Shibistova, O.; Lloyd, J.; Kolle, O.; Arneth, A.; Tchebakova, N.; Zolothukhin, D.; Zrazhevskaya, G.; Schulze, E.-D.: Eddy covariance assessment of CO2 accumulation in mature pine forest (in russian). Doklady Akademii Nauk 383 (3), pp. 425 - 429 (2002)
Shibistova, O.; Lloyd, J.; Zrazhevskaya, G.; Arneth, A.; Kolle, O.; Knohl, A.; Astrakhantceva, N.; Shijneva, I.; Schmerler, J.: Annual ecosystem respiration budget for a Pinus sylvestris stand in central Siberia. Tellus, Series B - Chemical and Physical Meteorology 54 (5), pp. 568 - 589 (2002)
Styles, J. M.; Lloyd, J.; Zolotoukhine, D.; Lawton, K. A.; Tchebakova, N.; Francey, R. J.; Arneth, A.; Salamakho, D.; Kolle, O.; Schulze, E.-D.: Estimates of regional surface carbon dioxide exchange and carbon and oxygen isotope discrimination during photosynthesis from concentration profiles in the atmospheric boundary layer. Tellus, Series B - Chemical and Physical Meteorology 54 (5), pp. 768 - 783 (2002)
Tchebakova, N. M.; Kolle, O.; Zolotoukhine, D.; Arneth, A.; Styles, J. M.; Vygodskaya, N. N.; Schulze, E.-D.; Shibistova, O.; Lloyd, J.: Inter-annual and seasonal variations of energy and water vapour fluxes above a Pinus sylvestris forest in the Siberian middle taiga. Tellus, Series B - Chemical and Physical Meteorology 54 (5), pp. 537 - 551 (2002)
Schierholz, I.; Schäfer, D.; Kolle, O.: The Weiherbach data set: An experimental data set for pesticide model testing on the field scale. Agricultural water management: an international journal 44 (1-3), pp. 43 - 61 (2000)
Valentini, R.; Dore, S.; Marchi, G.; Mollicone, D.; Panfyorov, M.; Rebmann, C.; Kolle, O.; Schulze, E.-D.: Carbon and water exchanges of two contrasting central Siberia landscape types: regenerating forest and bog. Functional Ecology 14 (1), pp. 87 - 96 (2000)
Kalthoff, N.; Fiedler, F.; Kohler, M.; Kolle, O.; Mayer, H.; Wenzel, A.: Analysis of energy balance components as a function of orography and land use and comparison of results with the distribution of variables influencing local climate. Theoretical and Applied Climatology 62 (1-2), pp. 65 - 84 (1999)
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Tchebakova, N. M.; Kolle, O.; Zolotoukhin, D. A.; Lloyd, J.; Arneth, A.; Parfenova, E. I.; Schulze, E.-D.: Annual and seasonal dynamics of energy- and mass exchange in pine forest of middle taiga. In: Forest ecosystems of the Yenisey Meridian, pp. 252 - 264 (Ed. Pleshikov, F. I.). Publishing House of SB RAS, Novosibirsk (2002)
Lloyd, J.; Kolle, O.; Shibistova, O.; Tchebakova, N.; Zolutukin, D.; Arneth, A.; Schulze, E.-D.: The carbon balance of a Siberian forest. In: Proceedings of the International Workshop for advanced flux network and flux evaluation, pp. 39 - 45 (Ed. Inoue, G.). Hokkaido University, Center for global environmental research, Sapporo (2001)
Europe is the fastest warming continent in the world. According to the European Environment Agency’s assessment, many of these risks have already reached critical levels and could become catastrophic without urgent and decisive action.
A new study shows a natural solution to mitigate the effects of climate change such as extreme weather events. Researchers found that a diverse plant community acts as a buffer against fluctuations in soil temperature. This buffer, in turn, can have a decisive influence on important ecosystem processes.
Removing a tonne of CO2 from the air and thus undoing a tonne of emissions? Doesn't quite work, says a study. And provides four objections in view of Earth systems.
The new report by the Global Carbon Project shows: Fossil CO2 emissions will reach a record high in 2023. If emissions remain this high, the carbon budget that remains before reaching the 1.5°C limit will probably be used up in seven years. Although emissions from land use are decreasing slightly, they are still too high to be compensated by renewable forests and reforestation.
Global experts have unveiled the annual 10 New Insights in Climate Science report. The report equips policymakers with the latest and most pivotal climate science research from the previous 18 months, synthesised to help inform negotiations at COP28 and policy implementation through 2024 and beyond.
Storing carbon in the soil can help to mitigate climate change. Soil organic matter bound to minerals in particular can store carbon in the long term. A new study shows that the formation of mineral-associated organic matter depends primarily on the type of mineral, but is also influenced by land use and cultivation intensity.
The international Cabo Verde Atmospheric Observatory (CVAO) is being further expanded: The President of the Republic of Cabo Verde José Maria Neves and German President Frank-Walter Steinmeier laid the foundation stone on Thursday for a new laboratory building on São Vicente, one of the Cape Verde Islands off Africa. The Max Planck Institute for Biogeochemistry was involved in the construction of the station and has since been conducting long-term measurements of the greenhouse gases methane, carbon dioxide and nitrous oxide, among others, at the CVAO.
Researchers at University of California and Max-Planck Institute for Biogeochemistry have created a more accurate model of global carbon cycling. The model better accounts for the contributions of Earth’s terrestrial ecosystems to atmospheric concentrations of the greenhouse gas carbon dioxide, a major source of uncertainty for scientists tallying global emissions.
Vegetation can respond to drought through different mechanisms, including changes in the plants’ structure and physiology. By analyzing state-of-the-art satellite-derived datasets with explainable machine learning methods, an international team around Wantong Li and René Orth showed that the vegetation’s physiology in many ecosystems has deviated from its structure under drought on a global scale.
Carbon sinks on the land surface mitigate the greenhouse effect. An international team of scientists has now determined that the vast majority of Europe’s total above-ground carbon storage is provided by the forests of Eastern Europe. However, this carbon sink has declined, mainly due to changes in land use.