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2012 OCSD Diversion Synthesis Report Template
2012 OCSD Diversion Synthesis Report Template

... Evidence of the plume was evident in salinity and CDOM. Initially, lower salinity and higher CDOM waters associated with the discharge were seen subsurface at the outfall (Station 2202), rising to the surface and moving downcoast and offshore of the outfall (September 12-18). On September 24 and 25, ...
some observations of short-term heat transfer through the surface
some observations of short-term heat transfer through the surface

Chapter 31
Chapter 31

... “Oceanographers use salinity -- the amount (in grams) of total dissolved salts present in 1 kilogram of water -- to express the salt content of seawater. Normal seawater has a salinity of 35 grams/kilogram (or liter) of water -- also expressed as 35‰. Seawater from Wormly in southern England is use ...
Text invitation press conference final
Text invitation press conference final

... And CO2 is the big evildoer of the earth’s warming up. Professor Baeyens is carrying out this research with the SeaExplorer robot. Everybody knows that the CO2-concentration in the atmosphere has to be reduced drastically. This can be achieved in 2 ways: by restricting the CO2-production or by incre ...
Climate variability and ocean production in the Leeuwin Current
Climate variability and ocean production in the Leeuwin Current

... The strength of the Leeuwin Current (LC) and its eddy field are both strong during the austral winter and weak during the austral summer on the annual time scale, and are strong during the La Niña years and weak during the El Niño years on the interannual time scale. As the LC is a warm current, the ...
Full-Text PDF - BioPublisher
Full-Text PDF - BioPublisher

... recorded at St.5 (Zyteia in port) during winter of 2015. Generally, the maximum mean value of 26.11 °C was recorded during summer and the minimum mean value of 19.24 °C was observed in winter. An inverse correlation (r= - 0.57) was found between the seasonal variations of phytoplankton and water tem ...
Zonally asymmetric response of the Southern Ocean mixed
Zonally asymmetric response of the Southern Ocean mixed

... (for example, nutrient concentration and light availability) and the phytoplankton grazing (for example, zooplankton concentration). The effect of MLD on phytoplankton concentration can be immediate or lagged in time. For example, the nutrient concentrations essential to phytoplankton growth are mor ...
Mesozooplankton in the Arctic Ocean in summer
Mesozooplankton in the Arctic Ocean in summer

50 - Association for the Sciences of Limnology and Oceanography
50 - Association for the Sciences of Limnology and Oceanography

D3.5: Aquaculture indicators report - AQUA
D3.5: Aquaculture indicators report - AQUA

... This  report  is  a  contribution  for  the  development  of  indicators  to  improve  aquaculture  development   and   sustainability.   Both   in   situ   and   satellite   data   are   used   to   establish   the   natural   variability   ...
Accurate focal depth determination of oceanic earthquakes using
Accurate focal depth determination of oceanic earthquakes using

In situ measurements of thermal diffusivity in sediments of the
In situ measurements of thermal diffusivity in sediments of the

WIND AND BUOYANCY-FORCED UPPER OCEAN
WIND AND BUOYANCY-FORCED UPPER OCEAN

Impacts of climate change on harmful algal blooms
Impacts of climate change on harmful algal blooms

... No clear trend that can be attributed to climate change can be observed in the incidence of shellfish toxin producing HABs since the last report card was issued. During the last two years the incidence of some shellfish toxins has continued to decrease (e.g. paralytic shellfish poisoning toxins in S ...
[Subramaniam et al. 2008]
[Subramaniam et al. 2008]

... This article contains supporting information online at www.pnas.org/cgi/content/full/ 0710279105/DCSupplemental. © 2008 by The National Academy of Sciences of the USA ...
PDF - compatibile with Acrobat 4.0
PDF - compatibile with Acrobat 4.0

... In marine environments, biotic and abiotic environmental factors have important effects on phytoplankton succession and abundance. The eastern Mediterranean Sea is one of the most oligotrophic marine areas in the world (Azov 1991). This pattern may have altered in the last few years, however, becaus ...
Dynamics of potentially harmful phytoplankton in a semi
Dynamics of potentially harmful phytoplankton in a semi

... water. Identification of harmful species was based on Hallegraeff et al. (2004). As there was no significant difference in diatom abundance or dinoflagellate abundance between samples collected at the surface (1 m) and at 10 m (paired t-tests for diatoms: P = 0.93; for dinoflagellates: P = 0.23, res ...
Global patterns of bioturbation intensity and mixed depth of marine
Global patterns of bioturbation intensity and mixed depth of marine

... centimetres of oceanic sediments provides a compelling reason for wanting to quantify in situ rates of bioturbation. Whilst several approaches can be used for estimating the rate and extent of bioturbation, most often it is characterized by calculating an intensity coefficient (D b) and/or a mixed l ...
Chapter 13 - COSEE Florida
Chapter 13 - COSEE Florida

Student Worksheets, Assessments, and Answer Keys
Student Worksheets, Assessments, and Answer Keys

... We know that sound travels. How fast does it travel? Sound travels about 1500 meters per second in seawater. That's approximately 15 football fields end-to-end in one second. Sound travels much more slowly in air, at about 340 meters per second, only 3 football fields a second. Unfortunately, the an ...
Calibration, correction and flagging from the chlorophyll
Calibration, correction and flagging from the chlorophyll

... months climatologically. Within any particular year, however, the spring bloom can peak as early as mid-February (e.g. 2012) or as late as April 20 (e.g. 2014) with peak values below 10 (mg chl m-3, 2011 and 2013) or in excess of 20 (mg chl m-3, 2007 and 2009). The fall blooms can be non-existent (e ...
PDF - Oxford Academic - Oxford University Press
PDF - Oxford Academic - Oxford University Press

... hydrothermal waters spreading just in the upper 0–1.5 m layer. The latter is evident from the salinity profiles (Figures 2 and 4). A significant part (40–80%) of the active phototrophic microplankton inhabits a dark water layer below the euphotic zone, e.g. below 6–7 m depth, (Kp curves, Figures 2 a ...
o L i cean
o L i cean

... The Ocean Life Institute supports groundbreaking basic research covering the full range of marine organisms, from bacteria to whales. Over the past year, OLI funded research in a number of important areas through a combination of research grants and fellowships to scientists, postdoctoral investigat ...
Development and field testing a satellite-linked fluorometer for marine vertebrates et al.
Development and field testing a satellite-linked fluorometer for marine vertebrates et al.

... Advances in technology can account for this (e.g., fluorometers on gliders, buoys, and drifters), but they can be spatially and temporally limiting or expensive. Marine animals tagged with satellite transmitters or other electronic instruments are commonly employed as autonomous ocean profilers to p ...
PICES XV W1-3036 Invited The organic complexation in modeling
PICES XV W1-3036 Invited The organic complexation in modeling

... Iron is an important trace nutrient for phytoplankton in the ocean. Recent studies have focused on the relationship between iron budget and marine ecosystem response. In the open ocean, the main source of iron in the surface layer is due to atmospheric deposition of mineral dust and/or supply from t ...
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Critical Depth

In biological oceanography, 'Critical Depth' is defined as a hypothesized surface mixing depth at which phytoplankton growth is precisely matched by losses of phytoplankton biomass within this depth interval.
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