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1 causes: a giant impact or mantle convection/overturn.
2 ion of the stored methane is oxidized during overturns.
3 very established "rule" seems destined to be overturned.
4 weakness of this connection, the concept is overturned.
5 t necessarily require a complete shutdown of overturning.
6 ich event 1 could have only affected shallow overturning.
7 the structure and variability of the ocean's overturning.
8 icit in models of the average Southern Ocean overturning.
9 vide insufficient constraints on the rate of overturning.
10 harp northern warming followed reinvigorated overturning.
11 the abrupt resumption of Atlantic meridional overturning.
12 stablished dogma of 'horror autotoxicus' was overturned 50 years ago with the publication of a paper
18 d by melt extraction in the mantle wedge, is overturned and re-introduced beneath the back-arc basin
19 a leads to major reductions in Pacific Ocean overturning and the loss of the modern North Pacific Dee
20 servations of enhanced cellular stress after overturning and the typically deleterious effects of str
23 ese findings show how changes in upper-ocean overturning associated with millennial-scale events diff
24 emisphere overturning to Northern Hemisphere overturning at the start of the Palaeocene/Eocene Therma
27 reports that a reexamination of the evidence overturns Burke et al.'s findings when alternative stati
29 We anticipated that these drawbacks could be overturned by judicious postsynthetic modification steps
30 ommensal bacteria eradication is efficiently overturned by mono-colonization with either Candida albi
37 er that this was achieved by a sluggish deep overturning cell, comprised of well-mixed northern- and
38 ation, with a maximum in Atlantic Meridional Overturning Circulation (AMOC) 15 years after the 1963 A
39 ed by both reductions in Atlantic Meridional Overturning Circulation (AMOC) and collapses of the West
40 with disruptions of the Atlantic Meridional Overturning Circulation (AMOC) during the deglacial peri
41 induced reduction in the Atlantic meridional overturning circulation (AMOC) during the early deglacia
43 Abrupt changes in the Atlantic meridional overturning circulation (AMOC) have often been invoked t
44 The importance of the Atlantic Meridional Overturning Circulation (AMOC) heat transport for climat
45 quantitative role of the Atlantic Meridional Overturning Circulation (AMOC) in dissolved organic carb
46 o a strengthening of the Atlantic Meridional Overturning Circulation (AMOC) in the first 25 y after t
47 a large reduction in the Atlantic meridional overturning circulation (AMOC) indicates a climate contr
48 with a weakening of the Atlantic Meridional Overturning Circulation (AMOC) inferred from ocean obser
51 tion, ice sheets and the Atlantic meridional overturning circulation (AMOC) on hemispheric temperatur
53 lity associated with the Atlantic Meridional Overturning Circulation (AMOC) undergoes a mode change f
54 ere models indicate that Atlantic meridional overturning circulation (AMOC) variability is tightly li
55 the strengthening of the Atlantic Meridional Overturning Circulation (AMOC) with a signature warming
56 ghly correlated with the Atlantic Meridional Overturning Circulation (AMOC), and its circulation stre
57 ed at 400 ka involving Atlantic Meridional Overturning Circulation (AMOC), inflowing warm Atlantic
58 ained reduction of North Atlantic Meridional Overturning Circulation (AMOC), resulting in an antiphas
59 ests that MOW influenced Atlantic Meridional Overturning Circulation (AMOC), THC, and climatic shifts
60 be driven partly by the Atlantic Meridional Overturning Circulation (AMOC), the atmosphere's dynamic
61 , the variability of the Atlantic meridional overturning circulation (AMOC), which has a role in cont
71 suggest a slowdown of the zonal atmospheric overturning circulation above the tropical Pacific Ocean
72 s been used as a baseline for estimating the overturning circulation and associated heat transport.
73 fficient to have reduced Atlantic meridional overturning circulation and caused the Younger Dryas col
74 drup, thus explaining the variability in the overturning circulation and climate during the Younger D
75 resulting changes in the Atlantic Meridional Overturning Circulation and equatorial annual cycle.
76 ayed a crucial role in regulating meridional overturning circulation and global climate changes durin
77 th Atlantic Ocean for a rapid return to deep overturning circulation and high-latitude warming by con
78 face in the Southern Ocean closes the global overturning circulation and is fundamentally important f
79 d with variations in the Atlantic meridional overturning circulation and the more gradual adjustments
80 at times suppressing the Atlantic meridional overturning circulation and triggering abrupt climate ch
81 ing to feedbacks between the strength of the overturning circulation and tropical Pacific hydrology.
83 ogenic warming could strengthen the Atlantic overturning circulation at a time when warming and accel
85 e and the restart of the Atlantic meridional overturning circulation at the start of the Bolling-Alle
86 a central role to the wind-driven meridional overturning circulation between the tropical and subtrop
87 been linked with reduced Atlantic Meridional Overturning Circulation by restricting surface water con
89 hat during the 1990s an enhanced upper-ocean overturning circulation drove increased outgassing of na
90 rved 30% downturn of the Atlantic meridional overturning circulation during 2009-10, and a significan
91 These indicators suggest reduced Atlantic overturning circulation during every cool northern stadi
92 ow that slowdowns of the Atlantic meridional overturning circulation during Heinrich stadials and the
94 servations implying that Atlantic meridional overturning circulation during the Last Glacial Maximum
95 the strength and location of North Atlantic overturning circulation during this period of highly var
96 antic, show that surface Atlantic meridional overturning circulation dynamics likely amplified the re
99 servations over the past 50 years, that this overturning circulation has been slowing down since the
100 arison suggests that the Atlantic meridional overturning circulation has slowed by about 30 per cent
106 an warming associated with variations in the overturning circulation increases underwater melt along
108 been possible to detect whether the ocean's overturning circulation is changing, but recent evidence
113 ons, a disruption of the Atlantic meridional overturning circulation leads to a collapse of the North
116 transport as part of the Atlantic Meridional Overturning Circulation must be accomplished via subsurf
117 convection is an essential component of the overturning circulation of the Atlantic Ocean, which hel
118 the three main centres of the global, zonal overturning circulation of the equatorial atmosphere (ge
121 ominant paradigm that the ocean's meridional overturning circulation operates like a conveyor belt, t
124 s in the strength of the Atlantic meridional overturning circulation recorded in marine sediments.
126 that the uncertainty in the mean meridional overturning circulation strength at upper levels of the
127 tennial scale changes in Atlantic meridional overturning circulation strength in regulating the clima
128 to fluctuations in North Atlantic meridional overturning circulation through its regulation of polewa
129 aviour was the result of Atlantic meridional overturning circulation variability superimposed on a de
130 is the mode and tempo of Atlantic meridional overturning circulation variability, and the significanc
131 inrich event 1, when the Atlantic meridional overturning circulation was weak, pointing to feedbacks
133 Reorganizations of the Atlantic meridional overturning circulation were associated with large and a
134 s that rapid accelerations of the meridional overturning circulation were concurrent with the two str
136 continental Europe, and any slowdown in the overturning circulation would have profound implications
137 ctic overturning relate to Northern Atlantic overturning circulation, a major driver of Northern Hemi
138 akening and shoaling of the interhemispheric overturning circulation, again consistent with proxy evi
139 port of water closing the ocean's meridional overturning circulation, and thus needs to be represente
140 /230Th, a kinematic proxy for the meridional overturning circulation, in a sediment core from the sub
141 an, with its large surface area and vigorous overturning circulation, is potentially a substantial si
142 , probably involving the Atlantic meridional overturning circulation, seem to be influencing global c
143 orced a reduction in the Atlantic meridional overturning circulation, thereby causing the Younger Dry
144 ome of a slowdown of the tropical meridional overturning circulation, which compensates for the aeros
164 stored methane was emitted during the autumn overturn, contributing approximately 80% of the annual d
168 . do not present enough empirical support to overturn decades of work supporting a number sense nor t
170 olcanic front, diminished melting within the overturned depleted mantle farther from the corner and n
171 gly influence responses to changing climate, overturning direct climatic effects within 5 years.
172 sistent neurogenesis in the adult brain have overturned dogma, provoked reevaluation of cellular plas
174 urface flowing salty water that helped drive overturning during past climatic changes is, however, no
177 nditioned the system for a subsequent abrupt overturning event during the Bolling-Allerod interstadia
179 thinner crust by plate tectonics, and mantle overturn following solidification of an early magma ocea
180 tamate N-methyl-D-aspartate (NMDA) receptor, overturns fundamental axioms of biology as well as those
182 ing that its activation is not sufficient to overturn growth inhibition due to diminished ERK1/2 acti
183 stimulation of the skin with ultrasound can overturn healing defects by activating a calcium/CamKina
184 erated in the adult mammalian brain has been overturned; however, endogenous adult neurogenesis appea
186 rtantly, we show numerically that convective overturn in a several-kilometre-thick layer of solid nit
187 ncepts of a hard-wired adult brain have been overturned in recent years by in vivo imaging studies re
189 BP, consistent with synchronous recovery of overturning in both hemispheres and increased Southern O
191 inter sea ice and curtailed meridional ocean overturning in the North Atlantic led to a strong interh
192 orcing are associated with greater mid-depth overturning in the obliquity band but less overturning i
194 ere being a southern component to the global overturning in which about 20 sverdrups (1 Sv = 10(6) m(
195 the prior federal ban that was subsequently overturned, in combination with a threat of litigation,
196 the ice shelf cavity triggers a centrifugal overturning instability that grows by extracting kinetic
201 A predominantly southern-sourced abyssal overturning limb that was more isolated from its shallow
202 sights into the cell biology of genomes have overturned long-held dogmas and have led to new models f
203 ilability of whole genome sequence data have overturned many long-held assumptions about the export a
205 red methane emitted to the atmosphere during overturn may be substantially larger and the fraction of
207 ecular data are upheld, but phenomic signals overturn molecular signals to show Sundatheria (Dermopte
209 ransient increase in core heat flux after an overturn of an initially stratified lunar mantle might e
210 aphically linked phenomena suggests that the overturn of anoxic deep oceans during the Late Permian i
211 aphically linked phenomena suggests that the overturn of anoxic deep oceans during the Late Permian i
212 ctions are strong enough to cause continuous overturn of species, in contrast to our previous Webworl
213 in divergence zones and by winter convective overturn of the water column, and the primary production
214 rculation is a large-scale zonal (east-west) overturning of air across the equatorial Pacific Ocean--
215 ce climate - is influenced by the meridional overturning of mass in the stratosphere, the Brewer-Dobs
225 conditions in the hypolimnion and the autumn overturn period represent key factors for the overall an
227 gh, on average 4 mmol m(-2) d(-1) during the overturn period, water column microbial methane oxidatio
230 gnificant intermediate-to-deep Mediterranean overturning perturbation reported by instrumental record
231 n anticipated as air density declines, which overturns prevailing expectations that this species shou
234 that both the deep water mass source and the overturning rate shifted rapidly and synchronously durin
237 lity with novel conclusions that appeared to overturn some major results from inclusive fitness.
240 nality closely track changes in the Atlantic overturning strength and support the hypothesis that abr
241 parison of our deep water source record with overturning strength proxies shows that both the deep wa
243 s, including reovirus, have been reported to overturn such immunosuppression and promote the developm
248 veys of pathological gambling may eventually overturn the established wisdom about pathological gambl
249 ants is an ongoing challenge, the ability to overturn the intrinsic anti-diastereospecificity of thes
250 ysis of previously published albatross data, overturn the notion that albatrosses do not exhibit Levy
253 tablish that a p27(Kip1) deficiency does not overturn the reduced skin tumorigenesis experienced by S
254 l-molecule-like) that predictably enhance or overturn the substrate's inherent reactivity preference
259 is mixing occurs where internal waves break, overturning the density stratification of the ocean and
260 em as potentially autonomous photoreceptors, overturning the dogma that all visual information origin
261 -mediated aldol reaction of methyl ketone 7 (overturning the inherent substrate induction from the al
262 they are more diverse than assumed hitherto, overturning the long-held paradigm that the early endoph
263 persion behaviour of our hedgehog particles, overturning the notion that like dissolves like, might h
266 MMP-9 promoter activity by PAF and that PAF overturns the repressor effect of Sp1 through activation
267 must undergo fundamental conceptual change, overturning their initially human-centered framework bef
271 the past 5 years have resulted in completely overturning this limitation; indeed, the reaction is now
274 nd to stabilize the upper atmosphere against overturning, thus increasing the soot lifetime, and to a
275 on patterns changed from Southern Hemisphere overturning to Northern Hemisphere overturning at the st
276 results support the inference that weakened overturning was a driver of Heinrich cooling, while sugg
278 e behaviour suggests that the Southern Ocean overturning was the dominant driver of changes in the At
279 a peak efflux to the atmosphere during fall overturn when 70% of total emissions were released, with
281 held to be a passive process, a concept now overturned with new evidence demonstrating that resoluti
283 lts in Earth-like circulations: a meridional overturning with warm water moving poleward at the surfa
284 ertical distribution of temperature promotes overturning, with colder water over warmer, while the sa
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