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1 causes: a giant impact or mantle convection/overturn.
2 ion of the stored methane is oxidized during overturns.
3 weakness of this connection, the concept is overturned.
4 very established "rule" seems destined to be overturned.
5 harp northern warming followed reinvigorated overturning.
6 the abrupt resumption of Atlantic meridional overturning.
7 ing, likely promoted by rejuvenated Atlantic overturning.
8 t necessarily require a complete shutdown of overturning.
9 ich event 1 could have only affected shallow overturning.
10 the structure and variability of the ocean's overturning.
11 icit in models of the average Southern Ocean overturning.
12 for its representation in models of oceanic overturning.
13 inated overturning and E: buoyancy-dominated overturning.
14 stablished dogma of 'horror autotoxicus' was overturned 50 years ago with the publication of a paper
20 nd Iceland basins is largely responsible for overturning and its variability in the subpolar basin.
21 The Southern Ocean is a key region for the overturning and mixing of water masses within the global
22 patterns consistent with changes in Atlantic overturning and repeatedly steepened the temperature gra
23 ships observed in climate models between the overturning and surface western boundary current transpo
24 a leads to major reductions in Pacific Ocean overturning and the loss of the modern North Pacific Dee
25 servations of enhanced cellular stress after overturning and the typically deleterious effects of str
28 ese findings show how changes in upper-ocean overturning associated with millennial-scale events diff
32 reports that a reexamination of the evidence overturns Burke et al.'s findings when alternative stati
33 We anticipated that these drawbacks could be overturned by judicious postsynthetic modification steps
34 ommensal bacteria eradication is efficiently overturned by mono-colonization with either Candida albi
39 er that this was achieved by a sluggish deep overturning cell, comprised of well-mixed northern- and
40 ation, with a maximum in Atlantic Meridional Overturning Circulation (AMOC) 15 years after the 1963 A
41 tion or weakening of the Atlantic meridional overturning circulation (AMOC) and associated northward
42 ed by both reductions in Atlantic Meridional Overturning Circulation (AMOC) and collapses of the West
44 ting the strength of the Atlantic Meridional Overturning Circulation (AMOC) and thereby northward hea
45 response to slow-down of Atlantic meridional overturning circulation (AMOC) during Heinrich Stadial 1
46 with disruptions of the Atlantic Meridional Overturning Circulation (AMOC) during the deglacial peri
47 induced reduction in the Atlantic meridional overturning circulation (AMOC) during the early deglacia
49 lacial periods, when the Atlantic Meridional Overturning Circulation (AMOC) experienced large variati
50 Abrupt changes in the Atlantic meridional overturning circulation (AMOC) have often been invoked t
51 The importance of the Atlantic Meridional Overturning Circulation (AMOC) heat transport for climat
52 quantitative role of the Atlantic Meridional Overturning Circulation (AMOC) in dissolved organic carb
53 o a strengthening of the Atlantic Meridional Overturning Circulation (AMOC) in the first 25 y after t
54 a large reduction in the Atlantic meridional overturning circulation (AMOC) indicates a climate contr
55 with a weakening of the Atlantic Meridional Overturning Circulation (AMOC) inferred from ocean obser
58 tion, ice sheets and the Atlantic meridional overturning circulation (AMOC) on hemispheric temperatur
60 lity associated with the Atlantic Meridional Overturning Circulation (AMOC) undergoes a mode change f
61 ere models indicate that Atlantic meridional overturning circulation (AMOC) variability is tightly li
62 the strengthening of the Atlantic Meridional Overturning Circulation (AMOC) with a signature warming
63 ghly correlated with the Atlantic Meridional Overturning Circulation (AMOC), and its circulation stre
64 ched at 400 ka involving Atlantic Meridional Overturning Circulation (AMOC), inflowing warm Atlantic
65 ained reduction of North Atlantic Meridional Overturning Circulation (AMOC), resulting in an antiphas
66 ests that MOW influenced Atlantic Meridional Overturning Circulation (AMOC), THC, and climatic shifts
67 be driven partly by the Atlantic Meridional Overturning Circulation (AMOC), the atmosphere's dynamic
68 , the variability of the Atlantic meridional overturning circulation (AMOC), which has a role in cont
78 projections of a slowing Atlantic meridional overturning circulation (MOC) in the 21st century, the O
81 suggest a slowdown of the zonal atmospheric overturning circulation above the tropical Pacific Ocean
82 fficient to have reduced Atlantic meridional overturning circulation and caused the Younger Dryas col
83 drup, thus explaining the variability in the overturning circulation and climate during the Younger D
84 resulting changes in the Atlantic Meridional Overturning Circulation and equatorial annual cycle.
85 ayed a crucial role in regulating meridional overturning circulation and global climate changes durin
86 th Atlantic Ocean for a rapid return to deep overturning circulation and high-latitude warming by con
87 face in the Southern Ocean closes the global overturning circulation and is fundamentally important f
88 d with variations in the Atlantic meridional overturning circulation and the more gradual adjustments
89 Antarctica, with implications for the global overturning circulation and the oceanic storage of atmos
90 at times suppressing the Atlantic meridional overturning circulation and triggering abrupt climate ch
91 ing to feedbacks between the strength of the overturning circulation and tropical Pacific hydrology.
92 (AABW) supplies the lower limb of the global overturning circulation and ventilates the abyssal ocean
94 ogenic warming could strengthen the Atlantic overturning circulation at a time when warming and accel
96 e and the restart of the Atlantic meridional overturning circulation at the start of the Bolling-Alle
97 been linked with reduced Atlantic Meridional Overturning Circulation by restricting surface water con
98 orate hypotheses that the deep branch of the overturning circulation declined over the recent past, a
99 hat during the 1990s an enhanced upper-ocean overturning circulation drove increased outgassing of na
100 rved 30% downturn of the Atlantic meridional overturning circulation during 2009-10, and a significan
101 These indicators suggest reduced Atlantic overturning circulation during every cool northern stadi
102 ow that slowdowns of the Atlantic meridional overturning circulation during Heinrich stadials and the
104 servations implying that Atlantic meridional overturning circulation during the Last Glacial Maximum
105 the strength and location of North Atlantic overturning circulation during this period of highly var
106 antic, show that surface Atlantic meridional overturning circulation dynamics likely amplified the re
114 an warming associated with variations in the overturning circulation increases underwater melt along
118 005 and 2010, a weakened Atlantic Meridional Overturning Circulation is the primary driver of positiv
123 transport as part of the Atlantic Meridional Overturning Circulation must be accomplished via subsurf
124 convection is an essential component of the overturning circulation of the Atlantic Ocean, which hel
127 ominant paradigm that the ocean's meridional overturning circulation operates like a conveyor belt, t
131 s in the strength of the Atlantic meridional overturning circulation recorded in marine sediments.
133 st 21-month record reveals a highly variable overturning circulation responsible for the majority of
134 that the uncertainty in the mean meridional overturning circulation strength at upper levels of the
135 tennial scale changes in Atlantic meridional overturning circulation strength in regulating the clima
136 to fluctuations in North Atlantic meridional overturning circulation through its regulation of polewa
137 aviour was the result of Atlantic meridional overturning circulation variability superimposed on a de
138 is the mode and tempo of Atlantic meridional overturning circulation variability, and the significanc
139 inrich event 1, when the Atlantic meridional overturning circulation was weak, pointing to feedbacks
143 es the lower limb of the Atlantic Meridional Overturning Circulation, a critical component of the cli
144 ctic overturning relate to Northern Atlantic overturning circulation, a major driver of Northern Hemi
145 akening and shoaling of the interhemispheric overturning circulation, again consistent with proxy evi
146 hese currents are a driving force for global overturning circulation, and affect climate by modulatin
147 ubpolar North Atlantic is a prerequisite for overturning circulation, and strong freshening could her
148 lead to substantial slowing of the Atlantic overturning circulation, and that meltwater from Antarct
149 tinued weakening of this Atlantic Meridional Overturning Circulation, as projected for the twenty-fir
150 an, with its large surface area and vigorous overturning circulation, is potentially a substantial si
151 elease of freshwater from icebergs drives an overturning circulation, resulting in a ~10% increase in
152 , probably involving the Atlantic meridional overturning circulation, seem to be influencing global c
153 orced a reduction in the Atlantic meridional overturning circulation, thereby causing the Younger Dry
154 ome of a slowdown of the tropical meridional overturning circulation, which compensates for the aeros
155 the deepest limb of the Atlantic Meridional Overturning Circulation, yet questions remain as to wher
156 vative observations of a major branch of the overturning circulation-an abyssal boundary current in t
157 O(2) transport to the ocean interior via the overturning circulation-has received much less attention
158 rent system known as the Atlantic Meridional Overturning Circulation-the strongest oceanic pacemaker
175 We suggest Antarctic sea ice and Atlantic overturning conditions favoured abyssal ocean ventilatio
177 stored methane was emitted during the autumn overturn, contributing approximately 80% of the annual d
182 . do not present enough empirical support to overturn decades of work supporting a number sense nor t
184 gly influence responses to changing climate, overturning direct climatic effects within 5 years.
186 urface flowing salty water that helped drive overturning during past climatic changes is, however, no
189 nditioned the system for a subsequent abrupt overturning event during the Bolling-Allerod interstadia
191 thinner crust by plate tectonics, and mantle overturn following solidification of an early magma ocea
193 stimulation of the skin with ultrasound can overturn healing defects by activating a calcium/CamKina
194 erated in the adult mammalian brain has been overturned; however, endogenous adult neurogenesis appea
196 rtantly, we show numerically that convective overturn in a several-kilometre-thick layer of solid nit
197 ncepts of a hard-wired adult brain have been overturned in recent years by in vivo imaging studies re
199 BP, consistent with synchronous recovery of overturning in both hemispheres and increased Southern O
200 inter sea ice and curtailed meridional ocean overturning in the North Atlantic led to a strong interh
201 orcing are associated with greater mid-depth overturning in the obliquity band but less overturning i
203 g circulation (MOC) in the 21st century, the Overturning in the Subpolar North Atlantic Program (OSNA
204 argued through the analysis of recent OSNAP (Overturning in the Subpolar North Atlantic Program) data
205 ere being a southern component to the global overturning in which about 20 sverdrups (1 Sv = 10(6) m(
206 the prior federal ban that was subsequently overturned, in combination with a threat of litigation,
207 the ice shelf cavity triggers a centrifugal overturning instability that grows by extracting kinetic
212 A predominantly southern-sourced abyssal overturning limb that was more isolated from its shallow
213 sights into the cell biology of genomes have overturned long-held dogmas and have led to new models f
214 ilability of whole genome sequence data have overturned many long-held assumptions about the export a
216 red methane emitted to the atmosphere during overturn may be substantially larger and the fraction of
218 ecular data are upheld, but phenomic signals overturn molecular signals to show Sundatheria (Dermopte
221 ater (NADW), a major component of the global overturning ocean circulation, was significantly more ra
222 in divergence zones and by winter convective overturn of the water column, and the primary production
223 rculation is a large-scale zonal (east-west) overturning of air across the equatorial Pacific Ocean--
224 ce climate - is influenced by the meridional overturning of mass in the stratosphere, the Brewer-Dobs
234 conditions in the hypolimnion and the autumn overturn period represent key factors for the overall an
236 gh, on average 4 mmol m(-2) d(-1) during the overturn period, water column microbial methane oxidatio
239 gnificant intermediate-to-deep Mediterranean overturning perturbation reported by instrumental record
240 n anticipated as air density declines, which overturns prevailing expectations that this species shou
243 results in immediate net benefits globally, overturning previous findings from cost-benefit models t
246 that both the deep water mass source and the overturning rate shifted rapidly and synchronously durin
248 ty, energetics research in red squirrels has overturned several standard pillars of knowledge in phys
249 lity with novel conclusions that appeared to overturn some major results from inclusive fitness.
251 nality closely track changes in the Atlantic overturning strength and support the hypothesis that abr
252 parison of our deep water source record with overturning strength proxies shows that both the deep wa
254 s, including reovirus, have been reported to overturn such immunosuppression and promote the developm
260 ants is an ongoing challenge, the ability to overturn the intrinsic anti-diastereospecificity of thes
261 ysis of previously published albatross data, overturn the notion that albatrosses do not exhibit Levy
264 tablish that a p27(Kip1) deficiency does not overturn the reduced skin tumorigenesis experienced by S
265 l-molecule-like) that predictably enhance or overturn the substrate's inherent reactivity preference
266 he correct orbitals" in chemistry and do not overturn the well-known conclusion that both delocalized
271 en Prize, for nitrogen metabolism (1906) and overturning the concept of active transport of gases acr
272 of order-to-disorder phase transformations, overturning the conventional view that irradiation cause
273 em as potentially autonomous photoreceptors, overturning the dogma that all visual information origin
274 the extinct sabertooth cats and dire wolves-overturning the idea that they heavily competed for simi
275 they are more diverse than assumed hitherto, overturning the long-held paradigm that the early endoph
276 persion behaviour of our hedgehog particles, overturning the notion that like dissolves like, might h
277 ution from finding local fitness optima-thus overturning the traditional assumption that local fitnes
278 stration of long-range hearing in mosquitoes overturns the common assumption that the thread-like ant
281 MMP-9 promoter activity by PAF and that PAF overturns the repressor effect of Sp1 through activation
282 must undergo fundamental conceptual change, overturning their initially human-centered framework bef
284 input stage fed to MT, and MT neurons cannot overturn this bias based on their own feature selectivit
287 the past 5 years have resulted in completely overturning this limitation; indeed, the reaction is now
291 results support the inference that weakened overturning was a driver of Heinrich cooling, while sugg
292 e behaviour suggests that the Southern Ocean overturning was the dominant driver of changes in the At
293 a peak efflux to the atmosphere during fall overturn when 70% of total emissions were released, with
294 held to be a passive process, a concept now overturned with new evidence demonstrating that resoluti
295 arked regional differences in Southern Ocean overturning with distinct South Indian fingerprints on (
297 lts in Earth-like circulations: a meridional overturning with warm water moving poleward at the surfa
298 or Sea contribution to the global meridional overturning, with a linear relationship between time-ave