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  • 2020-2024  (206)
  • 1935-1939
  • 2021  (206)
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  • 1
    Keywords: Freshwater ecology. ; Marine ecology. ; Biotic communities. ; Population biology. ; Animal culture. ; Conservation biology. ; Ecology . ; Freshwater and Marine Ecology. ; Community and Population Ecology. ; Animal Science. ; Conservation Biology. ; Ecosystems.
    Description / Table of Contents: Introduction. The Lake Charr: Biology, Ecology, Distribution, and Management -- Distribution -- Paleoecology -- Ecological Diversity -- Genetic Diversity -- Habitat -- Movement Ecology and Behavior -- Life History and Population Dynamics -- Trophic Ecology -- Reproduction -- Contaminants and Ecotoxicology -- A General, Life History Based Model for Sustainable Exploitation of Lake Charr across their Range -- Terminology Issues in Lake Charr Early Development.
    Abstract: The lake charr Salvelinus namaycush is a ubiquitous member of cold-water lake ecosystems in previously glaciated regions of northern continental U.S., Alaska, and Canada that often support important commercial, recreational, and subsistence fisheries. The lake charr differs from other charrs by its large size, longevity, iteroparity, top-predator specialization, reduced sexual dimorphism, prevalence of lacustrine spawning, and use of deepwater habitat. The species is remarkably variable in phenotype, physiology, and life history, some of which is reflected in its ecology and genetics, with as many as four morphs or ecotypes co-occurring in a single lake. The lake charr is often the top predator in these systems, but is highly adaptable trophically, and is frequently planktivorous in small lakes. The lake charr by their name highlights their common habitat, lakes both large and small, but often frequents rivers and occasionally moves into the Arctic Ocean. Movement and behaviour of lake charr are motivated by access to cool, well-oxygenated water, foraging opportunities, predator avoidance, and reproduction. Owing to their broad distribution and trophic level, the lake charr serves as a sentinel of anthropogenic change. This volume will provide an up-to-date summary of what is currently known about lake charr from distribution to genetics to physiology to ecology. The book provides a compilation and synthesis of available information on the lake charr, beginning with an updated distribution and a revised treatment of the paleoecology of the species. Understanding of ecological and genetic diversity and movement and behaviour of the species has advanced remarkably since the last major synthesis on the species over 40 years ago. Mid-sections of the book provide detailed accounts of the biology and life history of the species, and later sections are devoted to threats to conservation and fishery management practices used to ensure sustainability. A new standard lake charr-specific terminology is also presented. The book will be a valuable reference text for biologists around the world, ecologists, and fishery managers, and of interest to the angling public.
    Type of Medium: Online Resource
    Pages: XXXVII, 497 p. 107 illus., 71 illus. in color. , online resource.
    Edition: 1st ed. 2021.
    ISBN: 9783030622596
    Series Statement: Fish & Fisheries Series, 39
    DDC: 577.6
    Language: English
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  • 2
    Keywords: Human geography. ; Climatology. ; Public health. ; Human physiology. ; Sustainable architecture. ; Buildings Environmental engineering. ; Human Geography. ; Climate Sciences. ; Public Health. ; Human Physiology. ; Sustainable Architecture/Green Buildings. ; Building Physics, HVAC.
    Description / Table of Contents: Introduction -- Issues in UTCI Calculation from a Decade’s Experience -- Literature Review on UTCI Applications -- Sensitivity of UTCI thermal comfort prediction to personal and situational factors – residual analysis of pedestrian survey data -- Long and short-term acclimatization effects on outdoor thermal perception versus UTCI -- Regional adaptation of the UTCI: Comparisons between different datasets in Brazil -- Outdoor thermal environment and heat-related symptoms of pedestrians: An application of the UTCI for health risk assessment -- Mapping UTCI (in different scales) -- Application of the UTCI in high-resolution urban climate modeling techniques -- The universal thermal climate index as an operational forecasting tool of human biometeorological conditions in Europe -- Proposed framework for establishing a global database for outdoor thermal comfort research -- Afterword.
    Abstract: This book introduces the UTCI (Universal Thermal Climate Index) and summarises progress in this area. The UTCI (Universal Thermal Climate Index) was developed as part of the European COST Action Program and first announced to the scientific community in 2009. Since then a decade has followed of applicability tests and research results as well as knowledge gained from applying the UTCI in human adaptation and thermal perception. These findings are of interest to researchers in the interdisciplinary areas of biometeorology, climatology and urban planning. The book summarizes this progress, discussing the limitations found and provides pointers to future developments. It also discusses UTCI applications in the areas of human biometeorology and urban planning including possibilities of using UTCI and similar indices in climate-responsive urban planning. The book’s message is illustrated with many case studies from the real world. Chapter 10 is available open access under a Creative Commons Attribution 4.0 International License via link.springer.com.
    Type of Medium: Online Resource
    Pages: XII, 228 p. 50 illus., 43 illus. in color. , online resource.
    Edition: 1st ed. 2021.
    ISBN: 9783030767167
    Series Statement: Biometeorology, 4
    DDC: 304.2
    Language: English
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  • 3
    Publication Date: 2023-11-27
    Description: The Martian Moons Exploration (MMX) spacecraft is a JAXA mission to Mars and its moons Phobos and Deimos. MMX will be equipped with the Circum-Martian Dust Monitor (CMDM) which is a newly developed light-weight (650g) large area (1m〈sup〉2〈/sup〉) dust impact detector. Cometary meteoroid streams (also referred to as trails) exist along the orbits of comets, forming fine structures of the interplanetary dust cloud. The streams consist predominantly of the largest cometary particles (with sizes of approximately 100μm to 1 cm) which are ejected at low speeds and remain very close to the comet orbit for several revolutions around the Sun. The Interplanetary Meteoroid Environment for eXploration (IMEX) dust streams in space model is a new and recently published universal model for cometary meteoroid streams in the inner Solar System. We use IMEX to study the detection conditions of cometary dust stream particles with CMDM during the MMX mission in the time period 2024 to 2028. The model predicts traverses of 12 cometary meteoroid streams with fluxes of 100μm and bigger particles of at least 10〈sup〉-3〈/sup〉m〈sup〉-2〈/sup〉day〈sup〉-1〈/sup〉 during a total time period of approximately 90 days. The highest flux of 0.15m〈sup〉-2〈/sup〉day〈sup〉-1〈/sup〉 is predicted for comet 114P/Wiseman-Skiff in October 2026. With its large detection area and high sensitivity CMDM will be able to detect cometary meteoroid streams en route to Phobos. Our simulation results for the Mars orbital phase of MMX also predict the occurrence of meteor showers in the Martian atmosphere which may be observable from the Martian surface with cameras on board landers or rovers. Finally, the IMEX model can be used to study the impact hazards imposed by meteoroid impacts onto large-area spacecraft structures that will be particularly necessary for crewed deep space missions.
    Description: Max Planck Institute for Solar System Research (2)
    Keywords: Comets ; Meteoroid trails ; Meteoroid streams ; Interplanetary dust ; Martian moons ; Phobos ; Deimos ; Martian Moons Exploration ; MMX
    Language: English
    Type: doc-type:article
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  • 4
    Publication Date: 2023-06-29
    Type: Report , NonPeerReviewed
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  • 5
    Publication Date: 2024-02-07
    Description: The Los Chocoyos (14.6°N, 91.2°W) supereruption happened ∼75,000 years ago in Guatemala and was one of the largest eruptions of the past 100,000 years. It emitted enormous amounts of sulfur, chlorine, and bromine, with multi‐decadal consequences for the global climate and environment. Here, we simulate the impact of a Los Chocoyos‐like eruption on the quasi‐biennial oscillation (QBO), an oscillation of zonal winds in the tropical stratosphere, with a comprehensive aerosol chemistry Earth System Model. We find a ∼10‐year disruption of the QBO starting 4 months post eruption, with anomalous easterly winds lasting ∼5 years, followed by westerlies, before returning to QBO conditions with a slightly prolonged periodicity. Volcanic aerosol heating and ozone depletion cooling leads to the QBO disruption and anomalous wind regimes through radiative changes and wave‐mean flow interactions. Different model ensembles, volcanic forcing scenarios and results of a second model back up the robustness of our results.
    Type: Article , PeerReviewed
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  • 6
    Publication Date: 2024-02-07
    Description: Invasive species are co-introduced with microbiota from their native range and also interact with microbiota found in the novel environment to which they are introduced. Host flexibility toward microbiota, or host promiscuity, is an important trait underlying terrestrial plant invasions. To test whether host promiscuity may be important in macroalgal invasions, we experimentally simulated an invasion in a common garden setting, using the widespread invasive macroalga Agarophyton vermiculophyllum as a model invasive seaweed holobiont. After disturbing the microbiota of individuals from native and non-native populations with antibiotics, we monitored the microbial succession trajectories in the presence of a new source of microbes. Microbial communities were strongly impacted by the treatment and changed compositionally and in terms of diversity but recovered functionally by the end of the experiment in most respects. Beta-diversity in disturbed holobionts strongly decreased, indicating that different populations configure more similar –or more common– microbial communities when exposed to the same conditions. This decline in beta-diversity occurred not only more rapidly, but was also more pronounced in non-native populations, while individuals from native populations retained communities more similar to those observed in the field. This study demonstrates that microbial communities of non-native A. vermiculophyllum are more flexibly adjusted to the environment and suggests that an intraspecific increase in host promiscuity has promoted the invasion process of A. vermiculophyllum. This phenomenon may be important among invasive macroalgal holobionts in general.
    Type: Article , PeerReviewed
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  • 7
    Publication Date: 2024-02-07
    Description: This paper presents a modelling study on the fate of CHBr3 and its product gases in the troposphere within the context of tropical deep convection. A cloud-scale case study was conducted along the west coast of Borneo, where several deep convective systems were triggered on the afternoon and early evening of 19 November 2011. These systems were sampled by the Falcon aircraft during the field campaign of the SHIVA project and analysed using a simulation with the cloud-resolving meteorological model C-CATT-BRAMS at 2x2 km resolution that represents the emissions, transport by large-scale flow, convection, photochemistry, and washout of CHBr3 and its product gases (PGs). We find that simulated CHBr3 mixing ratios and the observed values in the boundary layer and the outflow of the convective systems agree. However, the model underestimates the background CHBr3 mixing ratios in the upper troposphere, which suggests a missing source at the regional scale. An analysis of the simulated chemical speciation of bromine within and around each simulated convective system during the mature convective stage reveals that 〉 85% of the bromine derived from CHBr3 and its PGs is transported vertically to the point of convective detrainment in the form of CHBr3 and that the remaining small fraction is in the form of organic PGs, principally insoluble brominated carbonyls produced from the photo-oxidation of CHBr3. The model simulates that within the boundary layer and free troposphere, the inorganic PGs are only present in soluble forms, i.e. HBr, HOBr, and BrONO2, and, consequently, within the convective clouds, the inorganic PGs are almost entirely removed by wet scavenging. We find that HBr is the most abundant PG in background lower-tropospheric air and that this prevalence of HBr is a result of the relatively low background tropospheric ozone levels at the regional scale. Contrary to a previous study in a different environment, for the conditions in the simulation, the insoluble Br-2 species is hardly formed within the convective systems and therefore plays no significant role in the vertical transport of bromine. This likely results from the relatively small quantities of simulated inorganic bromine involved, the presence of HBr in large excess compared to HOBr and BrO, and the relatively efficient removal of soluble compounds within the convective column.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 8
    Publication Date: 2024-02-07
    Description: The communication of current scientific topics with societal relevance to young people is of great importance in order to prepare them adequately for present and future life and to provide them with a solid basis for a sustainable development of society. The scientific, didactic and technical demands for communicating such complex topics in an authentic learning environment in a way that is appropriate to the subject matter and the target audience pose great challenges for scientists and educators allone. This doctoral thesis therefore presents the interdisciplinary development and evaluation of two out-reach activities for secondary grade students in a student laboratory. The students worked out the effects of future changes in the Baltic Sea with hands-on experiments and an interactive computer simulation. Computer simulations and experiments are important learning methods in modern sci-ence education. However, existing research has not sufficiently identified the educational and di-dactical advantages and disadvantages of both methods and often lacks appropriate comparability. The effects of the methods were investigated on knowledge gain, situational interest and beliefs about science first in a direct comparison (NStudy I = 443) and second in a combined approach (NStudy II = 367). The comparative study showed that a simulation conveyed more content knowledge and experi-ments caused higher situational interest. The combined approach indicated that two methods con-veyed more knowledge than one, and the combination of the two methods positively influenced the perceptions of scientific predictions. The results also showed that the students had a fundamentally high level of trust in science. Combinations of experiments and simulation can contribute to a comprehensive understanding of, and interest in com-plex current issues in science, and combine the potential of both media and methods.
    Type: Thesis , NonPeerReviewed
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  • 9
    Publication Date: 2024-02-07
    Description: Investigations of Lateglacial to Early Holocene lake sediments from the Nahe palaeolake (northern Germany) provided a high‐resolution palynological record. To increase the temporal resolution of the record a targeted search for cryptotephra was carried out on the basis of pollen stratigraphy. Three cryptotephra horizons were detected and geochemically identified as G10ka series tephra (a Saksunarvatn Ash), Vedde Ash and Laacher See Tephra. Here we present the first geochemically confirmed finding of the ash from the Laacher See Eruption in Schleswig‐Holstein—extending the so far detected fallout fan of the eruption further to the north‐west. These finds enable direct stratigraphical correlations and underline the potential of the site for further investigations.
    Type: Article , PeerReviewed
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  • 10
    Publication Date: 2024-02-07
    Description: Highlights • The structural inheritance of the Neoproterozoic mobile belts controlled the process of lithospheric rupture of West Gondwana. • This process began and ended around the Borborema and Benin–Nigeria Provinces. • The onset of rifting, and the onset of sea floor spreading are diachronic complex, and spatiotemporal. • At the space domain, six Structural Segments (or groups of marginal basins) were recognized, genetically linked with oceanic transform faults. • At the time domain, five chronological rift stages were recognized as the result of sorting in time thirty-three relevant tectonic related geological events. The Borborema and Benin–Nigeria Provinces are composed of a complex network of Neoproterozoic mobile belts, and large-scale shear zones. The evolution of the South Atlantic Cretaceous Rift System was controlled by the structural inheritance of the Borborema and Benin–Nigeria Provinces. The process of lithospheric rupture began and ended around the Borborema and Benin–Nigeria Provinces, which behaved as a “lithospheric relay ramp” and act as the main obstacle to the opening of the South Atlantic. The onset of rifting, and the onset of sea floor spreading are diachronic complex, and spatiotemporal. At the spatial domain, the basins can be described by groups of marginal basins with genetic links to eleven oceanic transform faults, distributed along three rift branches and twelve rift zones, grouped at six structural segments and aborted rift arms. In the time domain, five chronological rift stages are here identified as the result of sorting 33 “tectonic-related events”, that affect the tectono-stratigraphic record of each one of these basins. Oceanic crust initiation was diachronic with emplacement initiating at three times from south to north: (i) at 130 Ma, seafloor spreading begin south of Florianópolis fracture zone; (ii) after salt deposition (113 Ma), between Florianópolis and Bode Verde fracture zone; and (iii) at the end of Albian (~110 Ma), between Bode Verde and Chain fracture zone, and at the entire Equatorial Branch. Not until the end of Albian (~110 Ma) a full, continuous, and stable mid-ocean ridge was established. The time and space distribution of LIP's and the St. Helena and Tristan da Cunha hotspots trails on the Brazilian side allowed us to corroborate these timings within our model. Upper crustal structures did not play a decisive role in the rift compartmentation at the Equatorial and Orthogonal branches, where lithospheric processes controlled the final plate boundaries.
    Type: Article , PeerReviewed
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