Skip to content
  • Submit

  • Category

  • Sort by

  • Per page

Found 2696 publications. Showing page 92 of 270:

Publication  
Year  
Category

Assessment of air quality microsensors versus reference methods: The EuNetAir Joint Exercise – Part II

Borrego, Carlos; Ginja, Joao; Coutinho, Miguel; Ribeiro, Clara; Karatzas, Kostas; Sioumis, Th.; Katsifarakis, Nikos; Konstantinidis, Konstantinos; Vito, Saverio De; Esposito, Elena; Salvato, Maria; Smith, Paul D.; Andre, Nicolas; Gerard, Pierre; Francis, Laurent Alain; Castell, Nuria; Schneider, Philipp; Viana, Mar; Minguillón, María Cruz; Reimringer, Wolfhard; Otjes, Rene; Sicard, Oliver von; Pohle, Roland; Elen, Bart; Suriano, Domenico; Pfister, Valerio; Prato, Mario; Dipinto, S.; Penza, Michèle

2018

Atlantic multidecadal oscillation modulates the impacts of Arctic sea ice decline

Li, Fei; Orsolini, Yvan; Wang, Huijun; Gao, Yongqi; He, Shengping

The Arctic sea ice cover has been rapidly declining in the last two decades, concurrent with a shift in the Atlantic Multidecadal Oscillation (AMO) to its warm phase around 1996/1997. Here we use both observations and model simulations to investigate the modulation of the atmospheric impacts of the decreased sea ice cover in the Atlantic sector of the Arctic (AASIC) by the AMO. We find that the AASIC loss during a cold AMO phase induces increased Ural blocking activity, a southeastward‐extended snowpack, and a cold continent anomaly over Eurasia in December through northerly cold air advection and moisture transport from the Arctic. The increased Ural blocking activity and more extended Eurasian snowpack strengthen the upward propagation of planetary waves over the Siberian‐Pacific sector in the lower stratosphere and hence lead to a weakened stratospheric polar vortex and a negative Arctic Oscillation (AO) phase at the surface in February. However, corresponding to the AASIC loss during a warm AMO phase, one finds more widespread warming over the Arctic and a reduced snowpack over Northern Eurasia in December. The stratosphere‐troposphere coupling is suppressed in early winter and no negative AO anomaly is found in February. We suggest that the cold AMO phase is important to regulate the atmospheric response to AASIC decline, and our study provides insight to the ongoing debate on the connection between the Arctic sea ice and the AO.

2018

Assessing, quantifying and valuing the ecosystem services of coastal lagoons

Newton, Alice; Brito, Ana C.; Icely, John D.; Derolez, Valérie; Clara, Inês; Angus, Stewart; Schernewski, Gerard; Inácio, Miguel; Lillebø, Ana I.; Sousa, Ana Isabel; Béjaoui, Béchir; Solidoro, Cosimo; Tosic, Marko; Cañedo-Argüelles, Miguel; Yamamuro, Masumi; Reizopoulou, Sofia; Tseng, Hsiao-Chun; Donata, Canu; Roselli, Leonilde; Maanan, Mohamed; Cristina, Sónia; Ruiz-Fernández, Ana Carolina; Lima, Ricardo; Kjerfve, Björn; Rubio-Cisneros, Nadia; Perez-Ruzafa, Angel; Marcos, Concepción; Pastres, Roberto; Pranovi, Fabio; Snoussi, Maria; Turpie, Jane; Tuchkovenko, Yurii; Dyack, Brenda; Brookes, Justin; Povilanskas, Ramunas; Khokhlov, Valeriy

The natural conservation of coastal lagoons is important not only for their ecological importance, but also because of the valuable ecosystem services they provide for human welfare and wellbeing. Coastal lagoons are shallow semi-enclosed systems that support important habitats such as wetlands, mangroves, salt-marshes and seagrass meadows, as well as a rich biodiversity. Coastal lagoons are also complex social-ecological systems and the ecosystem services that lagoons deliver provide livelihoods, benefits wellbeing and welfare to humans. This study assessed, quantified and valued the ecosystem services of 32 coastal lagoons. The main findings of the study were: (i) the definitions of ecosystem services are still not generally accepted; (ii) the quantification of ecosystem services is made in many different ways, using different units; (iii) the evaluation in monetary terms of some ecosystem service is problematic, often relying on non-monetary evaluation methods; (iv) when ecosystem services are valued in monetary terms, this may represent very different human benefits; and, (v) different aspects of climate change, including increasing temperature (SST), sea-level rise (SLR) and changes in rainfall patterns threaten the valuable ecosystem services of coastal lagoons.

2018

CITI-SENSE Citizens' Observatories Architecture

Liu, Hai-Ying; Berre, Arne- Jørgen; Kobernus, Michael John; Fredriksen, Mirjam; Rombouts, Richard; Tamlin, Andrei; Cole-Hunter, Tom; Santiago, Leonardo; Bartonova, Alena

This paper introduces the architecture of the CITI-SENSE Citizens’ Observatories based on the ISO 19119 reference model. It describes the various parts of the architecture including boundary services with sensors and apps and data management services with the CITI-SENSE data model. It also describes the Web Feature Service (WFS) storage support and the reusable visualisation widgets used for both apps and web portals in various Citizens’ Observatories.

2018

An aerosol particle containing enriched uranium encountered in the remote upper troposphere

Murphy, D. M.; Froyd, K. D.; Apel, E.; Blake, D.; Evangeliou, Nikolaos; Hornbrook, R. S.; Peischl, J.; Ray, E.; Ryerson, T. B.; Thompson, C.; Stohl, Andreas

2018

Improved optical flow velocity analysis in SO2 camera images of volcanic plumes – implications for emission-rate retrievals investigated at Mt Etna, Italy and Guallatiri, Chile

Gliss, Jonas; Stebel, Kerstin; Kylling, Arve; Sudbø, Aasmund

Accurate gas velocity measurements in emission plumes are highly desirable for various atmospheric remote sensing applications. The imaging technique of UV SO2 cameras is commonly used to monitor SO2 emissions from volcanoes and anthropogenic sources (e.g. power plants, ships). The camera systems capture the emission plumes at high spatial and temporal resolution. This allows the gas velocities in the plume to be retrieved directly from the images. The latter can be measured at a pixel level using optical flow (OF) algorithms. This is particularly advantageous under turbulent plume conditions. However, OF algorithms intrinsically rely on contrast in the images and often fail to detect motion in low-contrast image areas. We present a new method to identify ill-constrained OF motion vectors and replace them using the local average velocity vector. The latter is derived based on histograms of the retrieved OF motion fields. The new method is applied to two example data sets recorded at Mt Etna (Italy) and Guallatiri (Chile). We show that in many cases, the uncorrected OF yields significantly underestimated SO2 emission rates. We further show that our proposed correction can account for this and that it significantly improves the reliability of optical-flow-based gas velocity retrievals.

In the case of Mt Etna, the SO2 emissions of the north-eastern crater are investigated. The corrected SO2 emission rates range between 4.8 and 10.7 kg s−1 (average of 7.1  ±  1.3 kg s−1) and are in good agreement with previously reported values. For the Guallatiri data, the emissions of the central crater and a fumarolic field are investigated. The retrieved SO2 emission rates are between 0.5 and 2.9 kg s−1 (average of 1.3  ±  0.5 kg s−1) and provide the first report of SO2 emissions from this remotely located and inaccessible volcano.

2018

Uptake and effects of 2, 4, 6 - trinitrotoluene (TNT) in juvenile Atlantic salmon (Salmo salar)

Mariussen, Espen; Stornes, Siv Marie; Bøifot, Kari Oline; Rosseland, Bjørn Olav; Salbu, Brit; Heier, Lene Sørlie

Elsevier

2018

Comparison of four inverse modelling systems applied to the estimation of HFC-125, HFC-134a, and SF6 emissions over Europe.

Brunner, D.; Arnold, T.; Henne, S.; Manning, A.; Thompson, R. L.; Maione, M.; O'Doherty, S.; Reimann, S.

2017

Wireless distributed environmental sensor networks for air pollution measurement - The promise and the current reality.

Broday, D. M.; Arpaci, A.; Bartonova, A.; Castell-Balaguer, N.; Cole-Hunter, T.; Dauge, F. R.; Fishbain, B.; Jones, R. L.; Galea, K. S.; Jovasevic-Stojanovic, M.; Kocman, D.; Martinez-Iniguez, T.; Nieuwenhuijsen, M.; Robinson, J.; Svecova, V.; Thai, P.

2017

Publication
Year
Category