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  • Books  (5)
  • Printed Books(GFZ-OPAC)  (5)
  • 2020-2024  (5)
  • 1
    Call number: 9/M 07.0421(495)
    In: Special publications / the Geological Society, London, No. 495
    Description / Table of Contents: This volume offers an up-to-date ‘geology-without-borders’ view of the stratigraphy, sedimentology, tectonics and oil-and-gas exploration trends of the entire Atlantic Margin and Barents Sea basin. The challenges associated with data continuity and nomenclature differences across median lines are discussed and mitigated. Examples of under-exploited cross-border plays and discoveries are discussed.
    Type of Medium: Monograph available for loan
    Pages: vi, 320 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 978-1-78620-458-5 , 9781786204585
    ISSN: 0305-8719
    Series Statement: Special publications / the Geological Society, London No. 495
    Language: English
    Note: Contents Acknowledgements Legend for the cover image Chiarella, D., Archer, S. G., Howell, J. A., Jackson, C. A.-L., Kombrink, H. and Patruno, S. / Cross-border subsurface geology in the Atlantic Margin and the Barents Sea: an introduction Tectonic evolution Libak, A., Torabi, A. and Alaei, B. / Normal fault geometric attribute variations with lithology: examples from the Norwegian Barents Sea Anell, I., Indrevær, K. and Serck, C. S. / Influence of structural highs on Triassic deposition on the western Barents Shelf Kristensen, T. B., Rotevatn, A., Marvik, M., Henstra, G. A., Gawthorpe, R. L. and Ravnås, R. / Quantitative analysis of fault-and-fold growth in a transtensional basin: the Sørvestsnaget Basin, Western Barents Sea Trice, R., Hiorth, C. and Holdsworth, R. / Fractured basement play development on the UK and Norwegian rifted margins Millett, J. M., Manton, B. M., Zastrozhnov, D., Planke, S., Maharjan, D., Bellwald, B., Gernigon, L., Faleide, J. I., Jolley, D. W., Walker, F., Abdelmalak, M. M., Jerram, D. A., Myklebust, R., Kjølhamar, B. E., Halliday, J. and Birch-Hawkins, A. / Basin structure and prospectivity of the NE Atlantic volcanic rifted margin: cross-border examples from the Faroe–Shetland, Møre and Southern Vøring basins Stratigraphic, sedimentological and reservoir characterization Jones, G. E. D., Welbon, A. I. F., Mohammadlou, H., Sakharov, A., Ford, J., Needham, T. and Ottesen, C. / Complex stratigraphic fill of a small, confined syn-rift basin: an Upper Jurassic example from offshore mid-Norway Chiarella, D. and Joel, D. / Stratigraphic and sedimentological characterization of the Late Cretaceous post-rift intra Lange Sandstones of the Gimsan Basin and Grinda Graben (Halten Terrace, Norwegian Sea) Walker, F., Schofield, N., Millett, J., Jolley, D., Hole, M. and Stewart, M. / Paleogene volcanic rocks in the northern Faroe–Shetland Basin and Møre Marginal High: understanding lava field stratigraphy Klausen, T. G., Müller, R., Poyatos-Moré, M., Olaussen, S. and Stueland, E. / Tectonic, provenance and sedimentological controls on reservoir characteristics in the Upper Triassic–Middle Jurassic Realgrunnen Subgroup, SW Barents Sea Riis, F. and Wolff, A. / Use of pore pressure data from the Norwegian Continental Shelf to characterize fluid-flow processes in geological timescales Hunt, G. A., Williams, R., Charnock, M. A., Moss, A., Meltveit, J. and Florescu, D. / Geological and petrophysical applications of imaging infrared spectroscopy for mineralogical analysis of core and cuttings: examples from the North Sea, Norwegian Sea and Barents Sea Index
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  • 2
    Call number: 9/M 07.0421(494)
    In: Special publications / the Geological Society, London, No. 494
    Description / Table of Contents: A cross-border approach to exploration, appraisal and development is important in mature basins such as the North Sea, where the ‘low hanging fruit’ have long gone. This approach emphasizes the need to see the basin as one geological entity, in order to maximize economic recovery and prepare the area for the energy transition. This volume offers an up-to-date, ‘geology-without-borders’ view of the stratigraphy, sedimentology, tectonics and oil-and-gas exploration trends of the entire North Sea basin, along with the challenges associated with differences in data continuity and nomenclature across median lines. This volume includes overviews of cross-border play statistics, lithostratigraphic naming conventions and exploration performance through to new facies models for cross-border areas. As such, this volume will be a valuable reference for every geoscientist working in the North Sea for years to come.
    Type of Medium: Monograph available for loan
    Pages: vi, 504 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 978-1-78620-457-8 , 9781786204578
    ISSN: 0305-8719
    Series Statement: Special publications / the Geological Society, London No. 494
    Language: English
    Note: Contents Acknowledgements Archer, S. G., Kombrink, H., Patruno, S., Chiarella, D., Jackson, C. A.-L. and Howell, J. A. / Cross-border petroleum geology in the North Sea: an introduction General North Sea Patruno, S., Kombrink, H. and Archer, S. G. / Cross-border stratigraphy of the Northern, Central and Southern North Sea: a comparative tectono-stratigraphic megasequence synthesis Kombrink, H. and Patruno, S. / The integration of public domain lithostratigraphic data into a series of cross-border North Sea well-penetration maps Quirk, D. G. and Archer, S. G. / Exploration play statistics in the Southern North Sea region of The Netherlands and UK Quirk, D. G. and Archer, S. G. / Exploration play statistics in the central–northern North Sea region of UK–Norway–Denmark Roberts, P., Jordan, O., Steen, Ø., Leppard, C., Janssen, J. S., Baudia, E., Ramm, A. and Helgesen, G. / One North Sea fairway analysis: revealing opportunities through data integration across scales Myers, K., Rouillard, P. and Zanella, E. / Exploration performance in the UK and Norwegian North Sea Quirk, D. G., Underhill, J. R., Gluyas, J. G., Howe, M. J., Wilson, H. A. M. and Anderson, S. A / low-carbon future for The North Sea Basin Paleozoic Boscolo Gallo, A., Kilhams, B., de Keijzer, M. and Nicolai, C. / Can thin coals be resolved in seismic data? An example of the challenges for Carboniferous (Visean to Westphalian) source-rock definition across the Elbow Spit Platform (Netherlands) and the Mid North Sea High (UK) through well synthetic modelling Doornenbal, J. C., Kombrink, H., Bouroullec, R., Dalman, R. A. F., De Bruin, G., Geel, C. R., Houben, A. J. P., Jaarsma, B., Juez-Larré, J., Kortekaas, M., Mijnlieff, H. F., Nelskamp, S., Pharaoh, T. C., Ten Veen, J. H., Ter Borgh, M., Van Ojik, K., Verreussel, R. M. C. H., Verweij, J. M. and Vis, G.-J. / New insights on subsurface energy resources in the Southern North Sea Basin area Daniels, S. E., Tucker, M. E., Mawson, M. J., Holdsworth, R. E., Long, J. J., Gluyas, J. G. and Jones, R. R. / Nature and origin of collapse breccias in the Zechstein of NE England: local observations with cross-border petroleum exploration and production significance, across the North Sea Scisciani, V., Patruno, S., D’Intino, N. and Esestime, P. / Paleozoic basin reactivation and inversion of the underexplored Northern North Sea platforms: a cross-border approach Mesozoic Archer, S. G., McKie, T., Andrews, S. D., Wilkins, A. D., Hutchison, M., Young-Ziolkowski, N., Osunde, C., Matheson, J., Thackrey, S., Lang, M., Sola, B., Mouritzen, C., Perrell, C., Greenwood, M., Mauritzen, E. and Tenepalli, S. / Triassic mudstones of the Central North Sea: cross-border characterization, correlation and their palaeoclimatic significance Gray, E., Hartley, A. and Howell, J. / The influence of stratigraphy and facies distribution on reservoir quality and production performance in the Triassic Skagerrak Formation of the UK and Norwegian Central North Sea Orre, L. T. E. and Folkestad, A. / Depositional environments of the Early to Middle Triassic northern North Sea in a syn-rift to a post-rift setting Galluccio, L., Foote, N., Bertouche, M., Kostic, B. and James, A. / Preliminary assessment of dolomite stringers in the Upper Jurassic Farsund Formation as a potential unconventional hydrocarbon reservoir Cenozoic Pernin, N., Feuilleaubois, L., Bird, T. and Reiser, C. / Identifying and de-risking near-field opportunities through reliable pre-stack broadband attributes: examples from the Paleocene North Sea (UK–Norway) injectites play Karstens, J., Müller, P., Berndt, C. and Patruno, S. / Deep-seated focused fluid migration as indicator for hydrocarbon leads in the East Shetland Platform, North Sea Province Medvedev, S., Hartz, E. H., Schmid, D. W., Zakariassen, E. and Varhaug, P. / Influence of glaciations on North Sea petroleum systems Index
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  • 3
    Monograph available for loan
    Monograph available for loan
    London : Elsevier
    Call number: PIK 23-95529
    Description / Table of Contents: front cover -- Half title -- Title -- Copyright -- Contents -- Contributors -- Acknowledgements -- Chapter 1 Using models to study food systems -- 1.1 Introduction -- 1.2 Models and why we use them -- 1.3 Models in food systems -- 1.4 Types of models used to study food systems -- 1.5 Stage of food production -- 1.5.1 Single stages of the food system -- 1.5.2 Supply chains -- 1.5.3 Broader food systems -- 1.6 Three major types of models -- 1.6.1 Biophysical models -- 1.6.2 Socio-Economic models -- 1.6.3 Participatory modeling -- 1.7 Common issues with models -- 1.8 Organization of this book -- Acknowledgements -- References -- Chapter 2 The origins, definitions and differences among concepts that underlie food systems modeling -- 2.1 Introduction -- 2.2 Origins and definitions of terms -- 2.2.1 Sustainability and related concepts -- 2.2.2 Sustainable development -- 2.2.3 Sustainable agriculture -- 2.3 Systems concepts -- 2.3.1 Food systems -- 2.3.2 Sustainable food systems -- 2.3.3 Systems thinking and modeling -- 2.3.4 Multi-, inter- and transdisciplinary research -- 2.4 Differences between sustainability and resilience and food systems and systems thinking -- 2.4.1 The difference between sustainability and resilience -- 2.4.2 The difference between food systems and systems thinking -- 2.4.3 Systems properties of food systems and their use in modeling -- 2.5 Conclusions -- References -- Chapter 3 Life cycle assessment of food systems and diets -- 3.1 Introduction -- 3.2 A brief history of life cycle assessment -- 3.3 The four phases of LCA -- 3.3.1 Phase 1: goal and scope -- 3.3.2 Phase 2: life cycle inventory (LCI) -- 3.3.3 The problem of multi-functionality -- 3.3.4 Phase 3: life cycle impact assessment (LCIA) -- 3.3.5 Phase 4: interpretation of the assessment -- 3.4 Yogurt case study: LCIA result and interpretation example at midpoint.
    Type of Medium: Monograph available for loan
    Pages: 388 Seiten
    ISBN: 9780128221129
    Language: English
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  • 4
    Call number: AWI Bio-23-95302
    Description / Table of Contents: Climate change of anthropogenic origin is affecting Earth’s biodiversity and therefore ecosystems and their services. High latitude ecosystems are even more impacted than the rest of Northern Hemisphere because of the amplified polar warming. Still, it is challenging to predict the dynamics of high latitude ecosystems because of complex interaction between abiotic and biotic components. As the past is the key to the future, the interpretation of past ecological changes to better understand ongoing processes is possible. In the Quaternary, the Pleistocene experienced several glacial and interglacial stages that affected past ecosystems. During the last Glacial, the Pleistocene steppe-tundra was covering most of unglaciated northern hemisphere and disappeared in parallel to the megafauna’s extinction at the transition to the Holocene (~11,700 years ago). The origin of the steppe-tundra decline is not well understood and knowledge on the mechanisms, which caused shifts in past communities and ecosystems, is of high priority as they are likely comparable to those affecting modern ecosystems. Lake or permafrost core sediments can be retrieved to investigate past biodiversity at transitions between glacial and interglacial stages. Siberia and Beringia were the origin of dispersal of the steppe-tundra, which make investigation this area of high priority. Until recently, macrofossils and pollen were the most common approaches. They are designed to reconstruct past composition changes but have limit and biases. Since the end of the 20th century, sedimentary ancient DNA (sedaDNA) can also be investigated. My main objectives were, by using sedaDNA approaches to provide scientific evidence of compositional and diversity changes in the Northern Hemisphere ecosystems at the transition between Quaternary glacial and interglacial stages. In this thesis, I provide snapshots of entire ancient ecosystems and describe compositional changes between Quaternary glacial and interglacial stages, and confirm the vegetation composition and the spatial and temporal boundaries of the Pleistocene steppe-tundra. I identify a general loss of plant diversity with extinction events happening in parallel of megafauna’ extinction. I demonstrate how loss of biotic resilience led to the collapse of a previously well-established system and discuss my results in regards to the ongoing climate change. With further work to constrain biases and limits, sedaDNA can be used in parallel or even replace the more established macrofossils and pollen approaches as my results support the robustness and potential of sedaDNA to answer new palaeoecological questions such as plant diversity changes, loss and provide snapshots of entire ancient biota.
    Description / Table of Contents: Der vom Menschen verursachte Klimawandel wirkt sich auf die biologische Vielfalt der Erde und damit auf die Ökosysteme und ihre Leistungen aus. Die Ökosysteme in den hohen Breitengraden sind aufgrund der verstärkten Erwärmung an den Polen noch stärker betroffen als der Rest der nördlichen Hemisphäre. Dennoch ist es schwierig, die Dynamik von Ökosystemen in den hohen Breitengraden vorherzusagen, da die Wechselwirkungen zwischen abiotischen und biotischen Komponenten sehr komplex sind. Da die Vergangenheit der Schlüssel zur Zukunft ist, ist die Interpretation vergangener ökologischer Veränderungen möglich, um laufende Prozesse besser zu verstehen. Im Quartär durchlief das Pleistozän mehrere glaziale und interglaziale Phasen, welche die Ökosysteme der Vergangenheit beeinflussten. Während des letzten Glazials bedeckte die pleistozäne Steppentundra den größten Teil der unvergletscherten nördlichen Hemisphäre und verschwand parallel zum Aussterben der Megafauna am Übergang zum Holozän (vor etwa 11 700 Jahren). Der Ursprung des Rückgangs der Steppentundra ist nicht gut erforscht, und die Kenntnis über die Mechanismen, die zu den Veränderungen in den vergangenen Lebensgemeinschaften und Ökosystemen geführt haben, ist von hoher Priorität, da sie wahrscheinlich mit denen vergleichbar sind, die sich auf moderne Ökosysteme auswirken. Durch die Entnahme von See- oder Permafrostkernsedimenten kann die vergangene Artenvielfalt an den Übergängen zwischen Eis- und Zwischeneiszeiten untersucht werden. Sibirien und Beringia waren der Ursprung der Ausbreitung der Steppentundra, weshalb die Untersuchung dieses Gebiets hohe Priorität hat. Bis vor kurzem waren Makrofossilien und Pollen die gängigsten Methoden. Sie dienen der Rekonstruktion vergangener Veränderungen in der Zusammensetzung der Bevölkerung, haben aber ihre Grenzen und Schwächen. Seit Ende des 20. Jahrhunderts kann auch sedimentäre alte DNA (sedaDNA) untersucht werden. Mein Hauptziel war es, durch den Einsatz von sedaDNA-Ansätzen wissenschaftliche Beweise für Veränderungen in der Zusammensetzung und Vielfalt der Ökosysteme der nördlichen Hemisphäre am Übergang zwischen den quartären Eiszeiten und Zwischeneiszeiten zu liefern. In dieser Arbeit liefere ich Momentaufnahmen ganzer alter Ökosysteme und beschreibe die Veränderungen in der Zusammensetzung zwischen Quartärglazialen und Interglazialen und bestätige die Vegetationszusammensetzung sowie die räumlichen und zeitlichen Grenzen der pleistozänen Steppentundra. Ich stelle einen allgemeinen Verlust der Pflanzenvielfalt fest, wobei das Aussterben der Pflanzen parallel zum Aussterben der Megafauna verlief. Ich zeige auf, wie der Verlust der biotischen Widerstandsfähigkeit zum Zusammenbruch eines zuvor gut etablierten Systems führte, und diskutiere meine Ergebnisse im Hinblick auf den laufenden Klimawandel. Mit weiteren Arbeiten zur Eingrenzung von Verzerrungen und Grenzen kann sedaDNA parallel zu den etablierteren Makrofossilien- und Pollenansätzen verwendet werden oder diese sogar ersetzen, da meine Ergebnisse die Robustheit und das Potenzial von sedaDNA zur Beantwortung neuer paläoökologischer Fragen wie Veränderungen der Pflanzenvielfalt und -verluste belegen und Momentaufnahmen ganzer alter Biota liefern.
    Type of Medium: Dissertations
    Pages: vi, 217 Seiten , Illustrationen, Diagramme, Karten
    Language: English
    Note: Dissertation, Universität Potsdam, 2023 , TABLE OF CONTENTS Acknowledgements Summary Zusammenfassung 1 General introduction 1.1 A changing world 1.1.1 Global changes of anthropogenic origin 1.1.2 Amplified crisis in the high latitudes 1.2 The past is the key to the future 1.2.1 The Quaternary glacial and interglacial stages 1.2.2 The Beringia study case 1.3 Investigating past biodiversity 1.3.1 Traditional tools 1.3.2 Newest sedaDNA proxies 1.4 Motivation and aims of the thesis 1.5 Structure of the thesis 1.6 Author’s contributions 2 Manuscript I 2.1 Abstract 2.2 Introduction 2.3 Materials and Methods 2.3.1 Geographical settings 2.3.2 Fieldwork and subsampling 2.3.3 Core splicing and dating 2.3.4 Sediment-geochemical analyses 2.3.5 Pollen analysis 2.3.6 Molecular genetic preparation 2.3.7 Processing of sedaDNA data 2.3.8 Statistical analysis and visualization 2.4 Results 2.4.1 Age model 2.4.2 Sediment-geochemical core composition 2.4.3 Pollen stratigraphy 2.4.4 sedaDNA composition 2.4.5 Comparison between pollen and sedaDNA 2.4.6 Taxa richness investigation 2.5 Discussion 2.5.1 Proxy validation 2.5.2 Vegetation compositional changes in response to climate inferred from pollen and sedaDNA records 2.5.3 The steppe-tundra of the Late Pleistocene 2.5.4 The disrupted Pleistocene-Holocene transition 2.5.5 The boreal forest of the Holocene 2.5.6 Changes in vegetation richness through the Pleistocene/Holocene transition inferred from the sedaDNA record 2.6 Conclusion Data availability statement Funding References 3 Manuscript II 3.1 Abstract 3.2 Introduction 3.3 Material and Method 3.3.1 Site description and timeframe 3.3.2 Sampling, DNA extraction and PCR 3.3.3 Filtering and cleaning dataset 3.3.4 Identification of taxa – species signal 3.3.5 Resampling 3.3.6 Assessment of the species pool stability 3.3.7 Quantification of extinct and extirpated taxa 3.3.8 Characterisation of species and candidate species 3.4 Results 3.4.1 Changes in the composition and species pool at the Pleistocene - Holocene transition 3.4.2 Decrease in the regional plant species richness between the Pleistocene and the Holocene 3.4.3 Identification of loss taxa events 3.4.4 Characterisation of lost taxa 3.5 Discussion 3.5.1 Biotic and abiotic changes in the ecosystem - a cocktail for extinction 3.5.2 Identification and quantification of potential plant taxa loss 3.5.3 Characterisation of potential taxa loss 3.5.4 Limits of the method 3.5.5 Conclusions and perspectives Funding References 4 Manuscript III 4.1 Abstract 4.2 Introduction 4.3 Material & Methods 4.3.1 Fieldwork and subsampling 4.3.2 Chronology 4.3.3 Pollen analysis 4.3.4 Isolation of sedimentary ancient DNA 4.3.5 Metabarcoding approach 4.3.6 Shotgun approach 4.3.7 Bioinformatic processing 4.4 Results 4.4.1 General results of the three approaches: pollen, metabarcoding and shotgun sequencing 4.4.2 Plants (Viridiplantae) 4.4.3 Fungi 4.4.4 Mammals (Mammalia) 4.4.5 Birds (Aves) 4.4.6 Insects (Insecta) 4.4.7 Prokaryotes (Bacteria, Archaea) and Viruses 4.5 Discussion 4.5.1 Interglacial communities 4.5.2 Glacial communities 4.5.3 Potential and limitations of the sedaDNA shotgun approach applied to ancient permafrost sediments 4.6 Conclusions Data availability statement Funding References 5 Synthesis 5.1 Ecological changes between glacial and interglacial stages 5.1.1 Changes in the compositional structure 5.1.2 Loss of plant diversity 5.1.3 Potential drivers of change 5.2 High potential of sedaDNA for past biodiversity reconstruction 5.3 Conclusions and future perspectives Bibliography Appendices Appendix 1: Supplementary material for Manuscript I Appendix 2: Supplementary material for Manuscript II Appendix 3: Supplementary material for Manuscript III Appendix 4: Manuscript IV Eidesstattliche Erklärung
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  • 5
    Call number: M 20.93963
    In: Advances in global change research, Volume 69
    Description / Table of Contents: This book offers a complete overview of the measurement of precipitation from space, which has made considerable advancements during the last two decades. This is mainly due to the Tropical Rainfall Measuring Mission (TRMM), the Global Precipitation Measurement (GPM) mission, CloudSat and a carefully maintained constellation of satellites hosting passive microwave sensors. The book revisits a previous book, Measuring Precipitation from Space, edited by V. Levizzani, P. Bauer and F. J. Turk, published with Springer in 2007. The current content has been completely renewed to incorporate the advancements of science and technology in the field since then. This book provides unique contributions from field experts and from the International Precipitation Working Group (IPWG). The book will be of interest to meteorologists, hydrologists, climatologists, water management authorities, students at various levels and many other parties interested in making use of satellite precipitation data sets.
    Type of Medium: Monograph available for loan
    Pages: xciii, 453-1176 Seiten , Illustrationen
    ISBN: 9783030357986
    Series Statement: Advances in Global Change Research 69
    Language: English
    Note: SECTION 4 Validation: Chapter 25. The IPWG satellite precipitation validation effort -- Chapter 26. The GPM Ground Validation Program -- Chapter 27. The GPM DPR Validation Program -- Chapter 28. Error and uncertainty characterization -- Chapter 29. Multiscale evaluation of satellite precipitation products: Effective resolution of IMERG -- Chapter 30. Remote sensing of orographic precipitation -- Chapter 31. Integrated multi-satellite evaluation for the Global Precipitation Measurement: Impact of precipitation types on spaceborne precipitation estimation -- Chapter 32. Hydrologic validation and flood analysis -- Chapter 33. Global-scale evaluation of 22 precipitation datasets using gauge observations and hydrological modeling -- Chapter 34. OceanRAIN – The global ocean surface-reference dataset for characterization, validation and evaluation of the water cycle -- SECTION 5 Observed Characteristics of Precipitation: Chapter 35. GPCP and the global characteristics of precipitation -- Chapter 36. Global snowfall detection and measurement -- Chapter 37. Snowfall detection by spaceborne radars -- Chapter 38. On the duration and lifecyle of precipitation systems in the tropics -- Chapter 39. Observational characteristics of warm-type heavy rainfall -- Chapter 40. Satellite precipitation measurement and extreme rainfall -- Chapter 41. Rainfall trends in East Africa from an ensemble of IR-based satellite products -- Chapter 42. Heavy precipitation systems in the Mediterranean area: The role of GPM -- Chapter 43. Dryland precipitation climatology from satellite observations -- Chapter 44. Haifall detection -- Chapter 45. Improving high-latitude and cold region precipitation analysis -- Chapter 46. Latent heating retrievals from satellite observations -- SECTION 6 Applications: Chapter 47. Operational applications of Global Precipitation Measurement observations -- Chapter 48. Assimilation of precipitation observations from space into numerical weather prediction (NWP) -- Chapter 49. Precipitation ensemble data assimilation in NWP models -- Chapter 50. PERSIANN-CDR for hydrology and hydro-climatic applications -- Chapter 51. Soil moisture and precipitation: The SM2RAIN algorithm for rainfall retrieval from satellite soil moisture -- Chapter 52. Drought risk management using satellite-based rainfall estimates -- Chapter 53. Two decades of urban hydroclimatological studies have yielded discovery and societal benefits -- Chapter 54. Validation of climate models -- Chapter 55. Extreme precipitation in the Himalayan landslide hotspot -- Chapter 56. The value of satellite rainfall estimates in agriculture and food security -- Chapter 57. Using satellite estimates of precipitation for fire danger rating -- Chapter 58. Variability of satellite sea surface salinity under rainfall.
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