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1 e extra heat in the ocean during the recent "hiatus".
2 , raising questions about the status of the "hiatus".
3 es in the Northern Hemisphere in winter (the hiatus).
4 ted at this level before transfer across the hiatus.
5 y change rate slowed down during the warming hiatus.
6 ed during a 5.5-month COVID-19-related trial hiatus.
7 ocean heat uptake during the surface warming hiatus.
8 ceans is closely tied to the surface warming hiatus.
9  do the hydrological extremes respond to the hiatus.
10 eration of flash droughts during the warming hiatus.
11 1998, whereas observations suggest a warming hiatus.
12 ern hemisphere before and during the warming hiatus.
13 ce between the greater trochanter and sacral hiatus.
14 ation regimen was repeated following a 7-day hiatus.
15 ,000 and ~11,100 yr BP; interrupted by seven hiatuses.
16 les until present day with only one apparent hiatus (3,400-2,800 YBP).
17 rom global warming to global surface warming hiatus after 1998.
18 tion (GEJ) and the apex of the diaphragmatic hiatus after maximal thoracic esophagus mobilization was
19        The recent global warming slowdown or hiatus after the big El Nino event in 1997/98 raises the
20 97 for 1970-2012 (which includes the current hiatus and a period of accelerated global warming).
21                              Annual banding, hiatuses, and high-precision uranium-series dating show
22  crus of diaphragm which form the esophageal hiatus are arranged like a "noose" around the esophagus.
23 is then shows a 2000-year-long stratigraphic hiatus as well as the recent resurgence of peat accumula
24  years, precluding the possibility of a long hiatus at the boundary and requiring extremely rapid fau
25 r temperature data indicate a global warming hiatus between 1998 and 2012, while its impacts on globa
26                                          The hiatus between oocyte and embryonic gene transcription d
27 cating factor is that there is a significant hiatus between the appearance of the first dispersed spo
28 outcomes support an ecological cause for the hiatus between the Mousterian and Aurignacian technocomp
29 ion in these two basins is not unique to the hiatus but is characteristic of anthropogenic warming an
30 lication superior margin was fixed below the hiatus, but over the GEJ.
31 s, epidural catheters inserted at the sacral hiatus can easily be advanced to a lumbar or thoracic le
32               This confirms that sedimentary hiatuses can span a substantial proportion of geological
33 over continental areas-namely, local warming hiatus-can be accompanied by excessive heat accumulation
34                     After a 4-week treatment hiatus, clinical responders were eligible to continue IL
35                                          The hiatuses coincide with regional tectonic events and chan
36 ns of changes in sedimentation rate (such as hiatuses, condensation, or lateral expansion) can be use
37  extending from a superiorly placed ureteral hiatus distally to the trigone.
38 dly reduced C accumulation and potentially a hiatus during the peat dome stage.
39                              After a 14-year hiatus, epidemic cholera swept through Burundi between J
40 shows an anomalous warming below 50 m during hiatus events due to an enhanced heat transport by the I
41                     Although similar decadal hiatus events may occur in the future, the multi-decadal
42 ew clumped isotope temperature record from a hiatus-free, expanded KPg boundary section from Seymour
43                   Remarkably, after a 5-year hiatus from in-person conferences, the 14th Internationa
44 al pattern remained intact even after a 3-mo hiatus from training.
45 uminescence ages reveal a common sedimentary hiatus from ~26 to ~17 thousand years ago (ka), reflecti
46 ore relationships between changes in genital hiatus (GH) and development of pelvic organ prolapse usi
47 on triggered by alluvial deposition, if such hiatuses have a heavy-tailed length distribution.
48 non that has been dubbed the global warming "hiatus." Here, we present an updated global surface temp
49 ents without hiatus hernia (NHH), and 7 with hiatus hernia (HH) were studied.
50 nts had Barrett's esophagus (n = 25, 51.0%), hiatus hernia (n = 26, 53.1%), esophagitis (n = 10, 20.4
51 ormal subjects (NL), 9 GERD patients without hiatus hernia (NHH), and 7 with hiatus hernia (HH) were
52 , while 38.6% had incompetent cardia without hiatus hernia and 26.2% with hiatus hernia.
53          In 1926, Akerlund proposed the term hiatus hernia and classified HH into the 3 types that we
54                         Six subjects without hiatus hernia had endoclips placed at the squamocolumnar
55                              Repair of large hiatus hernia is associated with radiological recurrence
56 ral or umbilical hernia repair (n = 19), and hiatus hernia repair (n = 10).
57  randomized controlled trial of 3 methods of hiatus hernia repair; sutures versus absorbable mesh ver
58         Caucasian ethnicity, the presence of hiatus hernia, and alcohol consumption were all associat
59 ed with reflux of stomach acid and usually a hiatus hernia, and it strongly predisposes to esophageal
60 reasing length of Barrett esophagus, size of hiatus hernia, and severity of acid reflux.
61 nificant differences were seen for recurrent hiatus hernia, and the clinical differences were unlikel
62  confirmed a gastric adenocarcinoma within a hiatus hernia, which had fistulated to the pericardium.
63  cardia without hiatus hernia and 26.2% with hiatus hernia.
64 ble or nonabsorbable mesh in repair of large hiatus hernias reduces the risk of recurrence, compared
65  up to 30% of patients after repair of large hiatus hernias, and mesh repair has been proposed as a s
66 s trial do not support mesh repair for large hiatus hernias.
67 quamocolumnar junction (SCJ) was beneath the hiatus in all control subjects.
68 ening aperture occurred at the diaphragmatic hiatus in all subjects.
69 s inconsistent with an apparent billion-year hiatus in glaciation.
70 te, the character of the ENSO cycle, and the hiatus in global surface warming.
71 rious mechanisms have been proposed for this hiatus in global warming, but their relative importance
72  archaeological sites, where the YDB marks a hiatus in human occupation or major changes in site use.
73                             A nearly 20-year hiatus in major seismic activity in southern California
74 ling in the GoP exacerbated a climate-driven hiatus in reef development in the late Holocene.
75 The principal cause of this millennial-scale hiatus in reef growth was increased variability of the E
76                          Despite an apparent hiatus in rising temperature and no significant trend in
77  and others have interpreted this widespread hiatus in sedimentation on the continents as a failure o
78                   These red clays indicate a hiatus in successive volcanic eruptions.
79 ue to internal variability, there might be a hiatus in the decline of September Arctic sea ice.
80 e question of global warming and the present hiatus in the global mean surface temperature.
81 haping climate trends and the global warming hiatus in the northern hemisphere.
82 he base of the dune, there is an ~ 8000-year hiatus in the record.
83 ent stents were deployed across the adductor hiatus in the same limbs.
84  general slowdown in magmatic activity and a hiatus in volcanism may have contributed to extreme diff
85                            We find that this hiatus in warming coincides with a period of little incr
86 seamounts, and are commonly linked to growth hiatuses in ferromanganese (Fe-Mn) crusts.
87 w discontinuities caused by obliquity-driven hiatuses in ice accumulation, forming internal debris la
88 ransect volume, even for scenarios with long hiatuses in preserved geochemical signals.
89 state behaviour can be explained by episodic hiatuses in river incision triggered by alluvial deposit
90 terature have frequently cited a "pause" or "hiatus" in global warming.
91  that there are multiple definitions of the "hiatus" in the literature, with its presumed onset spann
92 seasonal and regional characteristics of the hiatus, including the intensified Walker circulation, th
93                                 Depositional hiatuses indicate erosion by bottom currents related to
94 tending to the diaphragm near the esophageal hiatus; inferiorly, extending to the pelvis along the an
95            Our results show that the current hiatus is part of natural climate variability, tied spec
96          To examine whether the notion of a "hiatus" is justified by the available data, we first doc
97                The resulting surface warming hiatus lasts for 40-50 years.
98 Moreover, the recent global surface warming "hiatus" may be attributed to the SPNA as one of the majo
99           We assessed the LES and esophageal hiatus morphology using a block containing the human LES
100                                              Hiatuses most likely correspond to permafrost developmen
101 osits after a approximately 900-million year hiatus, occur shortly before the approximately 2.3-2.2 G
102 ross over" to review the other group after a hiatus of at least 8 weeks.
103 lantic and Southern Oceans during the recent hiatus of global warming.
104                                      After a hiatus of more than 20 years, three new medications appr
105                                  Following a hiatus of more than 500 years, the North Caucasian stepp
106                                            A hiatus of several decades followed, during which the imp
107 ur results suggest a possible recent warming hiatus on the northwestern TP.
108 fundoplication was undertaken for a patulous hiatus or large hiatal hernia or to buttress the repair
109                In late 2011, after a 12-year hiatus, oral vaccines against adenovirus types 4 (Ad4) a
110                               After a 4-week hiatus, patients with a response could receive interleuk
111 ibetan Plateau (TP), even during the warming hiatus period.
112 , which reached levels of 400 ppm during the hiatus period.
113 ne occurred during the recent global warming hiatus period.
114 ) were included in the calculation, alleged "hiatus" periods notwithstanding.
115 he warming effect of the adjusted SAT in the hiatus process.
116 al muscle of the crural diaphragm (esophagus hiatus) provide the sphincter mechanisms at the esophago
117 frequency was highly correlated with the SCJ-hiatus separation (r = 0.76; P < 0.001).
118         Eight GERD patients with >/=1-cm SCJ-hiatus separation were considered hernia patients, and 7
119 XNET measurements, mainly within the warming hiatus, shows that there were no widespread advancing (o
120 butes about 10% to the recent global warming hiatus since 1999.
121 slowdown (GSWS) or so-called "global warming hiatus" since the end of the 20(th) century.
122 tional to the separation between the SCJ and hiatus, suggesting that the perturbed anatomy associated
123 f the erosional event(s) and/or depositional hiatus that lead to its development are unknown.
124                        After a COVID-related hiatus, the fifth biennial symposium on Evolution and Co
125                 The analysis shows that the "hiatus" trends are encompassed within the overall distri
126             The median duration of treatment hiatus was 12 months.
127                                          The hiatus was a Pacific-wide phenomenon with an underlying
128                     We hypothesize that this hiatus was climate-driven and forced hunter-gatherers to
129 troesophageal junction and the diaphragmatic hiatus were 0.88 and 0.85, respectively.
130 y years of stripe rust research, the 20-year hiatus when stripe rust was not considered important and
131 dual migrations were punctuated by a 7-month hiatus, when crabs remained stationary, coincident with
132                 Closure of the diaphragmatic hiatus with crural sutures alone vs a tension-free techn
133                 The results also connect the hiatus with diminished contrast between temperatures ove
134 ic relationships, such as facies changes and hiatuses, within the deposit.

 
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