[PDF] Top 20 Evolution of 231Pa and 230Th in overflow waters of the North Atlantic
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Evolution of 231Pa and 230Th in overflow waters of the North Atlantic
... in waters immediately following ventila- tion at the start of Atlantic meridional ...young North Atlantic deep ...the Atlantic, ranging between ...young waters present in those ... See full document
15
Improving North Atlantic marine core chronologies using 230Th normalization
... surface waters and the contemporary atmosphere, commonly referred as the surface reservoir ...that north of ~40°N in the Atlantic, surface reservoir ages have undergone large variations through time ... See full document
17
Holocene evolution of the North Atlantic subsurface transport
... saline waters from the subtropical gyre and thus stabilize the Atlantic Meridional Overturning Circula- tion ...polar North Atlantic during the last 11 000 years, by combining new temperature ... See full document
12
Holocene atmospheric iodine evolution over the North Atlantic
... Abstract. Atmospheric iodine chemistry has a large influ- ence on the oxidizing capacity and associated radiative im- pacts in the troposphere. However, information on the evo- lution of past atmospheric iodine levels is ... See full document
12
A review ofPseudo-nitzschia, with special reference to the Skagerrak, North Atlantic, and adjacent waters
... = no data Valve symmetry (tt axis} iso hetero Central Fibulae & striae Hymenate velum nodule equal unequal simple sectors in nr.. wide in girdle view)... Season[r] ... See full document
45
Impact of North Atlantic – GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation
... the Atlantic Meridional Overturning Circulation (AMOC) is simulated and proposed as a key factor for the onset of the Bølling-Allerød (BA) warming ...of North Atlantic – GIN Sea exchange on the ... See full document
6
Vertical coarse aerosol fluxes in the atmospheric surface layer over the North Polar Waters of the Atlantic
... We show that most literature sea spray generation functions are underestimated for the 1 – 8 mm radius range, some of them by a factor of 6. Citation: Petelski, T., and J. Piskozub (2006), Vertical coarse aerosol fluxes ... See full document
9
Interaction of the Faroe Bank Channel overflow with Iceland Basin intermediate waters
... the north- ern limit of this water mass, which in part explains its patchy lateral distribution (Figure 6) and variable vertical ...low-oxygen waters from the Iceland Basin intruding between MNAW and NSDW ... See full document
13
An assessment of the vertical diffusive flux of iron and other nutrients to the surface waters of the subpolar North Atlantic Ocean
... surface waters indicated that regardless of the magni- tude of the turbulent diffusive flux the source waters that re- supply the surface ocean with Fe are inherently low in dFe relative to their NO − 3 ... See full document
18
Calcification in the planktonic foraminifera Globigerina bulloides linked to phosphate concentrations in surface waters of the North Atlantic Ocean
... It is possible that different genotypes of G. bulloides ex- hibit different calcification responses to the same environ- mental factors, as is the case in the coccolithophore Emilia- nia huxleyi (Langer et al., 2009). It ... See full document
15
Coastal and transitional waters North East Atlantic geographic intercalibration group: Seagrasses ecological assessment methods
... Coastal Waters (CW) (NEA 1/26) and Transitional Waters (TW) (NEA 11) in the North East Atlantic Geographical Intercalibration Group ... See full document
50
Water-mass evolution in the Cretaceous Western Interior Seaway of North America and equatorial Atlantic
... Tethyan waters, the other hiatal surfaces identified through- out the KWIS appear to be associated with increased bottom- water current activity linked to regional climatic and/or tec- tonic subsidence-induced ... See full document
24
Tectono-stratigraphic evolution and crustal architecture of the Orphan Basin during North Atlantic rifting
... of the Newfoundland margin, and it is bounded by the con- tinental shelf to the west, the Grand Banks to the south, and the continental blocks of Orphan Knoll and Flemish Cap to the east. The Orphan Basin formed in ... See full document
21
Sub meso scale phytoplankton distribution in the North East Atlantic surface waters determined with an automated flow cytometer
... Cells of C3 cluster exhibited a high periodicity with an abundance increase twice as fast as the FLR and FWS sig- natures up to the middle of M2 waters (i.e. 14 ◦ W, Table 3). This may be linked to thermal water ... See full document
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Transitional waters North East Atlantic geographic intercalibration group: Intercalibration of a new Fish ecological assessment method
... EMFI Transitional water None Conclusion: Intercalibration is feasible in terms of typology 3.2 Pressures addressed The response of the EMFI to anthropogenic disturbance was examined using two independent measures of ... See full document
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Coastal and transitional waters North East Atlantic geographic intercalibration group: Opportunistic macroalgae ecological assessment methods
... While it is clear that DIN has a relationship with this BQE this is confounded by the multiple pressures present in the estuarine environment. To account for this other factors known to affect OGA growth were considered. ... See full document
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Coastal waters North East Atlantic geographic intercalibration group: Benthic invertebrate fauna ecological assessment methods
... the North Sea related datasets and Portugal; a group with the datasets from shallow areas in the UK and France and a group with samples from less shallow areas (>30m depth) of UK, Spain, Norway and Ireland ... See full document
150
Return of naturally sourced Pb to Atlantic surface waters
... surface waters of the tropical North ...surface waters occur in restricted latitudinal bands, and their location and magnitude are influenced by the position of the North African dust plume, ... See full document
13
Estimates of cetacean abundance in European Atlantic waters in summer
... southern North Sea (Hammond et ...the North Sea and the Celtic Sea, and now encompasses the entire Channel, at least in ...the North Sea the estimate in 2016 (345,000, CV = ...the North Sea ... See full document
40
Methanol acetaldehyde and acetone in the surface waters of the Atlantic Ocean
... [ 25 ] There were three regions (8–13 N, 27 S, and 35 S) where the solar noon concentrations were noticeably higher than those predawn (Figure 2b), suggesting that photo- chemistry may have influenced acetaldehyde ... See full document
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