コーパス検索結果 (１語後でソート)
通し番号をクリックするとPubMedの該当ページを表示します
1 subpolar gyre (SPG) circulation of the North Atlantic Ocean.
2 nutrient concentrations of the (sub)tropical Atlantic Ocean.
3 trations ([Fe]) along a section of the North Atlantic Ocean.
4 via the denitrification pathway in the open Atlantic Ocean.
5 hout the extremely Pi-depleted western North Atlantic Ocean.
6 eature separating the Gulf of Maine from the Atlantic Ocean.
7 h was forced by AMOC variations in the North Atlantic Ocean.
8 pical gyres and the Equatorial Region of the Atlantic Ocean.
9 ntal shelf, slope, and rise of the northwest Atlantic Ocean.
10 Shanghai, China to Cape Verde in the Central Atlantic Ocean.
11 served sea surface temperatures in the North Atlantic Ocean.
12 ion of dissolved organic sulfur (DOS) in the Atlantic Ocean.
13 er in remote regions of the Indian and South Atlantic Ocean.
14 this time was solely eastward into the North Atlantic Ocean.
15 eridional overturning circulation within the Atlantic Ocean.
16 has previously been suggested for the North Atlantic Ocean.
17 alcium carbonate content from the equatorial Atlantic Ocean.
18 er and 1.3 x 10(15) W of heat into the North Atlantic ocean.
19 nd basin-wide environmental gradients in the Atlantic Ocean.
20 st percentage increase occurred in the North Atlantic Ocean.
21 gh krill densities observed in the southwest Atlantic Ocean.
22 21 to 32% of it to be exported to the North Atlantic Ocean.
23 st decade in the mid- to high-latitude North Atlantic Ocean.
24 de in the multidecadal behavior of the North Atlantic Ocean.
25 is vital to pelagic ecosystems in the North Atlantic Ocean.
26 n a sediment core from the subtropical North Atlantic Ocean.
27 and Chain transform faults in the equatorial Atlantic Ocean.
28 ounts of fresh water into the northern North Atlantic Ocean.
29 V methods and was tested on samples from the Atlantic Ocean.
30 cold and fresh water into the northern North Atlantic Ocean.
31 mospheric Observatory in the remote tropical Atlantic Ocean.
32 entricity--in the tropical and extratropical Atlantic Ocean.
33 ting the routing of fresh water to the North Atlantic Ocean.
34 ss properties in the North Pacific and North Atlantic Ocean.
35 9 organizations throughout the western North Atlantic Ocean.
36 collected from 100- to 5,000-m depth in the Atlantic Ocean.
37 irginia (USA) following voyages in the North Atlantic Ocean.
38 munities of 68 species were simulated in the Atlantic Ocean.
39 kton across diverse sites from the Northwest Atlantic Ocean.
40 of truly dissolved POPs at two sites in the Atlantic Ocean.
41 colonizing Greenland from both sides of the Atlantic Ocean.
42 east (toward the Tyrrhenian) and toward the Atlantic Ocean.
43 ir entire lifecycle without migrating to the Atlantic Ocean.
44 onsumes 72% of the DOC exported by the whole Atlantic Ocean.
45 istinct prymnesiophyte partners in the South Atlantic Ocean.
46 raltar and continue their migration into the Atlantic Ocean.
47 of new nutrients in the euphotic zone of the Atlantic Ocean.
48 outhern Ocean, North Pacific Ocean and North Atlantic Ocean.
49 c herring populations from both sides of the Atlantic Ocean.
50 mechanisms in two contrasting regions of the Atlantic Ocean.
51 n the mode of overturning circulation in the Atlantic Ocean.
52 0 years) temperature changes in the northern Atlantic Ocean.
53 III) compounds in the western tropical North Atlantic Ocean.
54 ritis linked to shellfish harvested from the Atlantic Ocean.
55 pine Abyssal Plain site in the eastern North Atlantic Ocean.
56 This is similar to observations from the Atlantic Ocean.
57 the variability of the tropical Pacific and Atlantic Oceans.
58 ated to direct advection from the Indian and Atlantic oceans.
59 are also present in the tropical Indian and Atlantic Oceans.
60 malies in the tropical Pacific and the North Atlantic oceans.
61 ation and divergence; (1) the opening of the Atlantic Ocean, (2) the breakup of Gondwana, and (3) the
64 a significant amount of HCB is stored in the Atlantic Ocean (4.8-26% of the global HCB environmental
65 DOC to the carbon sequestration in the North Atlantic Ocean (62 Tg-C.yr(-1)) is considerable and repr
67 exico, a major propagating rift in the South Atlantic Ocean, abyssal hill fabric on slow-spreading ri
69 the Mediterranean, but two eels reached the Atlantic Ocean after six months and at distances greater
70 d salt transfer from the Indian Ocean to the Atlantic Ocean (Agulhas leakage) has an important effect
72 dicate that the mid-depth North and tropical Atlantic Ocean almost always has lower SigmaCO2 levels t
73 to (15 +/- 12) x 10(6) m3 s(-1) in the North Atlantic Ocean and (21 +/- 6) x 10(6) m3 s(-1) in the So
74 ibuted to a meltwater outflow into the North Atlantic Ocean and a slowdown of North Atlantic Deep Wat
75 pulse, which predominantly entered the North Atlantic Ocean and accounted for about 70 per cent of th
79 aircraft measurement campaign over the North Atlantic Ocean and find evidence for rapid recycling of
80 r rivers that discharge to the western North Atlantic Ocean and find that these rivers are sources of
82 ions ([CO3(2-)]) during three cruises in the Atlantic Ocean and one in the Mediterranean Sea were use
83 xpressing nosZ in samples taken from the mid-Atlantic Ocean and Red Sea implying that Trichodesmium c
84 d phytoplankton community composition in the Atlantic Ocean and show that the distribution of diatoms
85 n of solid-phase extractable DOS in the East Atlantic Ocean and the Atlantic sector of the Southern O
88 adal variability is a notable feature of the Atlantic Ocean and the climate of the regions it influen
89 The water mass structure of the glacial deep Atlantic Ocean and the mechanism by which it may have se
90 m the closure of marine gateways between the Atlantic Ocean and the Mediterranean Sea, the causes of
91 d mesopelagic waters in both the Pacific and Atlantic oceans and has the unusual property of producin
92 most abundant cephalopods in the Pacific and Atlantic Oceans and is an important prey species for a v
93 sium-137 was deposited mostly in Pacific and Atlantic Oceans and North Pole (80%), whereas the rest i
94 d from two major populations, South Georgia (Atlantic Ocean) and the Prince Edward Islands (Indian Oc
95 n based on seawater measurements made in the Atlantic Ocean, and the resultant fluxes suggest that th
96 (-1)) than those previously reported for the Atlantic Ocean, and which are within the range of the hi
97 Cape Agulhas, which separates the Indian and Atlantic Oceans, and across the Drake Passage between th
99 rbon isotope excursion from Maud Rise (South Atlantic Ocean) are controversial, as they seem to indic
100 ginal salmon populations had migrated to the Atlantic Ocean as part of their lifecycle (anadromy), st
102 ly anisotropic model of Europe and the North Atlantic Ocean based on adjoint seismic tomography.
103 Here we use macrostratigraphic data from the Atlantic Ocean basin to show that changes in global spec
106 ion in which they gradually circle the north Atlantic Ocean before returning to the North American co
107 distribution during six cruises in the West Atlantic Ocean between 2008 and 2010 and examined enviro
109 and velocity fluctuations in the Pacific and Atlantic oceans between 42 degrees N and 2 degrees S to
111 mpact on climate variability in the tropical Atlantic Ocean, but a robust influence is found only in
112 on the climate and circulation of the North Atlantic Ocean, but their influence beyond that region r
113 carbonate-ion concentrations in the glacial Atlantic Ocean, by roughly 20 micromolkg-1, while little
114 sts that the provenance of deep water in the Atlantic Ocean can be decoupled from ventilation state o
115 pleted glacial delta(13)C values in the deep Atlantic Ocean cannot be explained solely by water mass
116 e remaining fraction was exported toward the Atlantic Ocean, Central Asia, Northern, and Tropical Afr
117 nity, suggesting a tight linkage between the Atlantic Ocean circulation and hydrologic cycle during t
119 ensive compilation of data from the subpolar Atlantic Ocean, clear evidence of a marked pre-bloom sil
121 cent equatorial and temperate regions of the Atlantic Ocean, collected on three Atlantic Meridional T
122 these cycles coincides with changes in North Atlantic Ocean conditions, indicating a connectivity bet
123 nts were detected in the Pacific, Indian and Atlantic oceans, confined to a strip along the equator (
124 idional overturning circulation in the North Atlantic Ocean does not lead to a net cooling in Europe.
125 involve changes in circulation of the North Atlantic Ocean due to the closing of the Isthmus of Pana
126 pecies that breed in North America cross the Atlantic Ocean during autumn migration when travelling t
129 position of ice-rafted detritus in the North Atlantic Ocean during the last glacial period interprete
130 ion of passive continental margins along the Atlantic Ocean during the opening phase of the current W
131 peratures of the deep Pacific, Southern, and Atlantic oceans during the LGM were relatively homogeneo
132 ficant debate as to the role played by North Atlantic Ocean dynamics in previous climate transitions
133 ti-decadal timescales, indicating that North Atlantic Ocean dynamics played an active role in modulat
135 stadial salinities preconditioned the North Atlantic Ocean for a rapid return to deep overturning ci
136 er clouds, separately in four regions of the Atlantic Ocean, for June through August 2002: marine aer
137 During one of his many voyages across the Atlantic Ocean, Franklin observed that oil had a calming
138 have been a swarming locust that crossed the Atlantic Ocean from Africa to America approximately 6 mi
139 Despite receiving unpolluted air off the Atlantic Ocean from northeasterly trade winds, during tw
140 tion depth in the tropical Pacific and South Atlantic oceans from approximately 42 million years ago,
141 water to the Arctic and high-latitude North Atlantic oceans from lows in the 1960s to highs in the 1
142 on of water masses in the northeastern North Atlantic Ocean has a strong influence on global climate
145 ation taken from sediment cores in the South Atlantic Ocean have yielded conflicting interpretations
146 culation response at only a few sites in the Atlantic Ocean, however, and the phase of circulation re
147 cal sea surface temperature anomalies in the Atlantic Ocean (i.e., Atlantic Multidecadal Oscillation,
149 of 772 Atlantic bluefin tuna in the western Atlantic Ocean in an effort to identify population struc
150 e lead isotope composition of the deep North Atlantic Ocean in response to chemical weathering, we fi
152 amine the timing of dust fluxes to the North Atlantic Ocean, in relation to climate records from the
153 d air during three cruises in the Arctic and Atlantic Oceans, in/over generally oligotrophic waters.
154 ame depth, 1800 meters, in the western North Atlantic Ocean increased by as much as 670 years during
155 Scotland, immediately downwind of the North Atlantic Ocean, indicating that the Scottish ice cap dis
156 undary (CMB) region beneath the southeastern Atlantic Ocean into the upper mantle beneath eastern Afr
159 nd the Faroe Shetland channel into the North Atlantic Ocean is the principal means of ventilating the
160 mixing in the deep Brazil Basin of the South Atlantic Ocean is weak at all depths above smooth abyssa
162 deep-water flow between the Arctic and North Atlantic oceans is critical for modelling climate change
163 out the entire Southern Hemisphere and North Atlantic Ocean, is the main source of nutrients for the
164 s in the Southwestern Pacific and equatorial Atlantic oceans, it came to our attention that misannota
165 rgs through the Hudson Strait into the North Atlantic Ocean, leaving behind distinct layers of ice-ra
166 s: Extensive iceberg influxes into the North Atlantic Ocean linked to global impacts on climate and b
168 asis of detailed observations from the North Atlantic Ocean, mantle temperature was identified as the
169 ation, it is plausible that the entire North Atlantic Ocean may vary in concert, resulting in a varia
172 anariensis, a coral species collected in the Atlantic Ocean never described as a PLTX-producer before
173 results of an experiment conducted over the Atlantic Ocean, off the coast of France, confirming the
174 c samples were collected across the tropical Atlantic Ocean on a transect of the R/V Endeavor in summ
175 nresolved, with tectonic restrictions to the Atlantic Ocean or glacio-eustatic restriction of flow du
177 ense hurricane activity in the western North Atlantic Ocean over the past 5,000 years based on sedime
179 nthic microfaunal record from the equatorial Atlantic Ocean over the past four glacial-interglacial c
181 Occurrence in animals from the Pacific and Atlantic oceans over 111 years made a pathophysiological
183 uesas Islands or between southern Indian and Atlantic Oceans-pointing to a tight correlation between
187 e of heat from warm waters in the deep North Atlantic Ocean probably triggered the Bolling-Allerod wa
188 new evidence that basin-scale changes in the Atlantic Ocean, probably related to the thermohaline cir
189 sages on the Mid-Atlantic Ridge in the North Atlantic Ocean produce as much buoyancy flux as has prev
191 ted from the bipolar seesaw behaviour of the Atlantic Ocean related to changes in the ocean circulati
192 e same latitude but on opposite sides of the Atlantic Ocean, responded by swimming in different direc
193 We suggest that stratification of the North Atlantic Ocean resulted in amplified seasonality that, p
194 tration in deep-sea cores from the southeast Atlantic Ocean reveal millennial-scale pulses of IRD del
196 ral phytoplankton community in the southeast Atlantic Ocean showed no significant toxic response at a
197 connected with the broad southern Indian and Atlantic Oceans, showing that the AC system is pivotal f
199 systems in the Gulf of Mexico (GOM) and U.S. Atlantic Ocean south of Chesapeake Bay were deemed to be
200 n isotope (delta(18)O) record from the South Atlantic Ocean spanning an interval between 30.1 My and
201 Here we reconstructed an index of the South Atlantic Ocean SST (SASD-like) for the past twelve thous
202 h groups detected on the eastern and western Atlantic Ocean suggest that these associations are a gen
203 he surface waters of the tropical North-East Atlantic Ocean, suggesting the global significance of mi
207 ralline algal time series from the northwest Atlantic Ocean that exhibits multidecadal variability ex
208 Mid-Atlantic Ridge in the subtropical North Atlantic Ocean that suggest that passages in rift valley
211 geographically isolated ocean provinces (the Atlantic Ocean, the Red Sea and the Indian Ocean) were s
212 with changes in a major climate mode in the Atlantic Ocean: the Atlantic Multidecadal Oscillation (A
213 Variations in the strength of the North Atlantic Ocean thermohaline circulation have been linked
214 s freshwater outburst delivered to the North Atlantic Ocean through the Lake Huron-North Bay-Ottawa R
216 trophic marine species from the southwestern Atlantic Ocean, tissue from bottlenose dolphins (Tursiop
218 e transition regions of the North Sea to the Atlantic Ocean, to the Baltic Sea, and upstream the Elbe
219 ediate depths (500-2,000 m) across the North Atlantic Ocean, to the south and to the east of the Labr
220 sses (Diomedeidae) do not occur in the North Atlantic Ocean today except as vagrants, although five s
221 lation from the Norwegian Sea into the North Atlantic Ocean took place much earlier than is currently
222 itrate in seawater and air samples along two Atlantic Ocean transects provide the first direct eviden
223 of the Equator arises primarily because the Atlantic Ocean transports energy northward across the Eq
224 re of surface waters in the western tropical Atlantic Ocean underwent pronounced variability about 10
225 he temperature of deep water in the tropical Atlantic Ocean was 4°C colder during the last glacia
227 of plants of any volcanic archipelago in the Atlantic Ocean, was performed to examine patterns of pla
228 e is enough heat contained in inflowing warm Atlantic Ocean water to melt all Arctic sea ice within a
229 d from the Last Glacial Maximum in the North Atlantic Ocean we found that past temperatures reconstru
231 ated with gas hydrates at Blake Ridge in the Atlantic Ocean were dated by measuring their iodine-129/
232 icate that the marine resources of the North Atlantic Ocean were used to sustain an international dem
233 here form four groups, corresponding to the Atlantic Ocean, West pacific, mid-Pacific, and east Paci
235 ed during a 15,000-kilometer transect in the Atlantic Ocean where iron concentrations are relatively
236 the South China Sea, Indian Ocean and South Atlantic Ocean where the relative wind direction matched
237 America and over the east Pacific and North Atlantic oceans where July wind anomalies, averaged betw
238 ose uptake by Prochlorococcus in the central Atlantic Ocean, where glucose concentrations were 0.5-2.
239 essfully made a 2-4 month migration into the Atlantic Ocean, where they utilised well-defined core ar
240 he water mass that fills the mid-depth North Atlantic Ocean, which had been believed to be formed ent
241 ponent of the overturning circulation of the Atlantic Ocean, which helps regulate global climate.
242 n intermediate and deep water in the glacial Atlantic Ocean, which indirectly points to an increase i
243 ays (Mobula tarapacana) in the central North Atlantic Ocean, which provide movement patterns of indiv
244 DZs) in both the Northeast Pacific and North Atlantic Oceans, which we attribute to Cd sulfide (CdS)
245 year-round habitat use of the western North Atlantic Ocean, with a decrease in detections in waters
247 ndergoing net deposition across the tropical Atlantic Ocean, with conditions closer to equilibrium of
WebLSDに未収録の専門用語（用法）は "新規対訳" から投稿できます。