ライフサイエンスコーパス: Atlantic

1 of the tropics and vice versa for the North Atlantic.

2 ronounced formation of deep waters in the NW Atlantic.

3 tuated by a mid-career relocation across the Atlantic.

4 anic carbon in the mesopelagic western North Atlantic.

5 Rockall Bank and Whittard Canyon, Northeast Atlantic.

6 he position of the jet stream over the North Atlantic.

7 mesopelagic waters of the subtropical North Atlantic.

8 w zinc and moderately low iron Western North Atlantic.

9 with spawning time in both the east and west Atlantic.

10 eneath the Saharan dust plume in the Eastern Atlantic.

11 various depths from seven sites in the North Atlantic.

12 s and population processes in the South-east Atlantic.

13 been linked to warming of the subpolar North Atlantic.

14 nhances atmospheric moisture inflow from the Atlantic.

15 fic followed by a radiation into the western Atlantic.

16 and those from the English Channel/northeast Atlantic.

17 tion over the western equatorial Pacific and Atlantic.

18 had previously been reported from cod in the Atlantic [2] and Pacific Oceans [3].

19 Greenland Interstadial (GI) 5.1 in the North Atlantic ( 30,400 to 28,400 years ago).

20 for radiology practices on both sides of the Atlantic about why the emphasis needs to shift from prov

21 t and other published studies from the North Atlantic, although seasonal or interannual variability c

22 mbalances in the rates of formation of North Atlantic and Antarctic Deep Water (the 'bipolar seesaw')

23 ith these springtime patterns: warm tropical Atlantic and cold northeast Pacific sea surface temperat

24 s from the tropical and subtropical Pacific, Atlantic and Indian Oceans were collected during the Mal

25 ward flow on the ocean floor of the Pacific, Atlantic and Indian Oceans.

26 hat on multi-year timescales, a warmer north Atlantic and Mediterranean enhance Sahel rainfall throug

27 l directions: (1) South Pacific, (2) eastern Atlantic and Mediterranean Sea and (3) Americas, the lat

28 ocean temperature in the high latitude North Atlantic and Nordic Seas are reflected in the climate of

29 r Hawaii and negative SLP anomalies over the Atlantic and North America.

30 eoceanic records from the mid-latitude North Atlantic and Osaka Bay, southwest Japan.

31 ng was the dominant driver of changes in the Atlantic and Pacific ventilation during deglaciation.

32 lved iron (DFe) isotope section in the South Atlantic and Southern Ocean.

33 an volcanic plume and was transported to the Atlantic and Tethysian realms through the stratosphere.

34 tmospheric circulation variability and North Atlantic/Arctic paleoceanographic conditions.

35 n eastward moisture transport from the North Atlantic are the primary mechanism by which the teleconn

36 ratures (SSTs) over the tropical Pacific and Atlantic are used to assess the role of tropical oceanic

37 uced productivity in the Subarctic Northwest Atlantic associated with AMO cool phases during the LIA,

38 Hg emission rates in North America and North Atlantic atmospheric Hg(0) concentrations during this pe

39 in growth rates starting in 1997 in the West Atlantic, based on previous studies.

40 imate driver of DOC distributions across the Atlantic basins.

41 nn-Whitney U-test p < 0.0001), and the South Atlantic Bight (20 +/- 8.8 versus 2.2 +/- 1.7 nmol L(-1)

42 ocean acidification on two species of North Atlantic bivalve shellfish, Mercenaria mercenaria and Ar

43 bservation suggests that weak EASM and North Atlantic Bond events may have been induced independently

44 dome field, we find that incursions of warm Atlantic bottom water forced rapid gas hydrate dissociat

45 cts early warming of the deep northern North Atlantic by approximately 1.4 degrees C, while deep Sout

46 Here we present an Atlantic capacitor effect mechanism to suggest that the

47 ded more favourable background state for the Atlantic capacitor effect, giving rise to enhanced bienn

48 wdown of organic carbon within Eastern North Atlantic Central Water (ENACW) that is entrained into si

49 Reported for the first time in southwestern Atlantic cetaceans and in contrast to North American mar

50 These new data support that subpolar North Atlantic circulation changes, likely forced by increased

51 with episodes of more abrupt change in North Atlantic climate and witness societal responses in food

52 y to decouple the EASM system from the North Atlantic climate system.

53 to large areas of tidal marsh along the U.S. Atlantic coast and in other urbanized coastal settings.

54 fasciatus) from a system of basins along the Atlantic coast of Brazil we test for the effects of pale

55 genetic diversity covering nearly the entire Atlantic coast of the Americas.

56 (Ophiothrix sp. III), occurring in the deep Atlantic coast of the Iberian Peninsula and the Alboran

57 hest rates of relative sea level rise on the Atlantic coast of the United States.

58 he United States, particularly along the Mid-Atlantic coast.

59 f RAD-Seq datasets resolved the classic Gulf-Atlantic coastal phylogeographic break, which was not si

60 mercially and ecologically important fishes, Atlantic cod (Gadus morhua) and haddock (Melanogrammus a

61 6 CE) and subsequent medieval (1066-1280 CE) Atlantic cod (Gadus morhua) specimens from excavation si

62 stick (LFD) assays for the identification of Atlantic cod (Gadus morhua), Pacific cod (Gadus macrocep

63 M) for the authentication of gadoid species: Atlantic cod (Gadus morhua), Pacific cod (Gadus macrocep

64 structure of a population complex of coastal Atlantic cod (Gadus morhua).

65 ice in distinguishing fillets and patties of Atlantic cod (n=80) from those of haddock (n=90), in com

66 rary from X-cell xenomas of blue whiting and Atlantic cod and assembled 63 X-cell protein-coding gene

67 ny, are traced back to the North East Arctic Atlantic cod population that has supported the Lofoten f

68 We also screened Atlantic cod populations for xenomas and residual pathol

69 For Atlantic cod, an historically dominant piscivore in the

70 Results suggest that North Atlantic cooling during Heinrich stadial 11 (HS11) affec

71 Here we show that the recent Atlantic cooling is likely to persist, as predicted by a

72 of the Arctic Ocean indicate the northbound Atlantic current as a significant conveyor of DDTs.

73 128-116 ka) tropical and extratropical North Atlantic cyclones may have been more intense than at pre

74 n in the Atlantic involving changes in North Atlantic Deep Water (NADW) and Antarctic Bottom Water (A

75 record reveals a similar proportion of North Atlantic Deep Water during the 'lukewarm interglacials'

76 record from the southernmost extent of North Atlantic Deep Water to reconstruct gateway-related chang

77 regated two distinct populations in the near Atlantic, despite their large spatial distance.

78 inant mode of atmospheric variability in the Atlantic domain.

79 Since the early 1990s, a warmer Atlantic due to the positive phase of Atlantic multideca

80 ktonic foraminifera in an Eastern Equatorial Atlantic (EEA) sediment core from the Niger Delta.

81 oxygen eddies in the eastern tropical North Atlantic (ETNA) can produce N2O concentrations much high

82 he bi-partition was not limited to the North Atlantic/European region, the data also imply a climatic

83 e natural latitudinal range in the Northeast Atlantic exhibit greater shell dissolution and the inabi

84 sm to explain the early warming in the North Atlantic, featuring a strong middepth warming and enhanc

85 67 +/- 1299 copies ml(-1) ) and the tropical Atlantic for BII (4125 +/- 339 copies ml(-1) ).

86 ed growth rate data from throughout the West Atlantic for green turtles, Chelonia mydas, which are lo

87 orthern Great Plains, New England, and South Atlantic for interstitial lung disease; along the southe

88 h sea surface temperatures (SST) in the West Atlantic for years of declining growth rates (r = -.94)

89 and geographic barriers within the Brazilian Atlantic Forest (AF) biota, and consequently two process

90 enetic (PBD) beta-diversity of snakes in the Atlantic Forest (AF) hotspot, South America.

91 he Eastern Arc Mountains of Tanzania and the Atlantic Forest of Brazil are two of the most fragmented

92 In the Atlantic Forest, regenerating 6,452 ha of forest would c

93 ustralia's Mount Lofty Ranges and Paraguay's Atlantic Forest.

94 l results suggest that, in response to North Atlantic freshwater forcing during the early phase of th

95 ific winter storm track in response to North Atlantic freshwater forcing, a mechanism suggested by si

96 Milk was collected from Atlantic grey seals (Halichoerus grypus) periodically fr

97 nducted at the eastern boundary of the South Atlantic gyre.

98 ly life stages of the commercially important Atlantic haddock (Melanogrammus aeglefinus).

99 ther a functional vwf gene is present in the Atlantic hagfish, Myxine glutinosa We found a single vwf

100 a surface temperatures in the northern North Atlantic have shown a marked decrease over the past seve

101 are strongly anti-correlated with trends in Atlantic heat transport across the Barents Sea Opening (

102 oupled climate models suggests that enhanced Atlantic heat transport across the BSO associated with r

103 This feature of the Atlantic herring facilitates the detection of genetic fa

104 Atlantic herring is an excellent species for studying th

105 The Atlantic herring is one of the most abundant vertebrates

106 e compared whole-genome resequencing data of Atlantic herring populations from both sides of the Atla

107 t conditions conducive to greater basin-wide Atlantic hurricane activity occur together with conditio

108 riability that is known to strongly modulate Atlantic hurricane activity.

109 The prevailing view of western Atlantic hydrography during the Last Glacial Maximum (LG

110 identify volcanism associated with the North Atlantic Igneous Province, rather than carbon from a sur

111 locline measurements for PFOS based on North Atlantic inflow (11-36 pg/L) agreed with measurements (m

112 state, with a substantially greater role for Atlantic inflows.

113 We here present Pliocene Atlantic interhemispheric sea surface temperature and sa

114 rganization of deep ocean circulation in the Atlantic involving changes in North Atlantic Deep Water

115 The subpolar North Atlantic is a key location for the Earth's climate syste

116 pacitor effect mechanism to suggest that the Atlantic is a key pacemaker of the biennial variability

117 The North Atlantic is characterized by diatom-dominated spring blo

118 rm wider-ranging movements in the north-east Atlantic is currently lacking.

119 that an ecological regime shift (ERS) in the Atlantic is driving growth dynamics.

120 In particular, the North Atlantic is identified as a region where the downward tr

121 of sea surface temperature anomalies in the Atlantic is not uniformly cool, but instead has anomalou

122 this hypothesis in several subpopulations of Atlantic killifish that have evolved a gradation of resi

123 erturning Circulation (AMOC), inflowing warm Atlantic Layer water, ice sheet, sea-ice and ice-shelf f

124 ntegrated with data from other western North Atlantic locations, indicate that the ocean was poorly v

125 The Central Atlantic Magmatic Province (CAMP) has long been proposed

126 ESM2G), here we show that the decline of the Atlantic major hurricane frequency during 2005-2015 is a

127 r this period, suggesting the decline of the Atlantic major hurricane frequency during 2005-2015 is n

128 Observed Atlantic major hurricane frequency has exhibited pronoun

129 l variations involving the inferred AMOC and Atlantic major hurricane frequency, along with indices o

130 nt role of the AMOC in the recent decline of Atlantic major hurricane frequency.

131 Such is the case for NE Atlantic marine macroalgal forests, important ecosystems

132 observe no divergence between the kauri and Atlantic marine sediment (14)C data sets, implying limit

133 We identify changes in tropical Atlantic mean state and variability caused by the moment

134 ed distribution (Eastern Pacific, Caribbean, Atlantic, Mediterranean, Madagascar, Australia).

135 antic were accompanied by both reductions in Atlantic Meridional Overturning Circulation (AMOC) and c

136 5-2015 is associated with a weakening of the Atlantic Meridional Overturning Circulation (AMOC) infer

137 imulations indicate the strengthening of the Atlantic Meridional Overturning Circulation (AMOC) with

138 content (OHC) is highly correlated with the Atlantic Meridional Overturning Circulation (AMOC), and

139 threshold was reached at 400 ka involving Atlantic Meridional Overturning Circulation (AMOC), infl

140 r for the YDS climate was a weakening of the Atlantic Meridional Overturning Circulation (AMOC).

141 ed with an abrupt (</=400 year) deepening of Atlantic Meridional Overturning Circulation (AMOC).

142 the inter-gyre heat transport as part of the Atlantic Meridional Overturning Circulation must be acco

143 a role of Caribbean hydroclimate in helping Atlantic Meridional Overturning Circulation recovery dur

144 Southern Ocean and the near collapse of the Atlantic Meridional Overturning Circulation.

145 ife stage that actually undertakes the trans-Atlantic migration.

146 cadal timescale via teleconnections with the Atlantic Multi-decadal Oscillation (AMO).

147 riability is largely explained by the remote Atlantic multidecadal oscillation (AMO).

148 iodicity of 60-80 years that is known as the Atlantic Multidecadal Oscillation (AMO).

149 he Pacific Decadal Oscillation (PDO) and the Atlantic Multidecadal Oscillation (AMO).

150 onsistent with the timing and phasing of the Atlantic Multidecadal Oscillation (AMO).

151 warmer Atlantic due to the positive phase of Atlantic multidecadal oscillation and global warming tre

152 represented by climate indexes, such as the Atlantic Multidecadal Oscillation and North Atlantic Osc

153 as it was during the last cold phase of the Atlantic Multidecadal Oscillation index in the 1990s.

154 ature anomalies in the Atlantic Ocean (i.e., Atlantic Multidecadal Oscillation, AMO).

155 r hurricane frequency, along with indices of Atlantic Multidecadal Variability and inverted vertical

156 the El Nio Southern Oscillation (ENSO), the Atlantic Nio and the Indian Dipole Mode.

157 ross large parts of the North Pacific, North Atlantic, North America and the Mediterranean.

158 (that is, ENSO imprinting the North Tropical Atlantic (NTA) sea surface temperature (SST) via an atmo

159 ollected along a latitudinal transect in the Atlantic Ocean (31 degrees N to 38 degrees S).

160 cal sea surface temperature anomalies in the Atlantic Ocean (i.e., Atlantic Multidecadal Oscillation,

161 Our findings suggest that the Atlantic Ocean acts as a key pacemaker for the western P

162 aircraft measurement campaign over the North Atlantic Ocean and find evidence for rapid recycling of

163 xpressing nosZ in samples taken from the mid-Atlantic Ocean and Red Sea implying that Trichodesmium c

164 water-exchange region between the North Sea-Atlantic Ocean and the Baltic Sea.

165 g and autumn-spawning populations across the Atlantic Ocean and the Baltic Sea.

166 sts that the provenance of deep water in the Atlantic Ocean can be decoupled from ventilation state o

167 pecies that breed in North America cross the Atlantic Ocean during autumn migration when travelling t

168 have been a swarming locust that crossed the Atlantic Ocean from Africa to America approximately 6 mi

169 The Atlantic Ocean is well ventilated, and unlike the major

170 anariensis, a coral species collected in the Atlantic Ocean never described as a PLTX-producer before

171 ral phytoplankton community in the southeast Atlantic Ocean showed no significant toxic response at a

172 n isotope (delta(18)O) record from the South Atlantic Ocean spanning an interval between 30.1 My and

173 ralline algal time series from the northwest Atlantic Ocean that exhibits multidecadal variability ex

174 e is enough heat contained in inflowing warm Atlantic Ocean water to melt all Arctic sea ice within a

175 icate that the marine resources of the North Atlantic Ocean were used to sustain an international dem

176 rbon isotope excursion from Maud Rise (South Atlantic Ocean) are controversial, as they seem to indic

177 ation and divergence; (1) the opening of the Atlantic Ocean, (2) the breakup of Gondwana, and (3) the

178 (-1)) than those previously reported for the Atlantic Ocean, and which are within the range of the hi

179 ensive compilation of data from the subpolar Atlantic Ocean, clear evidence of a marked pre-bloom sil

180 rgs through the Hudson Strait into the North Atlantic Ocean, leaving behind distinct layers of ice-ra

181 geographically isolated ocean provinces (the Atlantic Ocean, the Red Sea and the Indian Ocean) were s

182 trophic marine species from the southwestern Atlantic Ocean, tissue from bottlenose dolphins (Tursiop

183 e transition regions of the North Sea to the Atlantic Ocean, to the Baltic Sea, and upstream the Elbe

184 In the North Atlantic Ocean, we found that natural populations of Pro

185 year-round habitat use of the western North Atlantic Ocean, with a decrease in detections in waters

186 ion of dissolved organic sulfur (DOS) in the Atlantic Ocean.

187 mospheric Observatory in the remote tropical Atlantic Ocean.

188 ss properties in the North Pacific and North Atlantic Ocean.

189 9 organizations throughout the western North Atlantic Ocean.

190 collected from 100- to 5,000-m depth in the Atlantic Ocean.

191 is vital to pelagic ecosystems in the North Atlantic Ocean.

192 irginia (USA) following voyages in the North Atlantic Ocean.

193 munities of 68 species were simulated in the Atlantic Ocean.

194 kton across diverse sites from the Northwest Atlantic Ocean.

195 of truly dissolved POPs at two sites in the Atlantic Ocean.

196 colonizing Greenland from both sides of the Atlantic Ocean.

197 c herring populations from both sides of the Atlantic Ocean.

198 via the denitrification pathway in the open Atlantic Ocean.

199 The North Atlantic ocean/atmosphere environment exhibits pronounce

200 growth coincide with remote Arctic and North Atlantic oceanographic processes that link to the Gulf o

201 d air during three cruises in the Arctic and Atlantic Oceans, in/over generally oligotrophic waters.

202 are also present in the tropical Indian and Atlantic Oceans.

203 titative uncertainty estimates for the South Atlantic, offering a strong basis for studies of paleoci

204 ssolved oxygen and N2O concentrations in the Atlantic OMZ are relatively high and low, respectively.

205 on of aerosols from sea spray over the North Atlantic on board the exhaust-free solar-powered vessel

206 up, our results suggest both vicariance (the Atlantic opening) and dispersal.

207 ng the last ice age temperature in the North Atlantic oscillated in cycles known as Dansgaard-Oeschge

208 al stations, gridded climate data, and North Atlantic Oscillation (NAO) and Arctic Oscillation (AO) i

209 ressed latitude of crop damage against North Atlantic Oscillation (NAO) and crop area to test the hyp

210 The North Atlantic Oscillation (NAO) depicts annual and decadal os

211 Shifts in the North Atlantic Oscillation (NAO) from 1-2 to 0-1 in four episo

212 tween our new composite ITCZ-stack and North Atlantic Oscillation (NAO) records reveals a tight coupl

213 al was positively associated with June North Atlantic Oscillation (NAO) values, whereas male survival

214 arcity of paleo-records related to the North Atlantic Oscillation (NAO), particularly in East-Central

215 ate in Europe and North America is the North Atlantic Oscillation (NAO), the dominant mode of atmosph

216 e MASTREE database) and data on the Northern Atlantic Oscillation (NAO), we show that in the last 60

217 teristics of the negative phase of the North Atlantic Oscillation (NAO), while in the late Holocene t

218 h cannot be explained as driven by the North Atlantic Oscillation (NAO).

219 re accompanied by a rapid sub-seasonal North Atlantic Oscillation (NAO)/Arctic Oscillation (AO) phase

220 may promote the negative phase of the North Atlantic Oscillation (NAO-).

221 onal transport, are assessed using the North Atlantic Oscillation index.

222 cings, such as solar radiation and the North Atlantic Oscillation, during the late Holocene.

223 s large-scale atmospheric circulation (North Atlantic Oscillation, NAO).

224 ial evapotranspiration, along with the North Atlantic Oscillation, predicted variation in selection a

225 re modulated by dominant phases of the North Atlantic Oscillation, which had a major influence on veg

226 Atlantic Multidecadal Oscillation and North Atlantic Oscillation.

227 ological processes-and use it to reconstruct Atlantic overturning circulation during the last 800 kyr

228 in Antarctic overturning relate to Northern Atlantic overturning circulation, a major driver of Nort

229 A suite of Atlantic Pacemaker experiments successfully reproduces t

230 eport high microbial loads over the tropical Atlantic, Pacific and Indian oceans and propose islands

231 xed layer is 60-90 years.Deep waters of the Atlantic, Pacific and Indian Oceans upwell in the Southe

232 lity can be traced back to variations of the Atlantic/Pacific sea surface temperature gradient, exter

233 ssage frequency will decrease over the North Atlantic, particularly in the Gulf of Mexico, but will i

234 measured in muscle from juvenile male North Atlantic pilot whales (Globicephala melas) harvested bet

235 coast, the largest rookery for the Northwest Atlantic population.

236 ese questions, we track the migration of 270 Atlantic puffins Fratercula arctica, a red-listed, decli

237 sa and Alcyonium digitatum, in the northeast Atlantic (ranging from the northwest of Ireland and the

238 cific records are coeval with changes in the Atlantic records.

239 showed an increased NARW presence in the mid-Atlantic region and a simultaneous decrease in the north

240 The Mid-Atlantic region had the highest rate.

241 llennial-scale events than that of the North Atlantic region is likely to decouple the EASM system fr

242 er input and associated cooling in the North Atlantic region.

243 significantly increased within many coastal Atlantic regions between 40 degrees N and 60 degrees N,

244 zed large areas of the Caribbean and western Atlantic, resulting in an immense ecological damage.

245 ed Atlantis Massif oceanic core complex, Mid-Atlantic Ridge.

246 olivine-hosted melt inclusions from the Mid-Atlantic Ridge.

247 istribution patterns of the endangered North Atlantic right whale (NARW; Eubalaena glacialis) populat

248 ected here could be detrimental to the North Atlantic Right Whale and a host of important fishery spe

249 The North Atlantic right whale population is currently the focus o

250 usly undetected connectivity between western Atlantic sailfish fisheries and pelagic longline catches

251 rees C) affect the flesh quality of triploid Atlantic salmon (Salmo salar L., 1.6+/-0.3kg).

252 e show that nutrient pulses from decomposing Atlantic salmon (Salmo salar) parents alter selection pr

253 O. mykiss), Chinook salmon (O. tshawytscha), Atlantic salmon (Salmo salar), and Arctic charr (Salveli

254 re perhaps the most important problem facing Atlantic Salmon aquaculture after feed sustainability.

255 icrobiota harboured in the distal digesta of Atlantic salmon freshwater fish (FW) kept in a commercia

256 died among selected (FP) and unselected (WP) Atlantic salmon lines that were reared together to avoid

257 variation over five decades in four marginal Atlantic salmon populations located at the southern limi

258 Atlantic salmon undergo dramatic physiological changes a

259 Atlantic sardines (Sardina pilchardus) captured in the P

260 North Atlantic sea surface temperatures experience variability

261 The U.S. mid-Atlantic sea-level record is sensitive to the history of

262 An index of North Atlantic sea-surface temperatures in March-April can pre

263 ime atmospheric circulation--the summer East Atlantic (SEA) pattern--is predictable from the previous

264 pe and northern Asia through Beringia to the Atlantic seaboard of North America.

265 s of biomass and abundance) in the southwest Atlantic sector of the Southern Ocean, from net samples

266 Antarctic climate pattern extending into the Atlantic sector of the Southern Ocean.

267 graphic bias in Arctic BC studies toward the Atlantic sector, with lack of observational constraints

268 of the seasonal cycle in the European/North Atlantic sector.

269 However, a Southern Ocean (Atlantic-sector) iceberg rafted debris event appears to

270 ed concentrations of DDTs in the Barents and Atlantic sectors of the Arctic Ocean indicate the northb

271 ed to the New World with the 16-19th Century Atlantic Slave Trade.

272 e warmer conditions were caused by increased Atlantic-sourced water inflow combined with amplified se

273 stematic status of several transisthmian and Atlantic species are clarified.

274 e report on experiments performed with North Atlantic species of Ulva and Gracilaria grown in situ or

275 e no long-term warming in the subpolar North Atlantic (SPG).

276 The Subpolar North Atlantic (SPNA) is one of the most important areas to gl

277 the main hurricane-development region in the Atlantic, SST and VWS co-vary inversely, so that the two

278 Warm tropical Atlantic SSTs can trigger diabatic heating in the atmosp

279 across geographic space and suggest the mid-Atlantic states of North Carolina and Virginia as an eme

280 The model also predicts that the NE Atlantic storms are capable of producing boulderites tha

281 da Atlantic Time-series Station in the North Atlantic Subtropical Gyre, while assessing seasonal shif

282 noplastics) of debris collected in the North Atlantic subtropical gyre.

283 l covering the eastern boundary of the North Atlantic subtropical gyre.

284 Directly observed North Atlantic sulfate aerosol optical depth has not increased

285 hemisphere and global SAI scenarios on North Atlantic TC activity using the HadGEM2-ES general circul

286 However, unlike the last cold period in the Atlantic, the spatial pattern of sea surface temperature

287 ated quarterly over two years at the Bermuda Atlantic Time-series Station in the North Atlantic Subtr

288 ather than simple propagation from the North Atlantic to the EASM regions.

289 the atmospheric moisture transport from the Atlantic to the South American continent.

290 Later deepening and widening of the South Atlantic, together with gateway opening at Drake Passage

291 single hemisphere effectively modulate North Atlantic tropical cyclone (TC) activity in the following

292 lion Medicare enrollees of the Northeast/Mid-Atlantic United States between 2003-2010; (ii) long-term

293 In 2010, BMSB populations in the mid-Atlantic United States reached outbreak levels and subse

294 cent portions of the Caribbean Sea and North Atlantic using satellite-tracked drifter trajectory data

295 line, and shoaling of the intermediate-depth Atlantic Water layer in the eastern Eurasian Basin have

296 to centennial increases in alkenone-inferred Atlantic Water SSTs on the shelf occurred at times of re

297 ocline limits upward heat transport from the Atlantic water.

298 vidence show that cold stadials in the North Atlantic were accompanied by both reductions in Atlantic

299 pical Pacific (including El Nino events) and Atlantic were the main drivers of extreme droughts in So

300 rming was triggered by the entry of a strong Atlantic windstorm into the Arctic in late December 2015