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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
13                            These conclusions overturn a long-held view that such EPR signals in bovin
14                                These results overturn a long-standing dogma in the study of sensorine
15                          Recent reports have overturned a series of dogmas that have been well entren
16                                         This overturning also influences the uptake and storage of an
17 discharge, instigated by regional vegetation overturn and enhanced monsoon precipitation.
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
21                                          The overturning and withdrawal of several of the Office of R
22                  Philip Morris (PM) ignored, overturned, and weakened various attempts to restrict to
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
25                 In some cases, the interface overturns before returning to the initial, flat configur
26 fires, and soil carbon decay; and (iv) ocean overturn bringing high-CO2 water to the surface.
27 reports that a reexamination of the evidence overturns Burke et al.'s findings when alternative stati
28                              This theory was overturned by empirical studies that found food webs to
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
31 ity, 1.829 (95% CI: 1.005 to 3.329) that was overturned by sensitivity analysis.
32                This historical view has been overturned by the finding that genomes of even closely-r
33 ponse to hydrodynamic cues characteristic of overturning by Kolmogorov-scale eddies.
34                   Interannual changes in the overturning can be monitored with a resolution of 1.5 Sv
35           The Hadley circulation, a tropical overturning cell responsible for trade winds, largely co
36 hat ventilation ages in the southern-sourced overturning cell were significantly increased.
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
42                      The Atlantic Meridional Overturning Circulation (AMOC) exhibits two stable state
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
49                      The Atlantic Meridional Overturning Circulation (AMOC) is an important component
50        A collapse of the Atlantic Meridional Overturning Circulation (AMOC) leads to global cooling t
51 tion, ice sheets and the Atlantic meridional overturning circulation (AMOC) on hemispheric temperatur
52                      The Atlantic meridional overturning circulation (AMOC) transports warm salty sur
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
62 iyear predictions of the Atlantic Meridional Overturning Circulation (AMOC).
63 ened the strength of the Atlantic Meridional Overturning Circulation (AMOC).
64 h, namely changes in the Atlantic meridional overturning circulation (AMOC).
65 e was a weakening of the Atlantic Meridional Overturning Circulation (AMOC).
66 /=400 year) deepening of Atlantic Meridional Overturning Circulation (AMOC).
67 ght to have strengthened Atlantic Meridional Overturning Circulation (AMOC).
68 lation, specifically the Atlantic Meridional Overturning Circulation (AMOC).
69             The vigor of Atlantic meridional overturning circulation (MOC) is thought to be vulnerabl
70                      The Atlantic meridional overturning circulation (MOC), which provides one-quarte
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.
82 The factors driving glacial changes in ocean overturning circulation are not well understood.
83 ogenic warming could strengthen the Atlantic overturning circulation at a time when warming and accel
84             Here we investigate the Atlantic overturning circulation at the Last Glacial Maximum and
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
88                      The Atlantic meridional overturning circulation carries warm upper waters into f
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
93 processes-and use it to reconstruct Atlantic overturning circulation during the last 800 kyr.
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
97 tions in the rate of the Atlantic meridional overturning circulation for abrupt climate changes.
98                                  The oceanic overturning circulation has a central role in the Earth'
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
101 ought to be linked to changes in the mode of overturning circulation in the Atlantic Ocean.
102 ly reflects the depth of the mean meridional overturning circulation in the basin.
103 gulhas leakage', forms a choke point for the overturning circulation in the global ocean.
104        Projected weakening of the meridional overturning circulation in the North Atlantic Ocean does
105 raphy, giving rise to a short circuit of the overturning circulation in these regions.
106 an warming associated with variations in the overturning circulation increases underwater melt along
107          The strength of Atlantic meridional overturning circulation is believed to affect the climat
108  been possible to detect whether the ocean's overturning circulation is changing, but recent evidence
109                                 The Atlantic overturning circulation is declining and the AMO is movi
110                While the ocean's large-scale overturning circulation is thought to have been signific
111  such a significant downturn of the Atlantic overturning circulation is very unusual.
112                      The Atlantic meridional overturning circulation is widely believed to affect cli
113 ons, a disruption of the Atlantic meridional overturning circulation leads to a collapse of the North
114               The shallower interhemispheric overturning circulation makes room for slowly moving wat
115        Here we show that a deep and vigorous overturning circulation mode has persisted for most of t
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
119                                          The overturning circulation of the ocean plays an important
120                                  The shallow overturning circulation of the oceans transports heat fr
121 ominant paradigm that the ocean's meridional overturning circulation operates like a conveyor belt, t
122                     Zonal mean stratospheric overturning circulation organizes the transport of ozone
123 esized to originate from Atlantic meridional overturning circulation oscillations.
124 s in the strength of the Atlantic meridional overturning circulation recorded in marine sediments.
125  hydroclimate in helping Atlantic Meridional Overturning Circulation recovery during D-O events.
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
132  This trend reversed during the 2000s as the overturning circulation weakened.
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
135 te heat depending on the state of meridional overturning circulation within the Atlantic Ocean.
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
145 nd reinvigoration of the Atlantic meridional overturning circulation.
146  triggered by a weakened Atlantic meridional overturning circulation.
147  is an important process in the global ocean overturning circulation.
148 the near collapse of the Atlantic Meridional Overturning Circulation.
149 de and variations in the Atlantic meridional overturning circulation.
150 sing the deep branch of the ocean meridional overturning circulation.
151 nce on the upwelling branch of the Antarctic overturning circulation.
152 red when considering the Atlantic meridional overturning circulation.
153 n attendant reduction in Atlantic meridional overturning circulation.
154 Atlantic hydrologic cycle and North Atlantic overturning circulation.
155  downwelling limb of the Atlantic meridional overturning circulation.
156 l to that portion of the Atlantic meridional overturning circulation.
157 sitive to changes in the Atlantic meridional overturning circulation.
158 iderations of continuity in the global ocean overturning circulation.
159  suggests a mechanism for closing the global overturning circulation.
160 n hypothesised to be controlled by Antarctic overturning circulation.
161                              Furthermore, we overturn claims that chirality in the structure of the a
162                       Overall, these results overturn common beliefs and call for a specific handling
163 r the observed systems will be confirmed (or overturned) confidently in the near future.
164 stored methane was emitted during the autumn overturn, contributing approximately 80% of the annual d
165 h the outermost 30% of the Sun's interior by overturning convective motions.
166                                  The results overturn conventional wisdom that soluble ligands are al
167                          The ability to fast overturn could reduce the danger of dying.
168 . do not present enough empirical support to overturn decades of work supporting a number sense nor t
169                               These findings overturn decades-old ideas about primate vocalizations a
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
173 ficant reduction, although not cessation, of overturning during Heinrich Stadial 1.
174 urface flowing salty water that helped drive overturning during past climatic changes is, however, no
175                              Periods of lake overturn (during fall/winter) are short and therefore di
176                                      Here we overturn entrenched doctrine that uncritically treats bo
177 nditioned the system for a subsequent abrupt overturning event during the Bolling-Allerod interstadia
178                                 Our findings overturn existing models for Polycomb recruitment by Xis
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
181 nist in an ultimately successful campaign to overturn gene patents in court.
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
185             Predator saturation can actually overturn hyperpredation into hypopredation, an increase
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
188               Although this concept has been overturned in recent years, there is no unique mechanism
189  BP, consistent with synchronous recovery of overturning in both hemispheres and increased Southern O
190 ble the patterns of large-scale axisymmetric overturning in the Earth's atmosphere.
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
193 h overturning in the obliquity band but less overturning in the precession band.
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
197                        The year-long average overturning is 18.7 +/- 5.6 sverdrups (Sv) (range: 4.0 t
198       Continued weakening of the upper-ocean overturning is likely to strengthen the CO2 sink in the
199                  This suggests that Atlantic overturning is strongly sensitive to factors beyond ice
200 ace voluminous lava flows or by a cyclically overturning lava lake contained within the patera.
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
204 oxide, we calculate the global mean diabatic overturning mass flux throughout the stratosphere.
205 red methane emitted to the atmosphere during overturn may be substantially larger and the fraction of
206                    However, changes in ocean overturning may not produce the same effects globally as
207 ecular data are upheld, but phenomic signals overturn molecular signals to show Sundatheria (Dermopte
208                                      It also overturns more than a century of received wisdom regardi
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
216 er the ripples, typically without leading to overturning of the free surface.
217 tions of the mean strength of the meridional overturning of the stratosphere.
218              This, in turn, weakens the mass overturning of the tropical circulation.
219       Several findings in those studies have overturned old paradigms about the immune system and led
220                   Although the case could be overturned on appeal, it will probably change how gene p
221                However, this proposition was overturned on the basis of extensive kinetic analysis.
222 cean out-gassing during post-glacial oceanic overturn or methane hydrate destabilization.
223 ent well-being, especially if a diagnosis is overturned or modified years after treatment.
224 ar Pathology v Myriad Genetics, Inc seeks to overturn patents on isolated genes.
225 conditions in the hypolimnion and the autumn overturn period represent key factors for the overall an
226                                    After the overturn period, the entire water column was oxic, and o
227 gh, on average 4 mmol m(-2) d(-1) during the overturn period, water column microbial methane oxidatio
228 ane is released to the atmosphere during the overturn period.
229 mating the flux of methane from lakes during overturn periods.
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
232                   Our experiments and theory overturn previous hypotheses that suggest that blooming
233 s designed to bind promoter DNA, potentially overturning previous assumptions about mechanism.
234 that both the deep water mass source and the overturning rate shifted rapidly and synchronously durin
235                           This view has been overturned recently by demonstrating ionic conductivity
236            How these variations in Antarctic overturning relate to Northern Atlantic overturning circ
237 lity with novel conclusions that appeared to overturn some major results from inclusive fitness.
238                 Early user test results that overturned some of our intuitions strengthened our commi
239 ative importance of these two components and overturned some previously held notions.
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
242 "overshoot" events, with Atlantic meridional overturning stronger than that of the modern era.
243 s, including reovirus, have been reported to overturn such immunosuppression and promote the developm
244                                      Here we overturn that assumption and demonstrate that beta-pleat
245                               These findings overturn the conventional view, demonstrating that the c
246                                     Our data overturn the current paradigm that recruitment and phosp
247                  Collectively, these results overturn the current working hypothesis and suggest, ins
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
251        In this issue of Neuron, Frank et al. overturn the notion that synaptic homeostasis at Drosoph
252                                  Our results overturn the paradigm attributing these phenomena to the
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
255              Recent advances have completely overturned the classical view of chromosome segregation
256                     In vivo studies have now overturned the dogma that robust plasticity is limited t
257         Recent archaeobotanical evidence has overturned the notion of a rapid transition, resulting i
258                     Molecular dating largely overturned the paradigm that global cooling during recen
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
264                                         This overturns the established view that metal-ketimide linka
265                  This dual role for dopamine overturns the previous model that octopamine signalled r
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
268                         Recent findings have overturned theories emphasizing behavioral inhibition as
269 xperiments on the 4f-electron metal Yb2Pt2Pb overturn this conventional wisdom.
270                                      Here we overturn this established picture by observing an intens
271 the past 5 years have resulted in completely overturning this limitation; indeed, the reaction is now
272 n region, exciting work in the past years is overturning this notion.
273 illion-year-old teleost relative Aetheretmon overturns this long-held hypothesis.
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
277                  We find that the meridional overturning was nearly, or completely, eliminated during
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
280                              That belief was overturned when a transposing F subfamily, T(F), was dis
281  held to be a passive process, a concept now overturned with new evidence demonstrating that resoluti
282                   Upon experiencing repeated overturning with timescales and statistics representativ
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
285                                        Major overturn within a magma chamber can bring together felsi

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