scholarly journals Interactions among Multispheres of the Earth’s System and Polar Regions

Author(s):  
Masaki Kanao
Sensors ◽  
2019 ◽  
Vol 19 (24) ◽  
pp. 5399 ◽  
Author(s):  
Ghassem R. Asrar

A combination of multispectral visible, infra-red and microwave sensors on the constellation of international Earth-observing satellites are providing unprecedented observations for all Earth domains over multiple decades (i.e., atmosphere, land, oceans and polar regions). This Special Issue of Sensors is dedicated to papers that describe such advances in the field of Earth remote sensing and their applications to advance understanding of Earth’s planetary system and applying the resulting knowledge and information to meet the societal needs during recent decades. The papers accepted and published in this issue convey the exciting scientific and technical challenges and opportunities for remote sensing of all domains of Earth system, including terrestrial, aquatic and coastal ecosystems; bathymetry of coasts and islands; oceans and lakes; measurement of soil moisture and land surface temperature that affects both water resources and food production; and advances in use of sun-induced fluorescence (SIF) in measuring and monitoring the contribution of terrestrial vegetation in the cycling of carbon in Earth’s system. Measurements of SIF, for example, has had a profound impact on the field of terrestrial ecosystems research and modelling. The Earth Polychromatic Imaging Camera (EPIC) instrument on the Deep Space Climate Observatory (DSCVR) satellite located at the Sun–Earth Lagrange Point One, about 1.5 million miles away from Earth, is providing unique observations of the Earth’s full sun-lit disk from pole-to-pole and minute-by-minute, which overcomes a major limitation in temporal coverage of Earth by other polar-orbiting Earth-observing satellites. Active and passive microwave remote sensing instruments allow all-weather measurements and monitoring of clouds, weather phenomena, land-surface temperature and soil moisture by overcoming the presence of clouds that affect measurements by visible and infrared sensors. The use of powerful in-space lasers is allowing scientists and engineers to measure and monitor rapidly changing ice sheets in polar regions and mountain glaciers. These sensors and their measurements that are deployed on major space-based observatories and small- and micro-satellites, and the scientific knowledge they provide, are enhancing our understanding of planet Earth and development of Earth system models that are used increasingly to project future conditions due to Earth’s rapidly changing environmental conditions. Such knowledge and information are benefiting people, businesses and governments worldwide.


2013 ◽  
Vol 19 (4(83)) ◽  
pp. 50-56
Author(s):  
A.V. Bespalova ◽  
◽  
A.K. Fedorenko ◽  

Transfers ◽  
2016 ◽  
Vol 6 (3) ◽  
pp. 146-166
Author(s):  
Johannes Görbert ◽  
Russ Pottle ◽  
Jeff Morrison ◽  
Pramod K. Nayar ◽  
Dirk Göttsche ◽  
...  

German Literary Anthropology: Across Cultures, Across Genres Stefan Hermes and Sebastian Kaufmann, eds., Der ganze Mensch – die ganze Menschheit: Völkerkundliche Anthropologie, Literatur und Ästhetik um 1800 (Berlin: de Gruyter, 2014), 318 pp., 10 illustrations, €89.95What’s Old Is New Again, Mostly Julia Kuehn and Paul Smethurst, eds., New Directions in Travel Writing Studies (New York: Palgrave Macmillan, 2015), 325 pp., $90Complex Journeys around the World and through Literary and Intellectual Traditions around 1800 Johannes Görbert, Die Vertextung der Welt: Forschungsreisen als Literatur bei Georg Forster, Alexander von Humboldt und Adelbert von Chamisso. Weltliteraturen/World Literatures, Schriftenreihe der Friedrich Schlegel Graduiertenschule für literaturwissenschaftliche Studien, vol. 7 (Berlin: de Gruyter, 2014), vi, 426 pp., 8 illustrations, €109.95Travel as Cultural Work Gary Totten, African American Travel Narratives from Abroad: Mobility and Cultural Work in the Age of Jim Crow (Amherst: University of Massachusetts Press, 2015), 170 pp., $26.95Colonial Encounters between Africa and Europe—with Special Reference to Austria and Switzerland Manuel Menrath, ed., Afrika im Blick: Afrikabilder im deutschsprachigen Europa, 1870–1970 (Zurich: Chronos, 2012), 329 pp., €43Social Formations and Literary Forms in Long Nineteenth-Century Travel Writing Mary Henes and Brian H. Murray, eds., Travel Writing, Visual Culture and Form, 1760–1900 (London: Palgrave Macmillan, 2016), 248 pp., 21 illustrations, $95Travel Accounts of Polar Regions and Colonial Discourse Mike Frömel, Off ene Räume und gefährliche Reisen im Eis: Reisebeschreibungen über die Polarregionen und ein kolonialer Diskurs im 18. und frühen 19. Jahrhundert (Hannover: Wehrhahn, 2013), 288 pp., €29.50.“Imagined Geographies” and the Navigation of British European Identity Katarina Gephardt, Th e Idea of Europe in British Travel Narratives, 1789–1914 (Burlington, VT: Ashgate, 2014), 248 pp., 15 illustrations, $104.95Terminal and Threshold: Experiencing the Airport Christopher Schaberg, Th e End of Airports (London: Bloomsbury Academic, 2015), 216 pp., 25 illustrations, £13.99NOVEL REVIEW Finding Purity Jonathan Franzen, Purity (New York: Farrar, Straus and Giroux, 2015), 563 pp., $28


1876 ◽  
Vol 10 (6) ◽  
pp. 352-360
Author(s):  
A. E. Nordenskiold
Keyword(s):  

2021 ◽  
Vol 9 (2) ◽  
pp. 317
Author(s):  
Dolors Vaqué ◽  
Julia A. Boras ◽  
Jesús Maria Arrieta ◽  
Susana Agustí ◽  
Carlos M. Duarte ◽  
...  

The ocean surface microlayer (SML), with physicochemical characteristics different from those of subsurface waters (SSW), results in dense and active viral and microbial communities that may favor virus–host interactions. Conversely, wind speed and/or UV radiation could adversely affect virus infection. Furthermore, in polar regions, organic and inorganic nutrient inputs from melting ice may increase microbial activity in the SML. Since the role of viruses in the microbial food web of the SML is poorly understood in polar oceans, we aimed to study the impact of viruses on prokaryotic communities in the SML and in the SSW in Arctic and Antarctic waters. We hypothesized that a higher viral activity in the SML than in the SSW in both polar systems would be observed. We measured viral and prokaryote abundances, virus-mediated mortality on prokaryotes, heterotrophic and phototrophic nanoflagellate abundance, and environmental factors. In both polar zones, we found small differences in environmental factors between the SML and the SSW. In contrast, despite the adverse effect of wind, viral and prokaryote abundances and virus-mediated mortality on prokaryotes were higher in the SML than in the SSW. As a consequence, the higher carbon flux released by lysed cells in the SML than in the SSW would increase the pool of dissolved organic carbon (DOC) and be rapidly used by other prokaryotes to grow (the viral shunt). Thus, our results suggest that viral activity greatly contributes to the functioning of the microbial food web in the SML, which could influence the biogeochemical cycles of the water column.


2021 ◽  
Vol 22 ◽  
pp. 100846
Author(s):  
G.V. Kuznetsov ◽  
K.O. Ponomarev ◽  
D.V. Feoktistov ◽  
E.G. Orlova ◽  
Yu.V. Lyulin ◽  
...  

Molecules ◽  
2021 ◽  
Vol 26 (15) ◽  
pp. 4468
Author(s):  
Yalalt Nyamgerel ◽  
Yeongcheol Han ◽  
Minji Kim ◽  
Dongchan Koh ◽  
Jeonghoon Lee

The triple oxygen isotopes (16O, 17O, and 18O) are very useful in hydrological and climatological studies because of their sensitivity to environmental conditions. This review presents an overview of the published literature on the potential applications of 17O in hydrological studies. Dual-inlet isotope ratio mass spectrometry and laser absorption spectroscopy have been used to measure 17O, which provides information on atmospheric conditions at the moisture source and isotopic fractionations during transport and deposition processes. The variations of δ17O from the developed global meteoric water line, with a slope of 0.528, indicate the importance of regional or local effects on the 17O distribution. In polar regions, factors such as the supersaturation effect, intrusion of stratospheric vapor, post-depositional processes (local moisture recycling through sublimation), regional circulation patterns, sea ice concentration and local meteorological conditions determine the distribution of 17O-excess. Numerous studies have used these isotopes to detect the changes in the moisture source, mixing of different water vapor, evaporative loss in dry regions, re-evaporation of rain drops during warm precipitation and convective storms in low and mid-latitude waters. Owing to the large variation of the spatial scale of hydrological processes with their extent (i.e., whether the processes are local or regional), more studies based on isotopic composition of surface and subsurface water, convective precipitation, and water vapor, are required. In particular, in situ measurements are important for accurate simulations of atmospheric hydrological cycles by isotope-enabled general circulation models.


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