G. Civitarese

ORCID: 0000-0002-4572-6177
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About
Contact & Profiles
Research Areas
  • Marine and coastal ecosystems
  • Oceanographic and Atmospheric Processes
  • Marine Biology and Ecology Research
  • Geology and Paleoclimatology Research
  • Isotope Analysis in Ecology
  • Marine and environmental studies
  • Ocean Acidification Effects and Responses
  • Marine and fisheries research
  • Arctic and Antarctic ice dynamics
  • Methane Hydrates and Related Phenomena
  • Climate variability and models
  • Tropical and Extratropical Cyclones Research
  • Marine Invertebrate Physiology and Ecology
  • Scientific Research and Discoveries
  • Maritime and Coastal Archaeology
  • Microbial Community Ecology and Physiology
  • Offshore Engineering and Technologies
  • Marine Bivalve and Aquaculture Studies
  • Groundwater and Isotope Geochemistry
  • Protist diversity and phylogeny
  • Ocean Waves and Remote Sensing
  • Geological Studies and Exploration
  • Potato Plant Research
  • Mine drainage and remediation techniques
  • Plant Ecology and Soil Science

National Institute of Oceanography and Applied Geophysics
2013-2024

Istituto di Scienze Marine del Consiglio Nazionale delle Ricerche
2000-2005

Istituto Sperimentale Agronomico
1999-2003

University of Southampton
2000

Instytut Oceanologii Polskiej Akademii Nauk
2000

Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
2000

University of Trieste
1997

Massachusetts Institute of Technology
1996

In 1997 an inversion in the Ionian upper‐layer circulation was documented and ascribed to a massive inflow of Aegean dense waters associated with Eastern Mediterranean Transient (EMT) not wind‐stress (Borzelli et al., 2009). Here we generalize concept hypothesizing that such inversions are possible even absence influence. Indeed, salinity density data collected Southern Adriatic, main source deep water, show decadal variations coherent changes sea level height northern Ionian. Scaling...

10.1029/2010gl043216 article EN Geophysical Research Letters 2010-05-01

Abstract. Analysis of 20-year time-series the vertically averaged salinity and nutrient data in Southern Adriatic shows that two parameters are subject to strong decadal variability. In addition, it is documented variations out phase. Nutrients Ionian vary parallel except generally content lower than Ionian, a fact has been attributed primary producer consumption following winter convective mixing. As shown earlier, North Gyre (NIG) changes its circulation sense on scale due Bimodal...

10.5194/bg-7-3987-2010 article EN cc-by Biogeosciences 2010-12-15

In the Arctic Ocean, Pacific source water can be distinguished from Atlantic by nitrate‐phosphate concentration relationships, with having higher phosphate concentrations relative to those of nitrate. Furthermore, water, originally inflow through Bering Strait, is clearly recognizable in outflows low‐salinity waters Ocean northern North Canadian Archipelago and Fram Strait. Archipelago, we observe that almost all flowing Lancaster Jones sounds, most top 100 m Smith Sound (containing flow...

10.1029/2001jc001141 article EN Journal of Geophysical Research Atmospheres 2003-04-01

[1] We study the impact of decadal inversions Ionian upper layer circulation (denominated as Adriatic-Ionian Bimodal Oscillation System) on thermohaline properties Levantine and Cretan Seas. Lagrangian drifter data surface geostrophic currents show that Atlantic Water (AW) flow is well organized most intense when cyclonic. During anticyclonic phase, AW spreading pathway longest, contributing to its prolonged mixing higher salinity once it reaches Levantine. Thus, basin subject less dilution...

10.1029/2011jc007280 article EN Journal of Geophysical Research Atmospheres 2011-09-21

Maps of the remotely sensed Absolute Dynamic Topography (ADT) and Sea Surface Temperature (SST) over Eastern Mediterranean in period June 1993 to 2001 show a dramatic sudden change sea surface structure. This change, which is presumably associated with relaxation Transient (EMT), had taken place by middle 1997 consisted complete reversal Ionian upper‐layer circulation from anticyclonic cyclonic. In EMT phase, SST ADT maps suggest enhanced communication between Aegean basins as well waters...

10.1029/2009gl039261 article EN Geophysical Research Letters 2009-08-12

Abstract. The Mediterranean Sea (MedSea) is considered a "laboratory basin" being an ocean in miniature, suffering dramatic changes its oceanographic and biogeochemical conditions derived from natural anthropogenic forces. Moreover, the MedSea prone to absorb store carbon due particular CO2 chemistry active overturning circulation. Despite this, water column measurements covering whole basin are scarce. This work aims be base-line for future studies about system space-time variability...

10.5194/os-10-69-2014 article EN cc-by Ocean science 2014-02-14

Abstract. Adriatic and Ionian seas are Mediterranean sub-basins linked through the Bimodal Oscillating System mechanism responsible for decadal reversals of basin-wide circulation. Altimetric maps showed that last cyclonic mode started in 2011 but unexpectedly 2012 reversed to anticyclonic. We related this "premature" inversion extremely strong winter 2012, which caused formation very dense waters, flooding flanks May inverting bottom pressure gradient. Using Lagrangian float measurements,...

10.5194/os-10-513-2014 article EN cc-by Ocean science 2014-06-23

The Mediterranean is a marginal sea displaying peculiar biogeochemistry (enhanced deep respiration, non Redfieldian nutrient ratios, etc.). Here we discuss the different processes that may contribute to observed peculiarities, inferred from analysis of data generated mostly during last decade. Both nitrate orthophosphate (N:P) and orthosilicate (Si:N) ratios display decreasing east‐west gradient (N:P > 25 Si:N 1.3 in eastern Mediterranean, N:P ∼ 20 ≤ 1.0 western Mediterranean). transports...

10.1029/2002jc001650 article EN Journal of Geophysical Research Atmospheres 2003-09-01

Abstract. Previous studies have demonstrated that the salinity in Levantine basin depends on intensity of Atlantic water (AW) inflow. Moreover, its spreading eastward (to basin) or northward Ionian Sea) is determined by circulation pattern, i.e. Adriatic–Ionian Bimodal Oscillating System (BiOS) mechanism. The aim this paper to relate variations salt content variability core Intermediate Water (LIW) passing through Sicily Channel (SC) and possible impact Western Mediterranean Transition – WMT...

10.5194/os-9-83-2013 article EN cc-by Ocean science 2013-01-29

Abstract Under the emerging features of interannual-to-decadal ocean variability, periodical reversals North Ionian Gyre (NIG), driven mostly by mechanism named Adriatic-Ionian Bimodal Oscillating System (BiOS), are known as impacting on marine physics and biogeochemistry potentially influencing short-term regional climate predictability in Eastern Mediterranean. Whilst it has been suggested that local wind forcing cannot explain such aspects alternative hypothesis indicating NIG mainly...

10.1038/s41598-020-57862-6 article EN cc-by Scientific Reports 2020-02-05

The Mediterranean Sea presents several biogeochemical anomalies compared to the global ocean. An unbalanced N budget, high nitrate/phosphate ratios in subsurface waters and low 15 N/ 14 particulate dissolved nitrogen suggest a significant occurrence of 2 fixation. This study presents, for first time, basin‐wide overview direct measurements fixation, with values North Atlantic comparison, during late spring 2007. Very fixation rates (0.052 ± 0.031 nmols l −1 d ) were observed all sub‐regions...

10.1029/2009gl041635 article EN Geophysical Research Letters 2010-02-01

Abstract. In September 2021, as part of the Italian Arctic research programme, a multidisciplinary cruise along 75th parallel north through Greenland Sea Gyre was conducted aboard icebreaker Laura Bassi CASSANDRA project, which also contributed to Synoptic Survey (SAS) 2020/22. The took place during period lowest summer sea ice extent ever measured. data show strong horizontal gradients with temperatures between 1.5 °C and 9.0 salinity 30 35. Warm salty Atlantic Water (AW, θ > 3.0 °C, S...

10.5194/essd-2025-37 preprint EN cc-by 2025-02-26

MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout JournalEditorsTheme Sections 248:1-13 (2003) - doi:10.3354/meps248001 Vertical distribution of exopolymer particles in sea ice Fram Strait (Arctic) during autumn Klaus Meiners1,5,*, Rolf Gradinger2, Johanna Fehling1,3, Giuseppe Civitarese4, Michael Spindler1 1Institute for Polar Ecology, University Kiel, Wischhofstraße 1-3, Gebäude 12,...

10.3354/meps248001 article EN Marine Ecology Progress Series 2003-01-01

Since the Aegean took over deep water production of Eastern Mediterranean at end 1980s, proficiency Adriatic as a formation site has been under question. The salt supply in intermediate enabling to produce dense was diminished because salinity decrease by upwelling mid‐depth waters. Tracer data indeed indicate that layer not ventilated for most 1990s. presented also show dilution reached peak 1995, after which more and saline waters were added. recent increase an extremely mass supplied from...

10.1029/2000gl011620 article EN Geophysical Research Letters 2000-10-15
A. Crise Helen Kaberi Javier Ruiz А. Г. Зацепин Е. Г. Арашкевич and 95 more Michele Giani Aristomenis P. Karageorgis Laura Prieto Maria Pantazi Daniel González‐Fernández Maurizio Ribera d’Alcalà Victoria Tornero Vassiliki Vassilopoulou Xavier Durrieu de Madron Cécile Guieu Pere Puig Argyro Zenetos Bruno Andral Dror L. Angel Денис Алтухов Sakina‐Dorothée Ayata Yelda Aktan Esra Billur Balcıoğlu Fabio Benedetti Marc Bouchoucha Maria Cristina Buia J.-F. Cadiou Miquel Canals M. Chakroun Epaminondas Christou M.G. Christidis G. Civitarese Valentina Coatu Maria Corsini-Foka Stefano Cozzi Alan Deidun Alessandro Dell’Aquila Aikaterini Dogrammatzi Alina Dumitrache Dor Edelist Omar Ettahiri S. Fonda‐Umani Slim Gana François Galgani Stéphane Gasparini Antonia Giannakourou Marian-Traian Gomoiu Alexandra Gubanova Ali Cemal Gücü Özgür Gurses Georg Hanke Ioannis Hatzianestis Barak Herut R. Hone I. Emma Huertas Jean‐Olivier Irisson Melek İşinibilir José A. Jiménez Stefanos Kalogirou K. Kapiris Ventzislav Karamfilov Stefanos Kavadas Çetin Keskin Ahmet E. Kıdeyş Mahmut Hakan Koçak Gerasimos Kοndylatos C. Kontogiannis Ruben Kosyan Philippe Koubbi Grozdan Kušpilić R. La Ferla Leonardo Langone S. Laroche Luminița Lazăr Evgenia Lefkaditou I.E. Lemeshko A. Machias Alenka Malej Maria Grazia Mazzocchi В. И. Мединец N. Mihalopoulos Stefano Miserocchi Snejana Moncheva Vladimir Mukhanov G. Oaie Andra Oros Ayaka Amaha Öztürk Bayram Öztürk Marina Panayotova Aristides Prospathopoulos G. Radu Violin Raykov Patricia Reglero Gabriel Reygondeau N. Rougeron Barış Salihoğlu Anna Sánchez‐Vidal Gianmaria Sannino Chiara Santinelli Dan Secrieru

PERSEUS project aims to identify the most relevant pressures exerted on ecosystems of Southern European Seas (SES), highlighting knowledge and data gaps that endanger achievement SES Good Environmental Status (GES) as mandated by Marine Strategy Framework Directive (MSFD). A complementary approach has been adopted, a meta-analysis existing literature pressure/impact/knowledge summarized in tables related MSFD descriptors, discriminating open waters from coastal areas. comparative assessment...

10.1016/j.marpolbul.2015.03.024 article EN cc-by Marine Pollution Bulletin 2015-04-18

Abstract. Temperature, salinity and oxygen data collected during April June 2011 (M84/3 P414 cruises respectively) are analysed to derive the oceanographic characteristics of Eastern Mediterranean (EM) basin. These observed compared with those from previous over period 1987–2011. As a result, interannual decadal variability EM thermohaline properties discussed in context evolution Transient (EMT) general circulation We found that state is still far pre-EMT conditions, though results possibly...

10.5194/os-11-53-2015 article EN cc-by Ocean science 2015-01-09

In winter 1995 the last major field work of Physical Oceanography Eastern Mediterranean (POEM) program was carried out, Levantine Intermediate Water Experiment (LIWEX). this study a thorough analysis is presented data set collected during three successive surveys in January, February, and March–April 1995. The overall result that basin shown to be site for multiple, different, water mass formation processes. Deep (LDW) formed Rhodes gyre, with preconditioning phase starting December 1994....

10.1029/2002jc001643 article EN Journal of Geophysical Research Atmospheres 2003-09-01
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