ライフサイエンスコーパス: grounding

1 entity recognition (NER) and normalization (grounding).

2 der to keep airspace open and avoid aircraft groundings.

3 rences in their theoretical and experimental groundings.

4 ntly, electrostatic damage can be avoided by grounding a Pt electrode and nearby objects, most import

5 Term identification is the task of grounding ambiguous mentions of biomedical named entitie

6 f a century ago moved archaeology forward by grounding archaeological remains in time, LiDAR is provi

7 Grounding autonomous behavior in the nervous system is a

8 hat the results here may act as an excellent grounding for better understanding (1)pisigma* driven dy

9 cation in mathematics and physics was a good grounding for graduate studies in crystallographic studi

10 Here we provide theoretical grounding for this relationship.

11 f New York (CCNY) made a solid and priceless grounding in chemistry and biology available free of cha

12 gion has steadily expanded from its original grounding in epidemic disease to describe a vast array o

13 hese findings provide, for the first time, a grounding in pathology for gold standard behavior-based

14 es in well informed decision-making requires grounding in perspectives of comparison.

15 cal assessment of disorders now have a solid grounding in systems neuroscience.

16 ctroosmotic (EO) flow pump, a polyacrylamide grounding interface, and a nanoliter-to-picoliter pipet

17 features-consistent with parts-based models-grounding investigation of how the presence of a face is

18 Lake et al. point out that grounding learning in general principles of embodied per

19 continental ice from Antarctica reaches the grounding line and begins to float, its underside melts

20 the ocean has been demonstrated close to the grounding line and near the calving front.

21 nding-line history, but the locations of the grounding line before the advent of satellite monitoring

22 s ribs, potentially causing migration of the grounding line by changes in basal resistance in its vic

23 ice-shelf channels is seeded upstream of the grounding line by large basal obstacles indenting the ic

24 hat penetrate up to 1000 kilometers from the grounding line into the interior of the ice sheet.

25 The ice thickness at the grounding line is greater than that of floating ice in h

26 Sea-level fall near the grounding line of a retreating marine ice sheet has a st

27 previously unknown subglacial lake near the grounding line of Whillans Ice Stream is observed to dra

28 gued to reflect marine downdraw triggered by grounding line retreat into Hercules Inlet.

29 e shelf, and constrain the date at which the grounding line retreated from a prominent seafloor ridge

30 ity (MISI), a self-sustaining retreat of the grounding line triggered by oceanic or atmospheric chang

31 late that the eskers' size grows towards the grounding line where deposition rates are maximum.

32 Thus, the grounding line will tend to remain in the same location

33 Many of them originate near the grounding line, but their formation mechanisms remain po

34 hat unstable and irreversible retreat of the grounding line-which marks the boundary between grounded

35 bglacial Basin, 350-550 kilometres from this grounding line.

36 doubled, and calving is now occurring at its grounding line.

37 ip terminates at the ice stream edge and the grounding line.

38 en the ice and stabilize the position of the grounding line.

39 en Glacier, within 150 kilometres of today's grounding line; and deep within the Sabrina Subglacial B

40 Our observation is that grounding-line deposition serves to thicken the ice and

41 h-resolution nesting with a new treatment of grounding-line dynamics and ice-shelf buttressing to sim

42 g satellite measurements of calving flux and grounding-line flux, modelled ice-shelf snow accumulatio

43 ent retreat requires a detailed knowledge of grounding-line history, but the locations of the groundi

44 Southward grounding-line migration was dated past three locations

45 volume of the GZW cluster suggests that the grounding-line position of the paleo-Bindschadler Ice St

46 eventually retreated 1000 km to the current grounding-line position on the inner shelf.

47 th sufficient spatial resolution to simulate grounding-line processes have been too computationally e

48 which acceleration can initiate or modulate grounding-line retreat and ice loss.

49 helves helps to stabilize ice sheets against grounding-line retreat in response to a rise in relative

50 bglacial water could trigger or facilitate a grounding-line retreat in Thwaites Glacier capable of sp

51 In particular, a history of grounding-line retreat is required to understand the rel

52 bsequent punctuated large-distance ( 200 km) grounding-line retreat may have been a highly non-linear

53 Current grounding-line retreat may reflect ongoing ice recession

54 -Ronne and Ross ice shelves, which initiates grounding-line retreat there.

55 We report on the discovery of a grounding-line sedimentary wedge ("till delta") deposite

56 distributed subglacial till deformation, and grounding-line sedimentation, which have important impli

57 the Last Glacial Maximum is best known, with grounding lines advancing to the continental-shelf edges

58 The region's future, when glaciers reach grounding lines and iceberg production diminishes, is as

59 erienced by large outlet glaciers near their grounding lines are far higher than generally assumed.

60 Grounding lines are several hundred metres below sea lev

61 rctic Ice Sheet if ice shelves that buttress grounding lines more than 800 metres below sea level are

62 iations range from full glacial extents with grounding lines near the continental shelf break, interm

63 Where deep water has direct access to grounding lines, glaciers and ice shelves are vulnerable

64 Greenland, has intensified on key Antarctic grounding lines, has endured for decades after ice-shelf

65 d strong ocean thermal forcing on their deep grounding lines.

66 portunity arose as a result of the three-day grounding of all commercial aircraft in the United State

67 s additional deliberations on the functional grounding of Hulleman & Olivers' (H&O's) functional view

68 The arrival and grounding of Iceberg B9B in Commonwealth Bay in March 20

69 occurred at this site in the past after the grounding of Iceberg B9B.

70 We demonstrate that the straightforward grounding of the transfer line removes the influence of

71 experiment was facilitated by the temporary grounding of two immense icebergs that (i) erected a ver

72 Here we present new evidence of ice-shelf groundings on bathymetric highs in the central Arctic Oc

73 After grounding our argument in a discussion of stochastic noi

74 le accounting for imperfect observations and grounding our findings in species-level range dynamics.

75 ncluded (1) a second-degree skin burn at the grounding pad site, (2) transient bowel and bladder inco

76 s including impedance, voltage, current, and grounding pad temperature.

77 lectrodes in the system, one as the upstream grounding point and the other as the emitter electrode,

78 l bore-through union serving as the upstream grounding point in a floated electrospray emitter system

79 and auxiliary electrodes, and current at the grounding points upstream and downstream of the emitter

80 demonstrates how therapeutic change occurs, grounding psychotherapy in brain science.

81 in the DN and thus directly support theories grounding selfhood in the neural monitoring of visceral

82 ogical studies, we may develop a theoretical grounding that allows us to improve the application of i

83 Here, we argue for the advantages of grounding the psychological dynamics described in the mo

84 The paper therefore proposes grounding the study of decision making under uncertainty

85 All this brings social behavioral grounding to cognitive neuroscience.

86 This long duration grounding was probably facilitated by rapid GZW growth.

87 When the grounding was removed or when broadband electromagnetic

88 a response to surface warming rather than to grounding zone instability, strengthening the idea that

89 ted in 2006 reveal a large, arcuate, complex grounding zone sediment system at the front of Crane Fjo

90 of the fjord suggest that the Crane Glacier grounding zone was well within the fjord before 2002 and

91 deposited a voluminous stack of overlapping grounding zone wedges (GZWs) on the outer shelf of the W

92 Melting in the grounding zones is found to be much higher than steady-s

93 When grounding zones of glaciers retreat onto such slopes, th

94 magnitude is not well known in the critical grounding zones of the ASE's major glaciers.

95 The present-day grounding zones of the Pine Island and Thwaites glaciers

96 Grounding zones, where ice sheets transition between res