ライフサイエンスコーパス: meridional

1 elate configuration with the other six being meridional.

2 ial tension and the associated change in the meridional 14.5 nm reflection intensity, which are both

3 ing of the diffuse equatorial scattering and meridional accentuation of the (210) reflection at 3.8 A

4 e classified into three types based on their meridional aerosol distributions: NH volcanoes, SH volca

5 Meridional analysis of the refractive data indicated tha

6 These meridional and zonal patterns are best explained by a po

7 rly Pliocene climate had substantially lower meridional and zonal temperature gradients but similar m

8 tterns of the Pliocene, specifically reduced meridional and zonal temperature gradients.

9 of a cobalt(I)-N2 complex (2) supported by a meridional bis-phosphino-boryl (PBP) ligand.

10 annot account for the observed low-angle off-meridional Bragg peak intensity distribution.

11 reversible change in the intensities of the meridional Bragg peaks indicated that supramolecular rea

12 The meridional changes signal movement of at least 30% of al

13 appear in regions of convergence by the mean meridional circulation and over the poles during solstic

14 A meridional circulation with a poleward flow of about 20

15 ich positive PNA periods are associated with meridional circulation, leading to the dominance of sout

16 e regional manifestation of the atmosphere's meridional circulation.

17 re probed by alpha - Omega dynamo model with meridional circulation.

18 al features of these complexes; that is, the meridional configuration places strongly trans influenci

19 Data also suggest possible meridional contraction at the juncture between the apica

20 ean enhance Sahel rainfall through increased meridional convergence of low-level, externally sourced

21 ligands, their oxidation resistance, and the meridional coordination geometry.

22 xistence and area fractions, distribution of meridional curvature, and fluorescent-probe intensity di

23 A narrower distribution of meridional curvatures in GUVs with trans DOPC is suggest

24 At all ages, the retina showed meridional difference in cone densities, with cone photo

25 Meridional diffraction patterns obtained from the orient

26 l and cataractous oriented membranes yielded meridional diffraction peaks corresponding to a unit cel

27 drated bovine zonular filaments demonstrated meridional diffraction peaks indexing on a fundamental a

28 on micrographs is on the order of 9 A in the meridional direction and 12 A in the equatorial.

29 on data extending to 2.4 A resolution in the meridional direction and to 3.1 A resolution in the equa

30 tern of second cleavage divisions in which a meridional division is followed by one that is equatoria

31 from four-cell stage blastomeres from early meridional divisions develop normally.

32 fractive error with age were consistent with meridional emmetropization in children with INS and WTR

33 en with INS and whether there is evidence of meridional emmetropization.

34 subjects also can be explained in terms of "meridional emmetropization." The contrasting refractive

35 ferential wall expansion exceeds the rate of meridional expansion.

36 As active tension rose, the 14.5- and 7.2-nm meridionals fell, the first row line dropped at the 38.7

37 The percentage occurrence of meridional fibers decreased significantly from the inner

38 nerve head deformations, whereas equatorial meridional fibers may either provide resistance against

39 ificantly higher percentage of occurrence of meridional fibers than did the Caucasians (P < 0.001).

40 lasma would be deflected from radial flow to meridional flow (in solar heliospheric coordinates), whi

41 The structure and strength of the meridional flow determine both the strength of the Sun's

42 The Sun's meridional flow is an axisymmetric flow that is generall

43 We determine the meridional flow speed of magnetic features on the Sun us

44 o expectations, these observations yielded a meridional flow velocity of +3 +/- 11 km s(-1), that is,

45 on board Voyager 1 so that it could measure meridional flow.

46 oid degeneration (TCD), cystic retinal tuft, meridional fold, lattice and cobblestone degeneration, r

47 ora serrata pearl, TCD, cystic retinal tuft, meridional fold, lattice, and cobblestone degenerations.

48 pearl, ora tooth, TCD, cystic retinal tuft, meridional fold, retinal hole, and typical degenerative

49 g pathologies, such as lattice degeneration, meridional folds, retinal breaks, and rhegmatogenous ret

50 es has increased the subpolar to subtropical meridional gradient in SSTs, which are not represented b

51 The primary causal agent is the meridional gradient in the ionospheric Hall conductance

52 The meridional gradient is projected to strengthen throughou

53 anced in colder climates owing to a stronger meridional gradient of sea surface temperatures, with im

54 root hairs, wall expansion exhibits a strong meridional gradient with a maximum near the pole of the

55 lution produces a 9% enhanced transient eddy meridional heat flux and reconciles a decadal variation

56 er the past 22,000 years; however, the total meridional heat transport (MHT) of the climate system re

57 l circulation due to its fundamental role in meridional heat transport and forcing of stationary wave

58 The estimated meridional heat transport by eddy movement is similar in

59 Variations in oceanic meridional heat transport may contribute to these repeat

60 C), which provides one-quarter of the global meridional heat transport, is composed of a number of se

61 Through its attendant meridional heat transport, the AMOC helps maintain a war

62 ally paced ocean circulation changes altered meridional heat/vapor transport, triggering ice growth a

63 The patterns contain meridional intensities at 1/3.4 A(-1) and 1/6.5 A(-1), a

64 In addition, meridional intensities have been seen from C-protein (My

65 ous prions that show cross-beta diffraction: meridional intensity at 4.8 A resolution, indicating the

66 at 1/3.4 A(-1) and 1/6.5 A(-1), a strong off-meridional intensity at Z=1/5.6 A(-1) and diffuse scatte

67 Meridional intensity profiles of the peaks at the first

68 The meridional isomer of Ir(tpy)(3) and facial and meridiona

69 at 140-150 degrees C forms the corresponding meridional isomer, while higher reaction temperatures gi

70 The meridional isomers are easier to oxidize by ca. 50-100 m

71 nverted to facial forms, indicating that the meridional isomers are kinetically favored products.

72 The lower thermodynamic stabilities of the meridional isomers are likely related to structural feat

73 Both facial and meridional isomers can be obtained in good yield (>70%).

74 The meridional isomers for both pyridyl and pyrazolyl-based

75 The three meridional isomers have the expected bond length alterna

76 trans influence of the phenyl groups in the meridional isomers leads to the observation that they ar

77 The preparation of the facial and meridional isomers of [Ir(pyalk)3] (pyalk = 2-(2-pyridyl

78 We describe facial and meridional isomers of [Rh(III)(pyalk)3], as well as meri

79 ridional isomer of Ir(tpy)(3) and facial and meridional isomers of Ir(ppz)(3) and Ir(tfmppz)(3) have

80 We find that both the facial and the meridional isomers of the dopant have high efficiencies

81 The intensities of the off-meridional layer lines and fine interference structure o

82 -band, which must be occurring, the observed meridional M3 and M6 X-ray intensity changes can all be

83 lines and fine interference structure of the meridional M3 myosin x-ray reflection were resolved.

84 w clouds, and a rise of the level of maximum meridional mass outflow in the upper troposphere (200-10

85 the reduction of sea ice shows much broader meridional meanders in midlatitudes and clearly differen

86 Meridional (mer) coordination promotes the generation of

87 photophysics of a series of facial (fac) and meridional (mer) tris-cyclometalated Ir(III) complexes a

88 ollowing the pattern of the Southern Pacific Meridional Mode.

89 The meridional moisture stress gradient reconstructed from t

90 e European Alps are an effective barrier for meridional moisture transport and are thus uniquely plac

91 This pronounced meridional moisture transport, which contrasts with the

92 The meridional net flux pattern of this substance is expecte

93 and out of southern high latitudes point to meridional (north-south) mixing throughout southern wint

94 that extensive winter sea ice and curtailed meridional ocean overturning in the North Atlantic led t

95 th Atlantic Oscillation (NAO), a hemispheric meridional oscillation in atmospheric mass with centers

96 synchronization, with a maximum in Atlantic Meridional Overturning Circulation (AMOC) 15 years after

97 e accompanied by both reductions in Atlantic Meridional Overturning Circulation (AMOC) and collapses

98 associated with disruptions of the Atlantic Meridional Overturning Circulation (AMOC) during the deg

99 meltwater-induced reduction in the Atlantic meridional overturning circulation (AMOC) during the ear

100 The Atlantic Meridional Overturning Circulation (AMOC) exhibits two s

101 Abrupt changes in the Atlantic meridional overturning circulation (AMOC) have often bee

102 The importance of the Atlantic Meridional Overturning Circulation (AMOC) heat transport

103 The quantitative role of the Atlantic Meridional Overturning Circulation (AMOC) in dissolved o

104 lso leads to a strengthening of the Atlantic Meridional Overturning Circulation (AMOC) in the first 2

105 ination of a large reduction in the Atlantic meridional overturning circulation (AMOC) indicates a cl

106 associated with a weakening of the Atlantic Meridional Overturning Circulation (AMOC) inferred from

107 The Atlantic Meridional Overturning Circulation (AMOC) is an importan

108 A collapse of the Atlantic Meridional Overturning Circulation (AMOC) leads to globa

109 ) concentration, ice sheets and the Atlantic meridional overturning circulation (AMOC) on hemispheric

110 The Atlantic meridional overturning circulation (AMOC) transports war

111 ial variability associated with the Atlantic Meridional Overturning Circulation (AMOC) undergoes a mo

112 ean-atmosphere models indicate that Atlantic meridional overturning circulation (AMOC) variability is

113 s indicate the strengthening of the Atlantic Meridional Overturning Circulation (AMOC) with a signatu

114 (OHC) is highly correlated with the Atlantic Meridional Overturning Circulation (AMOC), and its circu

115 d was reached at 400 ka involving Atlantic Meridional Overturning Circulation (AMOC), inflowing war

116 used a sustained reduction of North Atlantic Meridional Overturning Circulation (AMOC), resulting in

117 This suggests that MOW influenced Atlantic Meridional Overturning Circulation (AMOC), THC, and clim

118 age SST may be driven partly by the Atlantic Meridional Overturning Circulation (AMOC), the atmospher

119 However, the variability of the Atlantic meridional overturning circulation (AMOC), which has a r

120 illful multiyear predictions of the Atlantic Meridional Overturning Circulation (AMOC).

121 ic and weakened the strength of the Atlantic Meridional Overturning Circulation (AMOC).

122 YDS climate was a weakening of the Atlantic Meridional Overturning Circulation (AMOC).

123 Stream path, namely changes in the Atlantic meridional overturning circulation (AMOC).

124 n abrupt (</=400 year) deepening of Atlantic Meridional Overturning Circulation (AMOC).

125 a), is thought to have strengthened Atlantic Meridional Overturning Circulation (AMOC).

126 ocean circulation, specifically the Atlantic Meridional Overturning Circulation (AMOC).

127 The vigor of Atlantic meridional overturning circulation (MOC) is thought to b

128 The Atlantic meridional overturning circulation (MOC), which provides

129 rease is sufficient to have reduced Atlantic meridional overturning circulation and caused the Younge

130 es and the resulting changes in the Atlantic Meridional Overturning Circulation and equatorial annual

131 may have played a crucial role in regulating meridional overturning circulation and global climate ch

132 s associated with variations in the Atlantic meridional overturning circulation and the more gradual

133 ng oceans, at times suppressing the Atlantic meridional overturning circulation and triggering abrupt

134 n Hemisphere and the restart of the Atlantic meridional overturning circulation at the start of the B

135 es ascribe a central role to the wind-driven meridional overturning circulation between the tropical

136 fronts has been linked with reduced Atlantic Meridional Overturning Circulation by restricting surfac

137 The Atlantic meridional overturning circulation carries warm upper wa

138 rs: an observed 30% downturn of the Atlantic meridional overturning circulation during 2009-10, and a

139 Here we show that slowdowns of the Atlantic meridional overturning circulation during Heinrich stadi

140 e review observations implying that Atlantic meridional overturning circulation during the Last Glaci

141 ropical Atlantic, show that surface Atlantic meridional overturning circulation dynamics likely ampli

142 ce of variations in the rate of the Atlantic meridional overturning circulation for abrupt climate ch

143 The comparison suggests that the Atlantic meridional overturning circulation has slowed by about 3

144 ng and merely reflects the depth of the mean meridional overturning circulation in the basin.

145 Projected weakening of the meridional overturning circulation in the North Atlantic

146 The strength of Atlantic meridional overturning circulation is believed to affect

147 The Atlantic meridional overturning circulation is widely believed to

148 he simulations, a disruption of the Atlantic meridional overturning circulation leads to a collapse o

149 -gyre heat transport as part of the Atlantic Meridional Overturning Circulation must be accomplished

150 raced the dominant paradigm that the ocean's meridional overturning circulation operates like a conve

151 ally hypothesized to originate from Atlantic meridional overturning circulation oscillations.

152 l variations in the strength of the Atlantic meridional overturning circulation recorded in marine se

153 f Caribbean hydroclimate in helping Atlantic Meridional Overturning Circulation recovery during D-O e

154 We conclude that the uncertainty in the mean meridional overturning circulation strength at upper lev

155 adal-to-centennial scale changes in Atlantic meridional overturning circulation strength in regulatin

156 re coupled to fluctuations in North Atlantic meridional overturning circulation through its regulatio

157 glacier behaviour was the result of Atlantic meridional overturning circulation variability superimpo

158 e dynamics is the mode and tempo of Atlantic meridional overturning circulation variability, and the

159 m during Heinrich event 1, when the Atlantic meridional overturning circulation was weak, pointing to

160 Reorganizations of the Atlantic meridional overturning circulation were associated with

161 rd indicates that rapid accelerations of the meridional overturning circulation were concurrent with

162 redistribute heat depending on the state of meridional overturning circulation within the Atlantic O

163 pward transport of water closing the ocean's meridional overturning circulation, and thus needs to be

164 ts of 231Pa/230Th, a kinematic proxy for the meridional overturning circulation, in a sediment core f

165 timescales, probably involving the Atlantic meridional overturning circulation, seem to be influenci

166 reshwater forced a reduction in the Atlantic meridional overturning circulation, thereby causing the

167 robust outcome of a slowdown of the tropical meridional overturning circulation, which compensates fo

168 role in closing the deep branch of the ocean meridional overturning circulation.

169 e second mode and variations in the Atlantic meridional overturning circulation.

170 not be ignored when considering the Atlantic meridional overturning circulation.

171 iver with an attendant reduction in Atlantic meridional overturning circulation.

172 to a major downwelling limb of the Atlantic meridional overturning circulation.

173 lds critical to that portion of the Atlantic meridional overturning circulation.

174 vity is sensitive to changes in the Atlantic meridional overturning circulation.

175 Ocean and the near collapse of the Atlantic Meridional Overturning Circulation.

176 d warming and reinvigoration of the Atlantic meridional overturning circulation.

177 e feedbacks triggered by a weakened Atlantic meridional overturning circulation.

178 ffect surface climate - is influenced by the meridional overturning of mass in the stratosphere, the

179 two calculations of the mean strength of the meridional overturning of the stratosphere.

180 500 years) "overshoot" events, with Atlantic meridional overturning stronger than that of the modern

181 We find that the meridional overturning was nearly, or completely, elimin

182 mption results in Earth-like circulations: a meridional overturning with warm water moving poleward a

183 ntic after the abrupt resumption of Atlantic meridional overturning.

184 Compound 3a exhibits meridional phosphines, with both silyl ligands equatoria

185 llation, the North Atlantic Oscillation, the meridional position of the intertropical convergence zon

186 of equatorial warming, because the enhanced meridional pressure gradient forces very strong meridion

187 strong radial expansion anisotropy where the meridional rate of expansion falls below the radial expa

188 ing mainly on the changes in the first order meridional reflection (M3) as compared to isometric.

189 ackbone was determined from the sixth myosin meridional reflection (M6) and the equilibrium positions

190 Electron diffraction gave a prominent meridional reflection at (0.47 nm)(-1), indicative of cr

191 eta fiber pattern, characterized by a strong meridional reflection at 4.74 A and a broad equatorial r

192 the detailed behavior of M3 (the first order meridional reflection from the myosin crossbridges, at 1

193 llary of this force increase by measuring M3 meridional reflection intensity during sinusoidal length

194 We also found that the spacing of the third meridional reflection of the thick filament is linked to

195 In addition to the strong 4.8 A meridional reflection, the recPrP amyloid diffraction is

196 , in the MyBP-C-deficient hearts these extra meridional reflections are weak or absent, suggesting th

197 Significant fixed contributions to the meridional reflections come from unattached myosin heads

198 Additional meridional reflections extend to at least the 12th layer

199 , to study X-ray interference effects in the meridional reflections generated by the arrays of myosin

200 Extra "forbidden" meridional reflections, at orders of 43 nm, in X-ray dif

201 similar measurements on higher order myosin meridional reflections, particularly M6.

202 exhibited up to six orders of MLL and sharp meridional reflections, signifying that myosin heads (cr

203 Changes observed in meridional refractive error with age were consistent wit

204 ipapillary sclera characterized by a stiffer meridional response.

205 nal isomers of [Rh(III)(pyalk)3], as well as meridional [Rh(IV)(pyalk)3](+) {pyalk =2-(2-pyridyl)-2-p

206 rphological and molecular evidence including meridional ribs on the cell wall, pigment production, an

207 al cells also fail to form precisely aligned meridional rows and lens fulcrum.

208 cells undergo cell-to-cell alignment to form meridional rows of hexagonal cells.

209 type hexagonal epithelial cells in organized meridional rows.

210 thelial cells fail to form precisely aligned meridional rows; moreover, the lens fulcrum, where the a

211 itivity) but also accurately quantifying how meridional sea-surface temperature patterns will change

212 km(-1), two orders of magnitude higher than meridional shears, and temporal variability above 1 bar

213 erically coherent variations, some proposing meridional shifts in global rainbelt position and the 'g

214 Previous research has suggested that meridional shifts in the ITCZ position on geologic times

215 sheets, freshwater hosing) generally produce meridional shifts in the zonal mean rainbelt, orbital va

216 ction also revealed the characteristic 4.7 A meridional signal and the position of the reflection cou

217 dional spot is present, but the second-order meridional spot (22 nm) disappears.

218 ivation by photorelease of Ca2+, the 14.3-nm meridional spot is present, but the second-order meridio

219 In relaxed fibers, OD patterns show strong meridional spots and layer lines up to the sixth order o

220 cial corals that show a considerably steeper meridional SST gradient than the present day in the cent

221 ENSO strongly rely on correctly modeling the meridional SST gradient, as well as its delicate feedbac

222 clera was conducted, and circumferential and meridional strain components were determined from the di

223 controls had significantly greater temporal meridional strain than B6 and had differences in the rat

224 s for both the effective circumferential and meridional strains (multivariable regression model, P =

225 Circumferential and meridional strains were computed from the digital image

226 arently linked to marked changes in the mean meridional structure of environmental vertical wind shea

227 ection fraction increased 20% (P=0.009), and meridional systolic wall stress decreased 48% (P=0.009).

228 ndicate that the GBR experienced substantial meridional temperature change during the last deglaciati

229 Our reconstruction shows that the meridional temperature gradient between the equator and

230 in baroclinicity associated with an enhanced meridional temperature gradient between the Sahara and G

231 On the other hand, the meridional temperature gradient spanning the Sahel has i

232 t corresponds to the emplacement of a strong meridional temperature gradient that typifies icehouse c

233 cover, which steepened the interhemispheric meridional temperature gradient.

234 n the Eocene cautions against inferring past meridional temperature gradients using spatially limited

235 than B6 and had differences in the ratios of meridional to effective circumferential strain from B6 m

236 A striking shift from meridional to zonal flow occurred at the end of the Litt

237 Meridional tow-yos were used to calculate the amount of

238 Atlantic Ocean, collected on three Atlantic Meridional Transect cruises on consecutive years, that b

239 dant cyanobacterium Prochlorococcus across a meridional transect in the central Pacific Ocean.

240 Here we present meridional transects of dust (derived from the (232)Th p

241 ic hydrologic cycle, such as the strength of meridional transport, are assessed using the North Atlan

242 f greenhouse gas emissions, is used to study meridional transports and their correlations with the Ar

243 gands as "pillars"; all metal centers have a meridional tris-chelate configuration.

244 s support the interpretation of vertical and meridional variability of temperatures in Saturn's strat

245 We identify a large and unexpected meridional variation in stratospheric (16)O(13)C(18)O, o

246 ieve the most plausible explanation for this meridional variation is either an unrecognized isotopic

247 e degree of nonlinearity closely follows the meridional variation of midlatitude storm track frequenc

248 pressed by the left ventricular end-systolic meridional wall stress (35 +/- 13 to 18 +/- 8 kdyn/cm, p

249 Inotropism, measured by using meridional wall stress corrected for ejection fraction,

250 was similar in both groups, despite reduced meridional wall stress in diabetics, suggesting impaired

251 lume, ejection fraction, cardiac output, and meridional wall stress were obtained 1 hour after MDMA a

252 The meridional warm pool expansion evidently had enormous im

253 The meridional width of the fifth layer line peaks is invers

254 a positive relationship between near-surface meridional wind anomalies and female foraging effort, bu

255 idional pressure gradient forces very strong meridional winds without accelerating the zonal wind com

256 Simulated meridional x-ray diffraction profiles and analyses of is

257 While both states displayed a 4.8-A meridional X-ray diffraction typical for amyloid cross-b

258 re of the cytochrome oxidase was studied via meridional x-ray diffraction, which directly provided el

259 es of the (1,1) equatorial and (14.5 nm)(-1) meridional X-ray reflections.