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 Limited meridional airborne transport restricts southward commun

6 Meridional analysis of the refractive data indicated tha

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

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

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

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

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

12 (d) Flat muscles, encircling each meridional canal.

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

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

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

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

17 vers of nutrient supply: vertical mixing and meridional circulation.

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

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

20 ic patterns, which are more predictable than meridional configurations.

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

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

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

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

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

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

27 Meridional diffraction patterns obtained from the orient

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

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

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

31 ation (+50% at Dasuopu) likely linked to the meridional displacement of the winter westerlies from 18

32 North American Atlantic and Gulf coasts the meridional distributions of dissolved inorganic carbon (

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

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

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

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

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

38 icity and compensates the associated oceanic meridional energy transport.

39 ferential wall expansion exceeds the rate of meridional expansion.

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

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

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

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

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

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

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

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

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

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

50 : these flows bear a striking resemblance to meridional flows, long predicted to occur during the ear

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

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

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

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

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

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

57 The meridional gradient is projected to strengthen throughou

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

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

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

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

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

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

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

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

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

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

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

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

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

71 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

72 Meridional intensity profiles of the peaks at the first

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

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

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

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

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

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

79 The meridional isomers for both pyridyl and pyrazolyl-based

80 The three meridional isomers have the expected bond length alterna

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

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

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

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

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

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

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

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

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

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

91 Meridional (mer) coordination promotes the generation of

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

93 ndarily to the positive phase of the Pacific Meridional Mode (PMM).

94 ollowing the pattern of the Southern Pacific Meridional Mode.

95 ts on the atmospheric forcing of the Pacific Meridional Modes (PMM) over 9 months timescales.

96 e North and South Pacific expressions of the Meridional Modes.

97 ween KE and the central tropical Pacific via Meridional Modes.

98 The meridional moisture stress gradient reconstructed from t

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

100 This pronounced meridional moisture transport, which contrasts with the

101 The meridional net flux pattern of this substance is expecte

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

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

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

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

106 to invigoration or weakening of the Atlantic meridional overturning circulation (AMOC) and associated

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

108 The change in the Atlantic Meridional Overturning Circulation (AMOC) and of the Ant

109 tion, affecting the strength of the Atlantic Meridional Overturning Circulation (AMOC) and thereby no

110 omalies in response to slow-down of Atlantic meridional overturning circulation (AMOC) during Heinric

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

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

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

114 ve during glacial periods, when the Atlantic Meridional Overturning Circulation (AMOC) experienced la

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

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

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

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

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

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

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

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

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

124 The Atlantic meridional overturning circulation (AMOC) transports war

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

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

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

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

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

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

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

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

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

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

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

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

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

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

139 diagnostic for the stability of the Atlantic Meridional Overturning Circulation (AMOC).

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

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

142 cean warming acts to strengthen the Atlantic meridional overturning circulation (AMOC).

143 ate Change projections of a slowing Atlantic meridional overturning circulation (MOC) in the 21st cen

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

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

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

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

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

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

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

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

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

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

154 The Atlantic meridional overturning circulation carries warm upper wa

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

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

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

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

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

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

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

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

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

164 In 2005 and 2010, a weakened Atlantic Meridional Overturning Circulation is the primary driver

165 The Atlantic meridional overturning circulation is widely believed to

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

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

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

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

170 undamental to improving climate and Atlantic Meridional Overturning Circulation predictability.

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

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

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

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

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

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

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

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

179 Reorganizations of the Atlantic meridional overturning circulation were associated with

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

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

182 ic stocks in response to a weakened Atlantic Meridional Overturning Circulation(6-8).

183 and supplies the lower limb of the Atlantic Meridional Overturning Circulation, a critical component

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

185 Continued weakening of this Atlantic Meridional Overturning Circulation, as projected for the

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

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

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

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

190 s comprises the deepest limb of the Atlantic Meridional Overturning Circulation, yet questions remain

191 owerful current system known as the Atlantic Meridional Overturning Circulation-the strongest oceanic

192 nto the North Atlantic as part of the global Meridional Overturning Circulation.

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

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

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

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

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

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

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

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

201 ction times to perturbations to the Atlantic Meridional Overturning Circulation.

202 ring times of substantially reduced Atlantic Meridional Overturning Circulation.

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

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

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

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

207 500 years) "overshoot" events, with Atlantic meridional overturning stronger than that of the modern

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

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

210 the Labrador Sea contribution to the global meridional overturning, with a linear relationship betwe

211 ntic after the abrupt resumption of Atlantic meridional overturning.

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

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

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

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

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

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

218 ting spacing of the third and sixth order of meridional reflection (S(M3) and S(M6) ) following tetan

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

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

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

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

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

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

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

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

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

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

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

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

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

232 ipapillary sclera characterized by a stiffer meridional response.

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

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

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

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

237 type hexagonal epithelial cells in organized meridional rows.

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

239 In this paper, the zonal and meridional sea surface height (SSH) wavenumber spectra a

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

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

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

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

244 shifts of advective pathways in the ENA and meridional shifts in the western intergyre region.

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

246 served cyclic rainfall changes are linked to meridional shifts in water vapor transport from the trop

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

248 differences are found between the zonal and meridional spectra, which suggest that SSH wavenumber sp

249 in the eastward-flowing high EKE regions the meridional spectrum is steeper than its zonal counterpar

250 l spectrum is steeper than its corresponding meridional spectrum, while in the eastward-flowing high

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

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

253 e find pronounced regional variations in the meridional steering wind response over North America, bu

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

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

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

257 Circumferential and meridional strains were computed from the digital image

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

259 ace temperature and decrease with decreasing meridional surface temperature gradient, but convective

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

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

262 The third mode-which arises from the meridional temperature gradient as affected by Earth's o

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

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

265 pogenic climate change is strengthening this meridional temperature gradient by cooling the polar low

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

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

268 tivities are weakened because of the reduced meridional temperature gradient under polar amplificatio

269 ification of global warming is weakening the meridional temperature gradient(8-10), acting to weaken

270 in summer is partly explained by a weakening meridional temperature gradient, but changes in vertical

271 cover, which steepened the interhemispheric meridional temperature gradient.

272 al wind response to the enhanced upper-level meridional temperature gradient.

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

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

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

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

277 of [Formula: see text] using a Pacific Ocean meridional transect crossing all major surface biome typ

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

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

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

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

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

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

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

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

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

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

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

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

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

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

292 The meridional warm pool expansion evidently had enormous im

293 The termination of meridional water mass exchange through the Tethyan Seawa

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

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

296 Female survival was positively affected by meridional winds and El Nino-Southern Oscillation (ENSO)

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

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

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

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