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  • 1
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    Marine Biological Laboratory Archives (Woods Hole, Mass.)
    In:  Viktor Hamburger collection, Box 2, Folder 35, Marine Biological Laboratory Archives
    Publikationsdatum: 2023-01-12
    Beschreibung: Part of To Francis Otto Schmitt from The Schmitty Verein, May 1941
    Beschreibung: Correspondence
    Schlagwort(e): People
    Repository-Name: Woods Hole Open Access Server
    Sprache: Englisch
    Materialart: Text
    Format: image/tiff
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
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    Marine Biological Laboratory (Woods Hole, Mass.)
    In:  Viktor Hamburger Papers, Box 1, Folder 34
    Publikationsdatum: 2023-01-12
    Beschreibung: Handwritten letter, 1 page
    Beschreibung: Work of graduate student
    Beschreibung: Correspondence
    Schlagwort(e): People
    Repository-Name: Woods Hole Open Access Server
    Sprache: Englisch
    Materialart: Text
    Format: image/tiff
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
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    Unbekannt
    Marine Biological Laboratory (Woods Hole, Mass.)
    In:  Viktor Hamburger Papers, Box 1, Folder 34
    Publikationsdatum: 2023-01-12
    Beschreibung: Handwritten letter, 1 page
    Beschreibung: Thank you note for reprints
    Beschreibung: Correspondence
    Schlagwort(e): People ; Publications
    Repository-Name: Woods Hole Open Access Server
    Sprache: Englisch
    Materialart: Text
    Format: image/tiff
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 2019-07-13
    Beschreibung: Simulation of volcanic emissions in climate models requires information that describes the eruption of the emissions into the atmosphere. While the total amount of gases and aerosols released from a volcanic eruption can be readily estimated from satellite observations, information about the source parameters, like injection altitude, eruption time and duration, is often not directly known. The AeroCOM volcanic emissions inventory provides estimates of eruption source parameters and has been used to initialize volcanic emissions in reanalysis projects, like MERRA. The AeroCOM volcanic emission inventory provides an eruptions daily SO2 flux and plume top altitude, yet an eruption can be very short lived, lasting only a few hours, and emit clouds at multiple altitudes. Case studies comparing the satellite observed dispersal of volcanic SO2 clouds to simulations in MERRA have shown mixed results. Some cases show good agreement with observations Okmok (2008), while for other eruptions the observed initial SO2 mass is half of that in the simulations, Sierra Negra (2005). In other cases, the initial SO2 amount agrees with the observations but shows very different dispersal rates, Soufriere Hills (2006). In the aviation hazards community, deriving accurate source terms is crucial for monitoring and short-term forecasting (24-h) of volcanic clouds. Back trajectory methods have been developed which use satellite observations and transport models to estimate the injection altitude, eruption time, and eruption duration of observed volcanic clouds. These methods can provide eruption timing estimates on a 2-hour temporal resolution and estimate the altitude and depth of a volcanic cloud. To better understand the differences between MERRA simulations and volcanic SO2 observations, back trajectory methods are used to estimate the source term parameters for a few volcanic eruptions and compared to their corresponding entry in the AeroCOM volcanic emission inventory. The nature of these mixed results is discussed with respect to the source term estimates.
    Schlagwort(e): Meteorology and Climatology
    Materialart: GSFC-E-DAA-TN20450 , AGU Fall Meeting; Dec 14, 2015 - Dec 18, 2015; San Francisco, CA; United States
    Format: application/pdf
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Publikationsdatum: 2019-07-13
    Beschreibung: Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding mechanisms of global climate change and associated sea-level fluctuations in the past, present and future. The significance of palaeo-ice sheets is further underlined by the broad range of disciplines concerned with reconstructing their behaviour, many of which have undergone a rapid expansion since the 1980s. In particular, there has been a major increase in the size and qualitative diversity of empirical data used to reconstruct and date ice sheets, and major improvements in our ability to simulate their dynamics in numerical ice sheet models. These developments have made it increasingly necessary to forge interdisciplinary links between sub-disciplines and to link numerical modelling with observations and dating of proxy records. The aim of this paper is to evaluate recent developments in the methods used to reconstruct ice sheets and outline some key challenges that remain, with an emphasis on how future work might integrate terrestrial and marine evidence together with numerical modelling. Our focus is on pan-ice sheet reconstructions of the last deglaciation, but regional case studies are used to illustrate methodological achievements, challenges and opportunities. Whilst various disciplines have made important progress in our understanding of ice-sheet dynamics, it is clear that data-model integration remains under-used, and that uncertainties remain poorly quantified in both empirically-based and numerical ice-sheet reconstructions. The representation of past climate will continue to be the largest source of uncertainty for numerical modelling. As such, palaeo-observations are critical to constrain and validate modelling. State-of-the-art numerical models will continue to improve both in model resolution and in the breadth of inclusion of relevant processes, thereby enabling more accurate and more direct comparison with the increasing range of palaeo-observations. Thus, the capability is developing to use all relevant palaeo-records to more strongly constrain deglacial (and to a lesser extent pre-LGM) ice sheet evolution. In working towards that goal, the accurate representation of uncertainties is required for both constraint data and model outputs. Close cooperation between modelling and data-gathering communities is essential to ensure this capability is realised and continues to progress.
    Schlagwort(e): Meteorology and Climatology
    Materialart: GSFC-E-DAA-TN27678 , Quaternary Science Reviews; 125; 15-49
    Format: text
    Standort Signatur Erwartet Verfügbarkeit
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