’s CO2 ACOS team). The merging algorithm has been developed at University of Bremen in order to generate a data product with the highest possible data quality for challenging carbon and climate applications.

The satellite CO2 observations are mean molecular mixing ratios (or mole fractions) of CO2 with respect to dry air averaged over the entire vertical extent of the atmosphere. 410 parts per million means that on average 1 million air molecules (excluding water vapour) contain 410 CO2 molecules in the air above a given location. Note that these column-averaged observations are similar but not identical to CO2 measurements at the surface carried out, for example, by NOAA.

Monitoring of the atmospheric CO2 concentration is important because increasing atmospheric concentrations lead to global warming as CO2 is an important greenhouse gas. Before the industrial revolution, the atmospheric concentration of CO2 was below approximately 280 ppm for at least the last 800000 years. Since then the amount of atmospheric CO2 has increased by more than 40%. The goal of the Paris Agreement on Climate Change is to reduce emissions of greenhouse gases to limit global warming to less than 2 degrees Celsius - or even better to less than 1.5 degrees - with respect to pre-industrial times. Achieving this goal requires a major international effort. It is currently unclear if this goal can be reached.

Text and Images: Michael Buchwitz, Maximilian Reuter, Stefan Noël

April 2018:

Further investigation on megacities: EMeRGe HALO campaign in East Asia

The measurement campaign of the project EMeRGe (Effect of Megacities on the Transport and Transformation of Pollutants on the Regional and Global Scales) in East Asia started in March 2018 and will continue till 09.04.2018.

EMeRGe (http://www.iup.uni-bremen.de/emerge/), led by the Institute of Environmental Physics of the University of Bremen,aims at improving the knowledge and prediction of the transport and transformation patterns of European and Asian pollutant outflows of megacities by using the HALO research aircraft (www.halo.dlr.de). The first measurement campaign in Europe was successfully carried out in summer 2017.

The HALO payload for EMeRGe combines in situ and remote sensing instruments measuring O3and aerosol precursors, aerosol amounts and composition. This information, which is gathered following optimal HALO transects and vertical profiling, enables the investigation of the photochemical evolution of the megacity plumes, the lifetime of the emissions and the transport of the air masses.

For the second EMeRGe campaign in East Asia, HALO left Germany on the 07.03 to reach its airbase in Tainan (Taiwan) where it will stay till the 7.04.2018. Around 140 flight hours will be flown to investigate the transport and transformation of emissions from the megacities Manila, Taipei, Seoul, Tokyo, Beijing, Shanghai and Guangzhou. Already 10 flights have been successfully performed in March 2018.

EMeRGe additionaly stimulates measurements and modelling studies within an international best effort research partnership with the European, Asian, and American science community. More than 50 partners from 16 different countries are participating in EMeRGe international. From them 27 are Asian partners. EMeRGe international facilitates a much more comprehensive integrated analysis of all sets of observational data products (i.e. aircraft, ground and satellite based data) in the study of the transport and transformation of plumes from MPCs.

Text and Images: Lola Andres Hernandez

First NO2 results from the Sentinel-5 Precursor

On October 13, 2017, the Sentinel-5 precursor (S5P), the first of the atmospheric Copernicus instruments was successfully launched into an afternoon low earth orbit. The TROPOMI instrument on-board of this satellite continues the atmospheric remote sensing measurements of the GOME, SCIAMACHY, OMI and GOME-2 instruments. The main data products are O3, NO2, HCHO, CO, CH4 and cloud and aerosol information, but additional data products are possible and are currently being developed at several institutes, including IUP Bremen. Compared to previous instruments, S5P combines global coverage with excellent spatial resolution of 3.5 x 7 km2 (7 x 7 km2 in the SWIR), resulting in an unprecedented level of detail of the derived global maps.

The instrument is still in commissioning phase and official release of operational data is foreseen for July 2018. However, first spectra and lv2 products have already been made available to the core team and validation groups, and so far, data quality appears to be very good. Using the verification algorithms developed over the last years, IUP Bremen has used S5-P radiances and irradiances to produce first maps of CO, CH4, NO2, HCHO, H2O and BrO, all of which show good quality and interesting details.

As an example, data from one S5P overpass over Germany on November 29, 2017 is shown in the figure.

Disclaimer: The presented work has been performed within the framework of the Sentinel-5 Precursor Level 1/Level 2 Product Working Group activities. Results are based on preliminary (not fully calibrated/validated) Sentinel-5 Precursor data that are still subject to change.

Acknowledgement:Sentinel-5 Precursor is a European Space Agency (ESA) mission on behalf of the European Commission (EC). The TROPOMI payload is a joint development by ESA and the Netherlands Space Office (NSO). The Sentinel-5 Precursor ground-segment development has been funded by ESA and with national contributions from The Netherlands, Germany, and Belgium.

Links: http://www.tropomi.eu/

Nachweis von Methanemissionen aus Mülldeponien

Erstmals gelang es Wissenschaftlern des Instituts für Umweltphysik, Methanemissionen von Mülldeponien mittels Flugzeug-gestützter Fernerkundungsmesstechnik unabhängig zu bestimmen.

Fernerkundungsdaten von Methankonzentrationen wurden zusammen mit Daten einer Standardmessmethode während einer Forschungsmeßkampagne in Kalifornien aufgenommen. Durch neue Auswertemethoden und einem Vergleich mit den Daten der Standardmessmethode konnte nun demonstriert werden, dass sich Fernerkundungsdaten zur unabhängigen Überprüfung der berichteten Methanemissionen aus Mülldeponien gut eignen. Im Falle der untersuchten Mülldeponie stimmen die mittels unabhängiger Prüfung bestimmten Emissionen gut mit den berichteten überein.

Während der Meßkampagne in Kalifornien konnten auch Methanemissionen von Ölfeldern bestimmt werden (vgl. auch Bild des Monats April 2015 [LINK]). Diese Forschungsarbeiten fanden kürzlich (Dezember 2017) im ARD Wirtschaftsmagazin PlusMinus Beachtung.

Im Rahmen eines vom BMBF geförderten Projekts arbeiten die Forscher am IUP derzeit an der Entwicklung der nächsten Generation von Methanfernerkundungssensoren, die eine weitaus bessere Meßgenauigkeit zur Quantifizierung von lokalen Methanemissionen haben wird.

Kontakt: heinrich.bovensmann@uni-bremen.de

Publikation:

Krautwurst, S., Gerilowski, K., Jonsson, H. H., Thompson, D. R., Kolyer, R. W., Iraci, L. T., Thorpe, A. K., Horstjann, M., Eastwood, M., Leifer, I., Vigil, S. A., Krings, T., Borchardt, J., Buchwitz, M., Fladeland, M. M., Burrows, J. P., and Bovensmann, H.: Methane emissions from a Californian landfill, determined from airborne remote sensing and in situ measurements, Atmos. Meas. Tech., 10, 3429-3452, https://doi.org/10.5194/amt-10-3429-2017, 2017

Link: https://www.atmos-meas-tech.net/10/3429/2017/

Methanleckagen von Ölfeldern (ARD PlusMinus), Sendung vom 7.12.2017

http://www.daserste.de/information/wirtschaft-boerse/plusminus/sendung/plusminus-erdgasfoerderung100.html

• Bilder des Monats 2020 - 2021
• Bilder des Monats 2018 - 2019
• Bilder des Monats 2016 - 2017
• Bilder des Monats 2014 - 2015