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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.
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
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
28 shows an anomalous warming below 50 m during hiatus events due to an enhanced heat transport by the I
30 ew clumped isotope temperature record from a hiatus-free, expanded KPg boundary section from Seymour
33 non that has been dubbed the global warming "hiatus." Here, we present an updated global surface temp
35 ormal subjects (NL), 9 GERD patients without hiatus hernia (NHH), and 7 with hiatus hernia (HH) were
41 ed with reflux of stomach acid and usually a hiatus hernia, and it strongly predisposes to esophageal
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
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
52 and others have interpreted this widespread hiatus in sedimentation on the continents as a failure o
56 state behaviour can be explained by episodic hiatuses in river incision triggered by alluvial deposit
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
61 tending to the diaphragm near the esophageal hiatus; inferiorly, extending to the pelvis along the an
65 Moreover, the recent global surface warming "hiatus" may be attributed to the SPNA as one of the majo
67 osits after a approximately 900-million year hiatus, occur shortly before the approximately 2.3-2.2 G
73 fundoplication was undertaken for a patulous hiatus or large hiatal hernia or to buttress the repair
84 tional to the separation between the SCJ and hiatus, suggesting that the perturbed anatomy associated
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
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