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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 ocean heat uptake during the surface warming hiatus.
4 ceans is closely tied to the surface warming hiatus.
5  do the hydrological extremes respond to the hiatus.
6 eration of flash droughts during the warming hiatus.
7 1998, whereas observations suggest a warming hiatus.
8 ce between the greater trochanter and sacral hiatus.
9 ation regimen was repeated following a 7-day hiatus.
10 ted at this level before transfer across the hiatus.
11 les until present day with only one apparent hiatus (3,400-2,800 YBP).
12 rom global warming to global surface warming hiatus after 1998.
13        The recent global warming slowdown or hiatus after the big El Nino event in 1997/98 raises the
14 97 for 1970-2012 (which includes the current hiatus and a period of accelerated global warming).
15                              Annual banding, hiatuses, and high-precision uranium-series dating show
16  crus of diaphragm which form the esophageal hiatus are arranged like a "noose" around the esophagus.
17 is then shows a 2000-year-long stratigraphic hiatus as well as the recent resurgence of peat accumula
18  years, precluding the possibility of a long hiatus at the boundary and requiring extremely rapid fau
19                                          The hiatus between oocyte and embryonic gene transcription d
20 cating factor is that there is a significant hiatus between the appearance of the first dispersed spo
21 ion in these two basins is not unique to the hiatus but is characteristic of anthropogenic warming an
22 s, epidural catheters inserted at the sacral hiatus can easily be advanced to a lumbar or thoracic le
23                     After a 4-week treatment hiatus, clinical responders were eligible to continue IL
24                                          The hiatuses coincide with regional tectonic events and chan
25  extending from a superiorly placed ureteral hiatus distally to the trigone.
26 dly reduced C accumulation and potentially a hiatus during the peat dome stage.
27                              After a 14-year hiatus, epidemic cholera swept through Burundi between J
28 shows an anomalous warming below 50 m during hiatus events due to an enhanced heat transport by the I
29                     Although similar decadal hiatus events may occur in the future, the multi-decadal
30 ew clumped isotope temperature record from a hiatus-free, expanded KPg boundary section from Seymour
31 al pattern remained intact even after a 3-mo hiatus from training.
32 on triggered by alluvial deposition, if such hiatuses have a heavy-tailed length distribution.
33 non that has been dubbed the global warming "hiatus." Here, we present an updated global surface temp
34 ents without hiatus hernia (NHH), and 7 with hiatus hernia (HH) were studied.
35 ormal subjects (NL), 9 GERD patients without hiatus hernia (NHH), and 7 with hiatus hernia (HH) were
36          In 1926, Akerlund proposed the term hiatus hernia and classified HH into the 3 types that we
37                         Six subjects without hiatus hernia had endoclips placed at the squamocolumnar
38                              Repair of large hiatus hernia is associated with radiological recurrence
39 ral or umbilical hernia repair (n = 19), and hiatus hernia repair (n = 10).
40         Caucasian ethnicity, the presence of hiatus hernia, and alcohol consumption were all associat
41 ed with reflux of stomach acid and usually a hiatus hernia, and it strongly predisposes to esophageal
42 reasing length of Barrett esophagus, size of hiatus hernia, and severity of acid reflux.
43 nificant differences were seen for recurrent hiatus hernia, and the clinical differences were unlikel
44  confirmed a gastric adenocarcinoma within a hiatus hernia, which had fistulated to the pericardium.
45 ble or nonabsorbable mesh in repair of large hiatus hernias reduces the risk of recurrence, compared
46 quamocolumnar junction (SCJ) was beneath the hiatus in all control subjects.
47 ening aperture occurred at the diaphragmatic hiatus in all subjects.
48 rious mechanisms have been proposed for this hiatus in global warming, but their relative importance
49  archaeological sites, where the YDB marks a hiatus in human occupation or major changes in site use.
50 The principal cause of this millennial-scale hiatus in reef growth was increased variability of the E
51                          Despite an apparent hiatus in rising temperature and no significant trend in
52  and others have interpreted this widespread hiatus in sedimentation on the continents as a failure o
53 ue to internal variability, there might be a hiatus in the decline of September Arctic sea ice.
54 e question of global warming and the present hiatus in the global mean surface temperature.
55                            We find that this hiatus in warming coincides with a period of little incr
56 state behaviour can be explained by episodic hiatuses in river incision triggered by alluvial deposit
57 terature have frequently cited a "pause" or "hiatus" in global warming.
58  that there are multiple definitions of the "hiatus" in the literature, with its presumed onset spann
59 seasonal and regional characteristics of the hiatus, including the intensified Walker circulation, th
60                                 Depositional hiatuses indicate erosion by bottom currents related to
61 tending to the diaphragm near the esophageal hiatus; inferiorly, extending to the pelvis along the an
62            Our results show that the current hiatus is part of natural climate variability, tied spec
63          To examine whether the notion of a "hiatus" is justified by the available data, we first doc
64                The resulting surface warming hiatus lasts for 40-50 years.
65 Moreover, the recent global surface warming "hiatus" may be attributed to the SPNA as one of the majo
66           We assessed the LES and esophageal hiatus morphology using a block containing the human LES
67 osits after a approximately 900-million year hiatus, occur shortly before the approximately 2.3-2.2 G
68 ross over" to review the other group after a hiatus of at least 8 weeks.
69 lantic and Southern Oceans during the recent hiatus of global warming.
70                                      After a hiatus of more than 20 years, three new medications appr
71                                            A hiatus of several decades followed, during which the imp
72 ur results suggest a possible recent warming hiatus on the northwestern TP.
73 fundoplication was undertaken for a patulous hiatus or large hiatal hernia or to buttress the repair
74                In late 2011, after a 12-year hiatus, oral vaccines against adenovirus types 4 (Ad4) a
75                               After a 4-week hiatus, patients with a response could receive interleuk
76 ibetan Plateau (TP), even during the warming hiatus period.
77 , which reached levels of 400 ppm during the hiatus period.
78 ne occurred during the recent global warming hiatus period.
79 ) were included in the calculation, alleged "hiatus" periods notwithstanding.
80 he warming effect of the adjusted SAT in the hiatus process.
81 frequency was highly correlated with the SCJ-hiatus separation (r = 0.76; P < 0.001).
82         Eight GERD patients with >/=1-cm SCJ-hiatus separation were considered hernia patients, and 7
83 butes about 10% to the recent global warming hiatus since 1999.
84 tional to the separation between the SCJ and hiatus, suggesting that the perturbed anatomy associated
85                 The analysis shows that the "hiatus" trends are encompassed within the overall distri
86                                          The hiatus was a Pacific-wide phenomenon with an underlying
87 troesophageal junction and the diaphragmatic hiatus were 0.88 and 0.85, respectively.
88 y years of stripe rust research, the 20-year hiatus when stripe rust was not considered important and
89 dual migrations were punctuated by a 7-month hiatus, when crabs remained stationary, coincident with
90 ic relationships, such as facies changes and hiatuses, within the deposit.

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