ライフサイエンスコーパス: latitude

1 creased for coastal wetlands with increasing latitude.

2 US cities, located from 35.8 to 42.4 degrees latitude.

3 52%) to South Sea (0.70%) with a decrease in latitude.

4 with large increases up to 40 degrees North latitude.

5 and significantly increased with increasing latitude.

6 ssumed, with genetic architecture varying by latitude.

7 n average SNP allele frequency corrected for latitude.

8 and body mass did not vary with elevation or latitude.

9 c diversity and gene flow are partitioned by latitude.

10 s N to largely positive to the north of that latitude.

11 l selection despite having shorter values by latitude.

12 percontinent Rodinia, also positioned at low latitude.

13 y geographically, with a strong signature of latitude.

14 iming of bud set were highly correlated with latitude.

15 stems, and particularly those at low- to mid-latitudes.

16 ation in the field, particularly in northern latitudes.

17 ries of urban warming gradients at different latitudes.

18 as well as climate change initiated at high latitudes.

19 emperate dryland regions, especially at high latitudes.

20 s, whereas actinorhizal species do at higher latitudes.

21 the tropics and detritivore-mediated at high latitudes.

22 inventory for BC emissions at high northern latitudes.

23 amplitude of atmospheric CO2 in the northern latitudes.

24 rrences of crop damage by moose at southerly latitudes.

25 ncrease in seasonal LAI in the northern high latitudes.

26 ly shifts towards higher mean elevations and latitudes.

27 ly and virus introduced from a wide range of latitudes.

28 ies were rarely found at high elevations and latitudes.

29 that was limited to Northern hemisphere high latitudes.

30 for increased primary productivity at higher latitudes.

31 via vapor pressure deficit (VPD) across all latitudes.

32 tions during the Eocene, especially at lower latitudes.

33 E trends, mainly over mid- and high northern latitudes.

34 transports heat from the tropics to the mid-latitudes.

35 ude of large-scale dynamics at extratropical latitudes.

36 e among samples from different altitudes and latitudes.

37 ranitic soils, on west aspects, and at lower latitudes.

38 he increase in AMPP-T and AMPT-P in the high latitudes.

39 northern regions and SR into the circumpolar latitudes.

40 ions between species are more intense at low latitudes [1,2].

41 We find that the peak of the jet (latitudes 10 degrees N to 10 degrees S) suffers intense

42 Compared with those living in lower latitudes (19.0-39.9 degrees ), onset of symptoms was 1.

43 dentified in this study were located between latitudes 20-30 degrees N and 15-25 degrees S, where the

44 summer temperature extremes, species in mid-latitude ( 20-50 degrees ) regions have the narrowest th

45 climate explains about 7-50% of the shift in latitude, 20-36% in longitude and 4-28% of that in eleva

46 des (40-80 degrees N), but negatively in mid-latitudes (25-40 degrees N).

47 n the Indian and Pacific Oceans, between the latitudes 37 degrees N and 37 degrees S, under represent

48 erized ancestry and genetic diversity across latitude (39-48 degrees S).

49 s positively to summer temperature over high latitudes (40-80 degrees N), but negatively in mid-latit

50 to subarctic boreal forest (38 sites between latitudes 48 degrees N and 69 degrees N) in Europe.

51 ms was 1.9 years earlier for those at higher latitudes (50.0-56.0 degrees ) (p=3.83x10(-23)).

52 smaller fraction of taxa at higher vs. lower latitudes (8% vs. 11% of genera), despite 11-fold lower

53 Atmospheric monitoring of high northern latitudes (above 40 degrees N) has shown an enhanced sea

54 from three to five populations at different latitudes across the Arctic.

55 d found that bacterial communities at cooler latitudes also tended to possess greater potential metab

56 ng and changes in water availability at high latitudes alter resource abundance, tree competition, an

57 tion to local environmental conditions (e.g. latitude, altitude), and here we propose that this varia

58 hat would otherwise arise over 14 degrees of latitude and 1 m of shore elevation.

59 envelope of the family across 70 degrees of latitude and 3700 m of altitude.

60 atic variables affecting growth shifted with latitude and altitude.

61 Nmin significantly decreased with increasing latitude and altitude.

62 yses reduced or eliminated the importance of latitude and biome in predicting outcrossing or self-inc

63 For high latitude and elevation portions of the tree's range, our

64 In contrast, toward lower latitude and elevation range limits, the models predicte

65 Patterns across both latitude and elevation were driven by arthropod predator

66 At cool locations (high latitude and elevation), cessation seems to be induced p

67 perature and precipitation forecasts vary by latitude and geographic region suggesting different traj

68 le, and is greater for cold lakes (e.g. high latitude and high altitude), which are characterised by

69 esponse genes PHYC and FRS10 correlated with latitude and longitude and temperature, and with precipi

70 h organic carbon content of the sediment and latitude and longitude as co-variates explained as ca. 7

71 tifying numbers for each incident along with latitude and longitude coordinates determined by global

72 tifying numbers for each incident along with latitude and longitude coordinates determined by global

73 multivariate regression trees fitted to the latitude and longitude of the population centroid of eac

74 ., >/=50 nmol/L] during winter regardless of latitude and skin color.In a longitudinal, double-blind,

75 hors point to an inverse correlation between latitude and the incidence of civil conflict and crime.

76 ition correlate most closely with changes in latitude and to a lesser extent changes in pH.

77 studies, this function is based on a simple latitude and topography model.

78 As latitude and water temperature are tightly coupled acros

79 species are expanding their ranges to higher latitudes and altitudes, resulting in novel species inte

80 k decline in outcrossing rate towards higher latitudes and among some biomes, but no biogeographic pa

81 t bloom timing generally shifts later at mid-latitudes and earlier at high and low latitudes by 5 da

82 ditions; small leaves are also found in high latitudes and elevations.

83 m that is high ( approximately 25%) at high latitudes and low ( approximately 5%) in subtropical gyr

84 g are likely to be felt most strongly at low latitudes and low elevations where metabolism-linked eco

85 coast as anomalies seen in the high northern latitudes and monsoon-influenced areas.

86 f environmental variability at high southern latitudes and provide insight regarding ice sheet sensit

87 igh relative humidity, semi-solid in the mid-latitudes and solid over dry lands.

88 of the natural environment such as altitude, latitude, and greenspaces are important determinants of

89 ble in marine than freshwaters, unrelated to latitude, and highest in food webs containing endotherms

90 e highest responsiveness appeared at central latitude, and moderate growth increase is projected at t

91 amorphosis was especially remarkable in high-latitude animals, as they appeared almost insensitive to

92 ming from maximum sea-level highstand in mid-latitudes, are key features for understanding the climat

93 , with considerable losses occurring in high-latitude areas.

94 ons should be driven to higher altitudes and latitudes as global temperatures rise.

95 s and species to establish at more northerly latitudes as the climate warms, potentially leading to l

96 nd therefore an increase in gene flow across latitudes as the climate warms.

97 and subtropical species moving towards high latitudes, as would be expected in climate warming.

98 Mid-latitude atmospheric circulation was likely impacted by

99 ges in the strength and location of low-high-latitude atmospheric teleconnections.

100 nge becoming trapped within an effective mid-latitude atmospheric waveguide.

101 lative to the rest of the martian mid-to-low latitudes (average crust) and flows in northwest Elysium

102 s shows moderate seasonal variation for most latitude bands, which is in agreement with satellite-bas

103 lternative account for less violence at high latitudes, based on a greater need for cooperation.

104 nearly all of its geographic range, exhibits latitude-based population divergence and nature selectio

105 nge of temperatures than species from higher latitudes because the tropics are hotter.

106 CI, 2.6-11.3) than individuals who lived at latitudes below 35 degrees North, independent of race or

107 rainfall climate in the tropics and the mid-latitude belt of the westerlies operating across the mos

108 ost severe effects expected to occur in high-latitude biomes.

109 is longest in the tropics and high northern latitudes (both vulnerable areas of Earth's climate syst

110 Average low-mid-latitude BSi burial flux in the superocean Panthalassa i

111 y stronger CNDD at tropical versus temperate latitudes but also a latitudinal shift in the relationsh

112 estimates were at a resolution of 0.1 degree latitude by 0.1 degree longitude (roughly 10 km x 10 km)

113 at mid-latitudes and earlier at high and low latitudes by 5 days per decade to 2100.

114 Ectotherms from higher latitudes can generally perform over broader temperature

115 nts show that migrant birds at high European latitudes can use magnetic declination to infer longitud

116 ve and positive effects, while those in high-latitude cities varied no more than expected by chance w

117 ming, and they did so in one of the two high-latitude cities; in the other, Queens (New York City), m

118 cies relatedness, functional feeding groups, latitude, climate, and experimental conditions could be

119 ed on these results, we suggest that the low-latitude closure of ocean basins along east-west trendin

120 an reduce phylogenetic diversity within high latitude communities, if colonizing species are typicall

121 ation, which is the faster warming of Arctic latitudes compared to the global mean, in the 2010s.

122 Changes were greatest at high elevations and latitudes - consistent with purported effects of ongoing

123 re projected to be especially severe in high-latitude continental interiors.

124 temporally discrete LIPs across a large low-latitude continental landmass.

125 t to drive the well documented high- and low-latitude cooling that occurred through the Eocene.

126 t Lizard Island and declined with increasing latitude, corresponding with differences in temperature.

127 after metamorphosis, yet notably only in low-latitude damselflies.

128 mpounds as the altitude increased and as the latitude decreased.

129 bacterial taxa were strongly correlated with latitude, decreasing closer to the equator, which coinci

130 ght to be dust transported from southern mid-latitude deserts.

131 ized that litter quality would increase with latitude (despite variation within regions) and traits w

132 Review of the high latitude distribution of Northern Hemisphere Mesozoic bi

133 ns in Toronto, Ontario, Canada (43 degrees N latitude) during 2009-2013.

134 n the contrary, the establishment of the mid-latitude East Asian monsoon was mainly controlled by the

135 Perennially frozen soil in high latitude ecosystems (permafrost) currently stores 1330-1

136 a GPP increase of 37 +/- 9 per cent for high-latitude ecosystems and 32 +/- 9 per cent for extratropi

137 biodiversity and community structure in high latitude ecosystems are largely unknown but critical to

138 High-latitude ecosystems have the capacity to release large a

139 dvanced emergence is widely reported in high-latitude ectotherms, but a significant number of species

140 s even though surface temperatures in higher latitude/elevation lakes are warming faster.

141 metabolic process is especially weak, higher latitude/elevation lakes had larger responses to warming

142 arming rates are sufficiently fast in higher latitude/elevation lakes, metabolic rate responses to wa

143 r metabolic responses to warming than higher latitude/elevation lakes.

144 g intermittent wastewater emissions and high latitude environmental conditions (low temperatures and

145 ut the harshness and unpredictability of low-latitude environments, calling into question the life hi

146 le and late Eocene epoch, especially at high latitudes, eventually led to continental ice sheet devel

147 ith effects that are not modified by parity, latitude, fetal sex, or smoking.

148 Water from mid-depths at lower latitudes flows in to replace the sinking polar surface

149 and freezing temperatures persist at middle latitudes for 3 y to 4 y.

150 es to warming across mid- and high temperate latitudes, for taxa whose thermal physiology has not bee

151 Therefore, N limitation in higher-latitude forests likely results from ecological constrai

152 dicted to evolve than currently inhabit high-latitude forests suggests a greater role for ecological

153 m, self-reinforcing carbon feedback from mid-latitude forests to the climate system as the world warm

154 cies from filling available niches in higher-latitude forests.

155 not explain N-fixing trees' rarity in higher-latitude forests.

156 ntrations decreased linearly with increasing latitude from 7.7 to 3.0 and from 1.0 to 0.6 pg.L(-1), r

157 pulations in 20 forests that span 12 degrees latitude from Georgia to Maine, USA.

158 between biosynthetic domain composition and latitude, from a practical perspective the identificatio

159 te during late Eocene, at least four degrees latitude further south than today, but that it migrated

160 ted mortality spans approximately 10 degrees latitude (half the native range of the species) and 7% o

161 n a 26-year soil warming experiment in a mid-latitude hardwood forest, we documented changes in soil

162 -fixing trees in frequently N-limited higher-latitude (here, > 35 degrees ) forests is a central biog

163 Across all latitudes, higher elevation species invested in offsprin

164 mpared to a HL diagnosis in summer at higher latitudes (HR = 1.082 [95%-CI: 1.009-1.161], p = 0.027).

165 recipitation record suggests significant low latitude hydrological responses to internal modes of cli

166 The eluent system allows particular latitude in controlling elution order/time of polyprotic

167 n, with positive correlations to storm track latitude in eastern Alaska and northwestern Canada but n

168 s such as black carbon (BC) at high northern latitudes in climate change is hampered by the scarcity

169 annual variability of GPP over mid- and high latitudes in North America.

170 driver of climate variability at mid to high latitudes in the Southern Hemisphere, affecting wildfire

171 count for unique climate impacts at northern latitudes, including near-surface permafrost thaw.

172 Furthermore, increasing northern latitude increases the additional mortality risk conferr

173 oid gluten than persons living south of this latitude, independent of race or ethnicity, socioeconomi

174 quality (greater egg mass) and (ii) whether latitude influences the traits involved and/or the trade

175 ted to astronomically driven changes in high-latitude insolation.

176 The presence of a low- to mid-latitude interhemispheric hydrologic seesaw is apparent

177 odecamethylcyclohexasiloxane (D6)) in a high latitude lake (Storvannet, 70 degrees N 23 degrees E), e

178 High-latitude lakes are particularly sensitive to the effects

179 ncentrations in water and sediment of higher latitude lakes.

180 ummer temperature at colder than warmer high-latitude locations.

181 aregression analysis showed that insolation, latitude, longitude, age, and race have a significant ef

182 sis of baseline risk factor measurements and latitude/longitude of participant residence collected fr

183 The Mediterranean Sea is a mid-latitude marginal sea, particularly responsive to climat

184 In extreme high-latitude marine environments that are without solar illu

185 less common at low latitudes than at higher latitudes, might be a useful indicator of climate change

186 bigger influence on future SOC losses in mid-latitude mineral soils than land use change dynamics.

187 icant driver of mass balance changes in high-latitude mountain systems, and demonstrate that debris-c

188 ove their current elevational limits in high-latitude mountains.

189 MPAs tended to increase, and the role of low-latitude MPAs as a sink for urchins changed significantl

190 Self-seeding within higher-latitude MPAs tended to increase, and the role of low-la

191 rsal limitation seems unlikely to limit high-latitude N-fixer diversity.

192 ry constraints hypothesis - posits that high-latitude N-fixing trees are rare because few have evolve

193 Here, we consider traits necessary for high-latitude N-fixing trees.

194 he interference fringe pattern about the mid-latitude NAA transmitter is due to a 3 km reduction in t

195 h recent observations, and conversion of mid-latitude natural forests to cropland and pastures is acc

196 variations in ocean temperature in the high latitude North Atlantic and Nordic Seas are reflected in

197 ations with paleoceanic records from the mid-latitude North Atlantic and Osaka Bay, southwest Japan.

198 ia is identified as being a special case and latitudes north of the equator as being pivotal in the e

199 sonal mean leaf area index (LAI) at northern latitudes (north of 30 degrees N) between 1982 and 2009

200 ments in the Antarctic ice cores tracked low latitude NWT, consistent with previously published discr

201 Such early, predominantly mid-latitude observations are essential because of shortcomi

202 LIG warming in the extratropical latitudes occurred in response to boreal insolation and

203 Food webs in high-latitude oceans are dominated by relatively few species.

204 We regressed latitude of crop damage against North Atlantic Oscillati

205 sated by storm tracks moving offshore at the latitude of New York City.

206 acking the seasons might differ depending on latitude of origin.

207 e duration of the summer circulation and the latitude of that circulation's ascent branch.

208 Phenological traits varied with latitude of the source population, such that southern po

209 The latitude of the tropical rainbelt oscillates seasonally

210 positions the Kaapvaal Craton at equatorial latitudes of 11 degrees +/- 6 degrees at this time.

211 s more common among individuals who lived at latitudes of 35 degrees -39 degrees North (odds ratio, 3

212 on, a higher proportion of persons living at latitudes of 35 degrees North or greater have celiac dis

213 3.2; 95% confidence interval, 1.4-7.1) or at latitudes of 40 degrees North or more (odds ratio, 5.4;

214 s more common among individuals who lived at latitudes of 40 degrees North or more, independent of de

215 stationary high-pressure anomalies over high latitudes of the CNP.

216 of these extinct birds at both mid and high latitudes on the northern continents provides evidence t

217 change in two dominant ways: range shifts in latitude or elevation and phenological shifts of life-hi

218 But at warm locations (low latitude or elevation), cessation seems to be induced pr

219 and warm-adapted species, and independent of latitude or elevation.

220 ved significant inverse correlations between latitude or longitude, and crude or age-standardized pre

221 ngly large groups occupying Eurasia's middle latitudes, or whether they emerged only with the onset o

222 ing systems are more common at low than high latitudes owing to a greater predictability of plant-pol

223 inusoid pattern is more pronounced at higher latitudes (p = 0.023).

224 ssociated with cold periods at high southern latitudes, perhaps due to a northward migration of the S

225 opulations derived from contrasting European latitudes placed in a novel laboratory environment.

226 rs, dominated by an ammonia-rich, narrow low-latitude plume resembling a deeper, wider version of Ear

227 impacts will be increasingly critical to mid-latitude population centres as sea levels rise and tropi

228 vity is negatively associated with wintering latitude, population size, and migration distance, which

229 ter plasticity (+16 days) compared to higher-latitude populations (+10 days).

230 In a warmer common garden, lower-latitude populations have greater plasticity (+16 days)

231 hnura elegans damselflies from high- and low-latitude populations.

232 or rare species at tropical versus temperate latitudes, potentially causing the persistence of greate

233 al climate change is likely to constrain low latitude range edges across many taxa and habitats.

234 ection of the frequency of life forms across latitudes rather than the strength of plant-pollinator i

235 mined effect measure modification by parity, latitude (region), fetal sex, and smoking.

236 ted across subpopulations defined by parity, latitude (region), fetal sex, and smoking.

237 CA lies within a transition zone, where mid-latitude regions are expected to become wetter and subtr

238 faster rates of climate change in many high latitude regions could combine with local adaptation to

239 in colder regions as compared with that low-latitude regions due to the higher Q10 .

240 An earlier AAO in higher latitude regions was found in this worldwide European-de

241 In high-latitude regions where mixed-layers are deep, this flux

242 brates as sentinels of climate change in mid-latitude regions.

243 All CRT-D patients in LATITUDE remote monitoring (2006-2011), programmed DDD,

244 High latitude sauropod dispersal might have been facilitated

245 tion in the behaviour of dawn singing across latitude, season and species.

246 rvey of inhibitory exposure severity, a full-latitude section of the mid-Pacific and near-equatorial

247 of temperature, rather than being related to latitude, seem to be tightly associated with microsite v

248 realistic climate warming in a seasonal mid-latitude setting.

249 eterized with data from insects at different latitudes, shows that peak abundance occurs earlier in t

250 ly sensed vegetation indices in the northern latitudes since the 1980s have been detected and attribu

251 data for 47 tundra plant species at 18 high-latitude sites along a climatic gradient.

252 phenology might be greater in colder, higher latitude sites than in warmer regions, in part because s

253 oproterozoic Earth was punctuated by two low-latitude Snowball Earth glaciations.

254 The establishment of the simulated low-latitude South Asian (northern Australian) monsoon appea

255 show that springtime zonal winds in the high latitude South Pacific drive western Ross Sea autumn sea

256 driven by springtime zonal winds in the high latitude South Pacific, with a lead-time of 5 months.

257 mean temperature is more detrimental to low-latitude species adapted to high mean temperatures and l

258 nal fluctuations is more detrimental to high-latitude species adapted to low mean temperatures and hi

259 reater phylogeographic diversity than higher latitude species and that intraspecific diversity showed

260 ily lead to a longer activity period in high-latitude species because it elevates summer temperatures

261 We found that lower latitude species had, on average, greater phylogeographi

262 associated with a poleward shift of the mid-latitude storm track.

263 d that its seasonal variation depends on the latitude, such that for people living in two different c

264 osperm families are represented in temperate latitudes suggests internal constraints on the evolution

265 hangelsk (White Sea), biomass burning in mid-latitudes, surface transportation, and residential and c

266 We expected high-latitude taxa to increase in abundance with warming, and

267 nd Scotland, indicating that the low- to mid-latitude teleconnection was also active over annual-deca

268 Convergence Zone (ITCZ) and the low- to mid-latitude teleconnections in the Northern Hemisphere over

269 ial and interglacial time periods, with high-latitude temperature changes on the order of 5-10 degree

270 are increasingly vulnerable to thaw as high-latitude temperatures warm.

271 s a high-precision chronological link to mid-latitude terrestrial and marine sites, and sheds light o

272 osaurs only gradually dominated mid- to high-latitude terrestrial ecosystems millions of years later,

273 ear less affected by light pollution at high latitudes than are late dawn singers.

274 al reproduction, which is less common at low latitudes than at higher latitudes, might be a useful in

275 ng of dawn song across the season and across latitudes than late dawn singers, and also appear less a

276 ific competition by 0.25% for each degree of latitude that an ecosystem is located closer to the Equa

277 At mid-to-high latitudes, the regolith contains high concentrations of

278 s birds migrate from breeding sites to lower latitudes, they become involved in transmission networks

279 Akin to northern sub-polar latitudes, this retreat is generally assumed to be linke

280 of a coastal and inland forests on the same latitude to determine if the proportion of animal tissue

281 ite 4- to 8-y-olds during winter in northern latitudes to maintain serum 25(OH)D >30-50 nmol/L depend

282 Permafrost soil in high latitude tundra is one of the largest terrestrial carbon

283 The records with mis-recorded longitude and latitude values were, in fact, taken from inland, freshw

284 s due to deposition of ash sourced from high-latitude volcanic eruptions.

285 ct the effects of Arctic sea ice loss on mid-latitude weather.

286 not all associations between trait means and latitude were caused by selection acting directly on eac

287 ween the prevalence of AMD and longitude and latitude were obtained by regression analysis.

288 he Southern Ocean and intensification of mid-latitude westerly winds today, such teleconnections coul

289 latitudinally, it is crucial to control for latitude when testing alternative mechanistic explanatio

290 r vapor feedbacks over land in low- and mid- latitudes where surface warming rates depend inversely o

291 sed biomass yields, particularly at northern latitudes, where late-flowering but southern-adapted var

292 axa dominate N-fixing tree richness at lower latitudes, whereas actinorhizal species do at higher lat

293 instantaneous response decreases R p for mid-latitudes, while acclimation lowers this for the tropics

294 Our new understanding of diversity across latitude will guide future research.

295 transition from winter snow to rain in high latitudes will cause significant changes in environmenta

296 othesis that warmer temperatures at northern latitudes will confer a fitness advantage to southern im

297 ion has been seen to vary across seasons and latitudes with plankton taxonomy and activity, and follo

298 Other behavioral differences emerge with latitude, with foraging effort and energy expenditure in

299 y states (LHSs) among the inhabitants of two latitudes would have an impact on the neuronal plasticit

300 have selected spatial data sets (0.5 degrees latitude x 1 degrees longitude) of fish abundance from N