ライフサイエンスコーパス: iceberg

1 ne, with seizures being just the 'tip of the iceberg'.

2 uropa, in which we find evidence for mobile 'icebergs'.

3 wn thus far may only represent the tip of an iceberg.

4 istance at both QTLs originate from cultivar Iceberg.

5 at we have now merely reached the tip of the iceberg.

6 intersections represent only the tip of the iceberg.

7 the available data show only the tip of the iceberg.

8 t these likely represent only the tip of the iceberg.

9 tory responses analogous to the CARD protein ICEBERG.

10 enes it contained proved to be the tip of an iceberg.

11 el regions we detect are just the tip of the iceberg.

12 ese described species is just the tip of the iceberg.

13 ented scale, yet this is just the tip of the iceberg.

14 atory compounds, we know just the tip of the iceberg.

15 ular domain is merely the tip of a molecular iceberg.

16 , this is just the tip of the research waste iceberg.

17 these efforts represent only the tip of the iceberg.

18 he freshwater flux that results from melting icebergs.

19 ion, similar to that identified in Antarctic icebergs.

20 red only by perennial sea ice with scattered icebergs.

21 l iron inputs are thought to be dominated by icebergs.

22 glacial halocline related to melt water from icebergs.

23 ert with the flux of freshwater from melting icebergs.

24 -1)) associated with suspended sediment than icebergs (0-241 kg km(-2) a(-1)).

25 (<0.45 mum) iron (6-81 kg km(-2) a(-1)) than icebergs (0.0-1.2 kg km(-2) a(-1)).

26 Two free-drifting icebergs, 0.1 and 30.8 square kilometers in aerial surfa

27 that link glacier calving-the detachment of icebergs(6)-and submarine melt to the broader fjord dyna

28 lf, Antarctica led to the calving of tabular iceberg A68 in July 2017, one of the largest icebergs on

29 In December 2020, giant tabular iceberg A68a (surface area 3900 km(2)) broke up in open

30 Data on whether icebergs affect bacterioplankton function and compositio

31 Iceberg-rafted debris data from Iceberg Alley identify eight retreat phases after the La

32 ving likely will not persist long enough for icebergs alone to cause catastrophic disruption to the A

33 Cultivars Iceberg and Grand Rapids that were released in the 18th

34 CARD-8 binds also to ICEBERG and pseudo-ICE, two other recently identified pr

35 and water viscosity, winter calm and summer (iceberg and storm) disturbance and resources.

36 terize the meltwater field around individual icebergs and integrate the results with regional- and gl

37 tunities to explore the interactions between icebergs and other components of the climate system and

38 uses, and nematodes represent the tip of the iceberg, and few details of their host-parasite relation

39 Pro-glacial melange (a mixture of sea ice, icebergs, and snow) may be tightly packed in the long, n

40 ially contributed to the melting of sea ice, icebergs, and terminal ice-sheet margins.

41 e newer treatments represent the "tip of the iceberg," and as our basic knowledge increases, so too w

42 Icebergs are a vector transporting the bioessential micr

43 Our results demonstrate that, whilst icebergs are the largest source of iron to the polar oce

44 c solute, water forms transient microscopic "icebergs" arising from strengthened water hydrogen bondi

45 tides played a catalytic role in liberating iceberg armadas during that time.

46 our glacial cycles, implying that in general icebergs arrived too late to have triggered cooling.

47 Using the iceberg as a metaphor, we argue that the effects of anti

48 acterized by small numbers of large, tabular icebergs as is observed today, which would produce wide,

49 therapeutic scenario is only the tip of the iceberg, as hundreds of new compounds and combinations a

50 The arrival and grounding of Iceberg B9B in Commonwealth Bay in March 2011 led to the

51 this site in the past after the grounding of Iceberg B9B.

52 The data presented may be the tip of the iceberg because we have only reported the children who r

53 change and may enhance the drift of melting icebergs, besides unraveling a primal strategy by which

54 een North Atlantic cold events and increased iceberg calving and dispersal from ice sheets surroundin

55 ergs, has been accompanied by an increase in iceberg calving and ice mass loss.

56 Understanding how regime shifts in iceberg calving behavior affect ice shelf stability rema

57 Here we show that iceberg calving can act as a submarine melt amplifier th

58 s of iceberg-keel plough marks, we find that iceberg calving during the most recent deglaciation was

59 e sheets are driven by submarine melting and iceberg calving from tidewater glacier margins.

60 Iceberg calving has been assumed to be the dominant caus

61 diverse set of ice shelves demonstrates that iceberg calving increases with the along-flow spreading

62 Iceberg calving is a major contributor to Greenland's ic

63 shelves like Petermann's is unlikely, unless iceberg calving is greatly reduced.

64 recedes from marine-terminating outlets, its iceberg calving likely will not persist long enough for

65 ront-proximal submarine fibre sensing of the iceberg calving process chain.

66 Tabular iceberg calving reduces ice-shelf extent, affecting ocea

67 shelves, mass losses due to basal melting or iceberg calving were significantly positively correlated

68 half of Greenland's mass loss occurs through iceberg calving, but the physical mechanisms operating d

69 onent of ice sheet and shelf mass balance is iceberg calving, which can generate large tsunamis endan

70 ospheric cooling reduces surface melting and iceberg calving.

71 hical perturbations introduced by a drifting iceberg can affect activity, composition, and substrate

72 the characteristic size-frequency scaling of icebergs can be explained by the emergence of a dominant

73 Although the size-frequency distributions of icebergs can provide insight into how they disintegrate,

74 These results suggest that free-drifting icebergs can substantially affect the pelagic ecosystem

75 results from the horizontal force caused by iceberg capsize and acceleration away from the glacier f

76 nge of ocean tide height, wind speed, and an iceberg collision in August 2021, as well as the long-te

77 derived from a cross between the susceptible iceberg cv. 'Salinas' and the resistant oil-seed accessi

78 ce of a dominant set of driving processes of iceberg degradation towards the open ocean.

79 silica in Greenland Ice Sheet meltwaters and icebergs, demonstrating the potential for high ice sheet

80 ersistent ice fracturing that coalesces into iceberg detachment, which in turn excites local tsunamis

81 e past five glaciation cycles, indicators of iceberg discharge and sea-surface temperature display dr

82 here storm tracks and the associated delayed iceberg discharge events as documented during other HS.

83 , the Laurentide Ice Sheet exhibited extreme iceberg discharge events that are recorded in North Atla

84 Atlantic region that culminated in extensive iceberg discharge events.

85 ntic region, beginning with the catastrophic iceberg discharge Heinrich event H1, 17,500 yr ago, and

86 lacial cycle, leading to the hypothesis that iceberg discharge may be a consequence of stadial condit

87 The model generates a time series of iceberg discharge that closely agrees with ice-rafted de

88 Ice Sheet (LIS) underwent episodes of rapid iceberg discharge, recorded in ocean sediments as "Heinr

89 riggering rapid margin retreat and increased iceberg discharge.

90 Episodic iceberg-discharge events from the Hudson Strait Ice Stre

91 ly 4 degrees to 6 degreesC, and catastrophic iceberg discharges begin alternating repeatedly with bri

92 e last glacial period interpreted as massive iceberg discharges from the Laurentide Ice Sheet.

93 Massive iceberg discharges from the Northern Hemisphere ice shee

94 tennial-scale excursions during catastrophic iceberg discharges of the Heinrich stadials.

95 The mechanisms linking North Atlantic iceberg discharges with subantarctic productivity remain

96 est reductions during episodic Hudson Strait iceberg discharges, while sharp northern warming followe

97 zes observed is a product of fracture-driven iceberg disintegration and dimensional reductions throug

98 seismic monitoring to examine mechanisms of iceberg disintegration as a function of drift.

99 ize-frequency distribution required to model iceberg distributions accurately must vary according to

100 nsion feeders, with an intermediate level of iceberg disturbance.

101 We assessed the influence of iceberg drift on bacterial community composition and on

102 The release of freshwater from icebergs drives an overturning circulation, resulting in

103 e of the generator potential (the so-called "iceberg effect"), but not to maximize the transmission o

104 Unlike the iceberg effect, contrast invariance remains intact even

105 et, such fast errors are only the tip of the iceberg: electromyography (EMG) revealed fast subthresho

106 A theoretical model for released iceberg energy supports this finding and the measured wa

107 Meltwater and icebergs entering the North Atlantic alter oceanic and a

108 During Heinrich events, great armadas of icebergs episodically flooded the North Atlantic Ocean a

109 Gravity-dominated icebergs essentially fall into the water body whereas bu

110 ansient currents at the ice front before the icebergs eventually decay into fragments.

111 ophyll, krill, and seabirds surrounding each iceberg, extending out to a radial distance of approxima

112 We document eight events of increased iceberg flux from various parts of the AIS between 20,00

113 Therefore, increasing iceberg fluxes due to global warming have the potential

114 re be not only sensitive to increasing total iceberg fluxes, but also to changing iceberg properties,

115 nstrated that miRNAs are just the tip of the iceberg for sRNAs.

116 Our findings represent only the tip of the iceberg for substantial health externalities of high-inp

117 phases likely represent only the "tip of the iceberg" for this family.

118 The proliferation of icebergs from Antarctica over the past decade has raised

119 r 'icehouse' world influenced by sea ice and icebergs from the middle Eocene epoch to the present.

120 evidence favors the latter scenario because iceberg furrows that cross cut the ridges in deep water

121 lange, a floating aggregation of sea ice and icebergs, has been accompanied by an increase in iceberg

122 Ice melange, tightly packed sea ice and icebergs, has been hypothesized to buttress the calving

123 esults highlight the substantial impact that icebergs have on the dynamics of a major Greenlandic fjo

124 high-metabolic quality (top 5: apples/pears, iceberg/head lettuce, raw spinach, alfalfa sprouts, and

125 deposits of lysozyme are only the tip of an iceberg hiding a crowd of insoluble aggregates.

126 hed examples likely represent the tip of the iceberg in terms of the total extent of ancient hybridiz

127 bal warming, increased frequency of drifting icebergs in polar regions holds the potential to affect

128 vidence for enhanced hydrogen bonding and/or icebergs in such solutions.

129 Extrapolating these results to all icebergs in the same size range, with the use of iceberg

130 s suggests that they were carved by grounded icebergs influenced by tidal and geostrophic ocean curre

131 to utilize specific carbon substrates in the iceberg-influenced waters compared with the undisturbed

132 erent community composition were observed in iceberg-influenced waters relative to the undisturbed wa

133 s associated with Heinrich events: Extensive iceberg influxes into the North Atlantic Ocean linked to

134 with this, enforced retroviral expression of ICEBERG inhibits lipopolysaccharide-induced IL-1beta gen

135 Calving icebergs interact with the surrounding water through dif

136 analysis of iceberg samples, we reveal that iceberg iron concentrations vary over 6 orders of magnit

137 However, the magnitude of the iceberg iron flux, the subsequent fertilization effect a

138 ICEBERG is a novel protein that inhibits generation of I

139 ICEBERG is induced by proinflammatory stimuli, suggestin

140 e present-day Greenland Ice Sheet calving of icebergs is comparable to that of a mid-range Heinrich e

141 Iceberg-keel plough marks on the sea-floor provide geolo

142 rm shape and cross-sectional morphologies of iceberg-keel plough marks, we find that iceberg calving

143 DO cooling events during massive releases of icebergs known as Heinrich (H) events, contrary to ice-c

144 on potential of suspended sediment-plume and iceberg-laden particulate matter from two adjacent, yet

145 ed in continuous wash experiments of chopped iceberg lettuce, and predicted the FC (R(2) = 0.96) and

146 ed in continuous wash experiments of chopped iceberg lettuce, and predicted the FC (R(2) = 0.96) and

147 Using single wash of iceberg lettuce, green cabbage, and carrots, we report t

148 Using single wash of iceberg lettuce, green cabbage, and carrots, we report t

149 Although the freshwater derived from melting icebergs may provide a positive feedback for enhancing a

150 and quantify all OHCs, the size of the OHC "iceberg" may be underestimated.

151 nhibited by viscous flow and back force from iceberg melange.

152 e showing that northward shifts in Antarctic iceberg melt in the Indian-Atlantic Southern Ocean (0-50

153 In addition, we find that submarine iceberg melting accounts for over 95% of heat used for i

154 harge - sourced primarily from ice shelf and iceberg melting along the eastern Antarctic Peninsula -

155 Here we find that submarine iceberg melting cools and freshens the fjord by up to ~5

156 modify an ocean model to simulate submarine iceberg melting in Sermilik Fjord, east Greenland.

157 Submarine iceberg melting releases large volumes of freshwater wit

158 he sensitivity of overturning circulation to iceberg melting.

159 These drifting icebergs mix the water column, influence stratification

160 We described these incidences in terms of an iceberg model of self-harm.

161 In contrast to the classical "iceberg" model of hydrophobic hydration, the favorable e

162 vide a physical picture of the long-debated "iceberg" model; we show that the slow, long-time compone

163 We propose an 'iceberg' model, by which increased neuronal excitability

164 vide geological evidence of past and present iceberg morphology, keel depth and drift direction.

165 the complex interactions between ice-sheets, icebergs, ocean and the atmosphere.

166 er the two families represent the tip of the iceberg of a subset of COVID-19 male patients.

167 he well-known Inca Empire was the tip of the iceberg of an evolutionary process that started 11,000 t

168 inly used information from the Exploring the Iceberg of Celiacs in Sweden (ETICS) study, a school-bas

169 proteins are likely to be just the tip of an iceberg of multifunctional proteins that stabilize and c

170 ntified to date represent just the tip of an iceberg of risk variants likely to include hundreds of m

171 re breathtaking, they are only the tip of an iceberg of technologies that have yet to be utilized in

172 orphological changes are only the tip of the iceberg of the entire protective mechanisms.

173 ocal reports may only reflect the tip of the iceberg of underlying effects.

174 iceberg A68 in July 2017, one of the largest icebergs on record, posing a threat for the stability of

175 rdinary evidence that massive (>300 m thick) icebergs once drifted >5,000 km south along the eastern

176 ver, is this just the tip of a 'conservation iceberg' or do these sequences represent a specific clas

177 The CZS could be just "the tip of the iceberg", pending the documentation of a spectrum of dis

178 ergs in the same size range, with the use of iceberg population estimates from satellite surveys, ind

179 undamentally, there is a discrepancy between iceberg power-law size-frequency distributions observed

180 The number of icebergs produced from ice-shelf disintegration has incr

181 of icebergs smaller than the typical tabular icebergs produced today.

182 ure, when glaciers reach grounding lines and iceberg production diminishes, is as a major global sink

183 g total iceberg fluxes, but also to changing iceberg properties, internal sediment distribution and m

184 However, a Southern Ocean (Atlantic-sector) iceberg rafted debris event appears to have occurred syn

185 Marine records of iceberg-rafted debris (IBRD) provide a nearly continuous

186 Iceberg-rafted debris data from Iceberg Alley identify e

187 analysed high-temporal-resolution records of iceberg-rafted debris derived from the Antarctic Ice She

188 alignment of key climate data sets spanning iceberg-rafted debris event Heinrich 3 and Greenland Int

189 , corresponding to the period of the highest iceberg-rafted debris flux and the occurrence of the mel

190 The structure of ICEBERG reveals it to be a member of the death-domain-fo

191 to the water body whereas buoyancy-dominated icebergs rise to the water surface.

192 Using a global analysis of iceberg samples, we reveal that iceberg iron concentrati

193 correlated positively with the frequency of iceberg scour at the different sites with the highest re

194 helves are typically deeper than most modern iceberg scouring, bacterial breakdown rates are slow, an

195 Reduced fast ice after 2006 ramped iceberg scouring, killing half the encrusting benthos ea

196 rgest disturbance gradients on earth, due to iceberg scouring.

197 h along the eastern United States, with >700 iceberg scours now identified south of Cape Hatteras.

198 ed on an exquisitely preserved set of buried iceberg scours seen in three-dimensional seismic reflect

199 rced ice losses are increasing potential for iceberg-seabed collisions, termed ice scour.

200 Numerical glacial iceberg simulations indicate that the transport of icebe

201 shift in the size-frequency distribution of iceberg sizes observed is a product of fracture-driven i

202 0 years ago, which produced large numbers of icebergs smaller than the typical tabular icebergs produ

203 ent only the clearance-resistant "tip of the iceberg." Such aberrantly circulating mucins could play

204 d in the Sahel region at the time of massive iceberg surges, leading to large freshwater discharges.

205 ed by the temporary grounding of two immense icebergs that (i) erected a veritable fence separating c

206 heet sporadically discharged huge numbers of icebergs through the Hudson Strait into the North Atlant

207 ationship between the meltwater field of the iceberg to the larger-scale marine ecosystem of the Sout

208 harge-charge interactions mediate binding of ICEBERG to the prodomain of caspase-1.

209 Transport of icebergs to the subtropics, away from deep water formati

210 g simulations indicate that the transport of icebergs to these sites occurs during massive, but short

211 ies are likely to be the tip of an "invasion iceberg" to the NW Atlantic from Great Britain and Irela

212 nt less than previous estimates derived from iceberg tracking.

213 riments, we demonstrate that such a shift in iceberg trajectories during glacial periods can result i

214 With the aid of iceberg-trajectory model experiments, we demonstrate tha

215 ique large-scale laboratory experiments that iceberg-tsunami heights from gravity-dominated mechanism

216 stimates of an upper envelope of the maximum iceberg-tsunami heights, they fail to capture the physic

217 ts, they fail to capture the physics of most iceberg-tsunami mechanisms.

218 Such iceberg-tsunamis have reached amplitudes of 50 m and des

219 en neglected genetic disease source, a true "iceberg under water."

220 ive (5-10 s km wide, 50-180 m thick) tabular icebergs until widespread ice shelf break-up shifted the

221 tifying the unidentified fraction of the OHC iceberg using targeted analyses of major OHCs together w

222 owever, this research is only the tip of the iceberg when it comes to writing an 'epigenetic instruct

223 y verified TMD, although that was a "symptom iceberg" when compared with the 19% annual rate of facia

224 ndeed likely to represent only the tip of an iceberg with hundreds or more of additional micro-RNAs (

225 fection may therefore reflect the tip of the iceberg with regard to the burden of colonization of a s

226 Giant icebergs with lengths exceeding 18.5 km account for most

227 as characterized by large numbers of smaller icebergs with V-shaped keels.

228 n tissue samples reveal only the "tip of the iceberg", with most of the important changes occurring o

229 antibiotics on AMR represent the tip of the iceberg, with much greater repercussions stemming from t

230 We also introduce methods to represent giant icebergs within climate models that currently do not hav