ライフサイエンスコーパス: latitude

1 ST changes, but it had obvious difference in latitude.

2 of magnitude in grasslands across 16 degrees latitude.

3 icance of this relationship was dependent on latitude.

4 -0.79, respectively; P < 0.05), but not with latitude.

5 egions between 21 degrees N and 24 degrees S latitude.

6 n, shelf regions and polewards of 60 degrees latitude.

7 derlie a change in interaction outcomes with latitude.

8 monious predictor of food web structure than latitude.

9 th a migratory divide spanning 20 degrees of latitude.

10 ecosystems and climate in the northern high-latitude.

11 Niche breadths tend to be greater at higher latitudes.

12 reasing severity has been noted in northerly latitudes.

13 es UV tolerance and rice yields at different latitudes.

14 ng to the greater number of species at lower latitudes.

15 impacts of climate change on biota at higher latitudes.

16 certain developing countries along tropical latitudes.

17 TTX levels and snake resistance at southern latitudes.

18 its and in species that have attained higher latitudes.

19 ter in the tropics relative to those at high latitudes.

20 ertebrates at tropical relative to temperate latitudes.

21 apid directional changes should focus on low latitudes.

22 of birds in northern, southern and tropical latitudes.

23 ll and at higher latitudes compared to lower latitudes.

24 those geographical regions situated at lower latitudes.

25 higher frequency of the male mimic at higher latitudes.

26 ospheric CO(2) dynamics in the northern high latitudes.

27 gions becoming warmer or drier, such as high latitudes.

28 limate warming and burning intensify in high latitudes.

29 the rotation peak, near the cloud top at low latitudes.

30 global forest loss, mostly in northern high latitudes.

31 der crops, flax included, spread to European latitudes.

32 ed to be higher in cooler regions and higher latitudes.

33 solved the timing of events in southern high-latitudes.

34 vely at high latitudes and negatively at low latitudes.

35 apting new varieties for growth at different latitudes.

36 driven a marked slowdown observed at higher latitudes.

37 osperms but few angiosperms adapting to high latitudes.

38 at long leads, especially over mid- and high-latitudes.

39 itivity increases sixfold at low versus high latitudes.

40 existence of closely-related species at high latitudes.

41 using Fe isotopes in surface waters at high latitudes.

42 layer at low latitudes than at mid- and high latitudes.

43 ust the angular-momentum distribution at mid-latitudes.

44 engers, and this subsidy decreased at higher latitudes.

45 Climate warming is occurring fastest at high latitudes.

46 ics and at high latitudes, and lowest at mid-latitudes.

47 during the Early Cretaceous at southern high latitudes.

48 rth temperate, tropical, and south temperate latitudes.

49 s of 2.0 degrees -9.9 degrees towards higher latitudes.

50 d chlorophyll-a concentration at low and mid-latitudes.

51 time gene associated with adaptation to high latitudes.

52 cury concentrations are enriched in southern latitudes (10 degrees S-20 degrees S) relative to the eq

53 ber of migrants per species crossing Mali at latitude 14 degrees N were in the trillions, and the nig

54 al forests in China spanning a wide range of latitudes (18 degrees 16' to 51 degrees 37'N) and longit

55 ntial source for the re-peopling of northern latitudes [2].

56 orage of soil organic carbon at mid and high latitudes(2,3), hydroclimate may be the dominant driver

57 m tropical soils relative to those at higher latitudes(5,7), but there have been no warming experimen

58 g late fall and winter in 2 areas of Sweden (latitude 63 degrees N and 55 degrees N, respectively) in

59 e of emission seen only at positive Galactic latitudes(7,8), but again indicative of energy injection

60 LDD distance was positively correlated with latitude, a proxy for migration strategy, suggesting tha

61 che breadths show similar relationships with latitude across groups.

62 predictors of apparent survival compared to latitude alone, the relationship between apparent surviv

63 n also mediate biotic interactions along low-latitude/altitude limits (44 of 68 studies).

64 (RLT) posits that abiotic factors form high-latitude/altitude limits, whereas biotic interactions cr

65 liorate harsh climatic conditions along high-latitude/altitude limits.

66 Low-latitude Amazonia mosquitoes had the fastest larval deve

67 uitoes was accelerated and equivalent to low-latitude Amazonia.

68 Latitude and elevation affected the likelihood and inten

69 diversity generally declines with increasing latitude and elevation, (ii) temperature variability and

70 Study sites spanned 9 degrees in latitude and encompassed a gradient in average temperatu

71 phenology and GEP applied especially to high latitude and high altitude peatlands and during phenolog

72 lant phenologically sensitive phases in high latitude and high altitude regions.

73 d a hump-shaped relationship between CVp and latitude and intermediate phylogenetic and geographic si

74 ies were passerines or nonpasserines surpass latitude and its underlying climatic factors in explaini

75 gradients in pollutants were explored using latitude and longitude centroid positions of polar bears

76 Latitude and longitude coordinates on firearm-related de

77 Vineyard location (i.e. latitude and longitude) was one of the main factors desc

78 The orchards differed in terms of longitude, latitude and microclimate.

79 f airborne bacterial communities varied with latitude and temperature, but not with other meteorologi

80 Variability in agent density increased with latitude and was positively correlated with host density

81 ater depth at 16 sites spanning 5 degrees of latitude and ~700 km along the western boundary of the b

82 omplex movement patterns over ~45 degrees of latitude and ~72 degrees of longitude and distinguish re

83 pothesis that predation is stronger at lower latitudes and can shape contemporary patterns of prey di

84 ts point at the differential response across latitudes and commercial relative maturity, as well as t

85 ring wave generation zones in higher (lower) latitudes and consequent southerly (easterly) wave compo

86 ecies' geographic range shifts toward higher latitudes and elevations are among the most frequently r

87 safeguard against warming from trees at high latitudes and elevations, and considered afforestation o

88 of ectotherms have been demonstrated across latitudes and elevations.

89 geographical niches-from the tropics to high latitudes and from shallow to deep water-which better al

90 vely small range of tropical and subtropical latitudes and grows poorly or not at all outside of this

91 century, many species will move into higher latitudes and higher elevations as the climate warms.

92 that all plants, particularly at mid-to-high latitudes and in their nonhardened state, will become in

93 d with global temperature positively at high latitudes and negatively at low latitudes.

94 and ecosystem productivity at northern high-latitudes and signal continental-scale shifts in the str

95 10,338 (>99%) species, increasing at higher latitudes and with migration, and decreasing with territ

96 ate ultraviolet-light mutagenesis with tumor latitude, and describe tumors with heritable hyperactivi

97 y, nitrogen fixation ability, deciduousness, latitude, and species climate niche.

98 position, cold edges shifted 0.47 degrees of latitude, and warm edges shifted only 0.28 degrees.

99 -density for different attainable yields and latitudes, and (iii) characterize their influence on EOP

100 and whether these responses vary among taxa, latitudes, and elevations.

101 els and snake TTX resistance at the northern latitudes, and higher TTX levels and snake resistance at

102 ed to be greatest in the tropics and at high latitudes, and lowest at mid-latitudes.

103 lated at high latitudes than at intermediate latitudes, and the strength of this effect depended on b

104 Here we turn to the first high-latitude annually-resolved and absolutely dated marine r

105 ssic Rapoport Rule (broader ranges at higher latitudes) applies on a geographical scale.

106 n aerosol Fe and organic ligands in the high-latitude Arctic atmosphere.

107 featuring positive height anomalies in high latitudes are occurring more often as the Arctic warms f

108 Currently, the northern high latitudes are warming at rates nearly double the global

109 ive, the solar wind(1,2) is observed at high latitudes as a predominantly fast (more than 500 kilomet

110 tion correlate with probabilistic changes in latitude at recruitment, in doing so quantitatively fulf

111 ative of the summer solstice at 40 degrees N latitude at sea level on a clear day.

112 ctions between North Atlantic and mid-to-low latitudes at the transition from Marine Isotope Stage (M

113 the top-down teleconnection between the high-latitude atmospheric circulation anomalies and the subtr

114 rnal factor in shaping Asian monsoon and mid-latitude atmospheric circulation.

115 marine aerosols, particularly in coastal mid-latitude atmospheric environments, where it initiates th

116 In the mid-latitude Baltoscandian Basin, conodonts displaying low d

117 r an area of 5 degrees x 5 degrees longitude/latitude based on TRMM/GPM satellite data.

118 hain lengths should increase with increasing latitude because larger-amplitude seasonal fluctuations

119 2) This Oligocene warmth, especially at high latitudes, belies a simple relationship between climate

120 re often as the Arctic warms faster than mid-latitudes, both in the recent past and in model projecti

121 ative temperature estimates for northern mid-latitude bottom waters.

122 tically among species and predictably across latitudes, but causes of this variation are unclear.

123 dicate differences in speciation rate across latitudes, but underlying causes have been difficult to

124 d species did not relocate to the warmer low latitudes, but went extinct.

125 ojected to continue-particularly in northern latitudes-but future greening may be constrained by nutr

126 ts than do terrestrial ectotherms across all latitudes-but that this is the case only if terrestrial

127 ns and spread to tropical forests and higher latitudes by 2050.

128 s show that ectothermic animals also at high latitudes can suffer from overheating and challenge the

129 ompositions were correlated principally with latitude, carbon and carbonates content, and terrigenous

130 twenty years ago, therefore compliments high latitude changes to amplify CO(2) drawdown.

131 cean-atmosphere interaction and low- to high-latitude circulation are thought to be key factors in re

132 Northern Hemispheric high-latitude climate variations during the last glacial are

133 ree in spring compared to fall and at higher latitudes compared to lower latitudes.

134 find that planktonic duration increased with latitude, confirming predictions that temperature effect

135 tent with Arctic cooling: Prior to 6 Ma, low-latitude continental carbon reservoirs expanded during a

136 ncreases with losses of marine ice over high latitude continental shelf areas.

137 nd flooding in the coastal areas of many mid-latitude continents, and thus the atmospheric processes

138 in heating, and we provide evidence that low-latitude coronal holes are a key source of the slow sola

139 interaction strength that may be related to latitude-correlated environmental gradients.

140 t, is commonly deficient over winter in high latitude countries due to insufficient ultraviolet radia

141 n of these data suggests that the global low-latitude deep-pelagic shrimp biomass (1700 million tons)

142 evels of genetic introgression from the high latitude Dent maize grown in Europe.

143 respect to Amazonian populations of similar latitudes do not extend northward.

144 ecules, while the same components from lower-latitude DOM were assigned to lignin-like species.

145 rence, biomass, and feeding intensity across latitudes due to climate change.

146 Surface warming occurs at mid-to-high latitudes due to the physiological acclimation-induced r

147 mmer pole to be rapidly transported to lower latitudes during the night, where it then can be lifted

148 lnerable to climate change were found at all latitudes, e.g. in Australia, Indonesia, the Caribbean,

149 ti-colored flowers advances from low to high latitudes each spring.

150 and mortality of 14 coral genera across high-latitude eastern Australia during a global heat stress e

151 , fierce alternating zonal flows, and a high-latitude eastward jet with a polygonal pattern.

152 attern across all the LMEs, independent from latitude, ecosystem, environmental conditions, and stres

153 oalgae within seawater and sea ice fuel high-latitude ecosystems and drive biogeochemical cycles thro

154 he tightly coupled, nonlinear nature of high-latitude ecosystems implies that short-term (<10 year) w

155 the structure and function of northern high-latitude ecosystems in response to climate change.

156 nt input into soil carbon pools of many high-latitude ecosystems, little is known about the effects o

157 h and soil temperatures across mid- and high-latitude ecosystems, with important implications for sur

158 s influenced by migration timing rather than latitude, elevation, or migration distance such that sym

159 nteract with body size, life stage, habitat, latitude, elevation, phylogeny and International Union f

160 have been adapted to grow at a wide range of latitudes, enabling expansion of cultivation worldwide.

161 everity, coupled with high mortality of high-latitude endemics, point to climate-driven simplificatio

162 Here we show that vegetation at high latitudes enhances the Arctic amplification via remote a

163 dvantageous under stressful high altitude or latitude environment where short growing seasons, low te

164 find evidence of adaptation to cold and high-latitude environments in Alaska, while in the southeaste

165 At these latitudes, EOPD depended mostly on the maximum attainabl

166 For the northern latitudes, EOPD was not only dependent on the attainable

167 At latitudes equatorward of 75 degrees , static stability d

168 at radiative forcing from this massive, high-latitude eruption led to pronounced changes in hydroclim

169 tion rate tended to decrease with increasing latitude, especially in the Northern Hemisphere, and var

170 forces and emerging disease patterns across latitude for a globally distributed disease.

171 as well as that between delta(18)O(carb) and latitude for lakes located on the Tibetan Plateau.

172 Climate change has likely altered high-latitude forests globally, but direct evidence remains r

173 diversity losses are occurring in intact low-latitude forests.

174 n four environments across China, ranging in latitude from 18.23 degrees to 45.75 degrees N, with dif

175 estern Atlantic Ocean spanning 30 degrees of latitude from the temperate zone to the tropics.

176 At high latitudes, greater dispersal distances were driven by mo

177 o different types of endemism; we found that latitude, habitat availability and climate stability had

178 climate on the biological world vary across latitudes, habitats and spatial scales.

179 ons are stronger at lower relative to higher latitudes has a rich history, drawing from ecological an

180 deglaciation in the Southern Hemisphere mid-latitudes has been attributed to the southward transmiss

181 ng during Pleistocene cold periods at middle latitudes have been intensely studied using various appr

182 ics and cold water glendonites in the higher latitudes have been largely dismissed due to ambiguity o

183 We find that, independent of latitude, high-elevation assemblages emerge as exception

184 f locally adaptive loci across 17 degrees of latitude in a four-grandparent outbred mapping populatio

185 its in the field at 20 sites over 20 degrees latitude in China (invasive range) and 28 sites over 17

186 e did not detect any methane over a range of latitudes in both hemispheres, obtaining an upper limit

187 Feeding by invertivores declines across all latitudes in future predictions, jeopardizing a critical

188 ole for moisture and heat transport from low latitudes in North Pacific paleoclimate.

189 ine of seven-fold greater seed set at higher latitudes in the introduced but not the native range.

190 is, fungal diversity is concentrated at high latitudes, in contrast with the opposite pattern previou

191 y associate with seed dispersal distance and latitude, including dispersal mode and plant height.

192 h other species breeding at a similarly high latitude, indicating connectivity across the tundra belt

193 suggest that abiotic factors covarying with latitude interact with the genetic loci underlying plant

194 One potential cue for latitude is magnetic inclination.

195 e relationship between apparent survival and latitude is strongly mediated by intrinsic traits - larg

196 nly observed in tropical and south temperate latitudes is associated with slower metabolic rate remai

197 of many tropical coral populations at higher latitudes is highly dependent on the persistence of up-c

198 ole temperature gradient drives westerly mid-latitude jet streams through thermal wind balance(1).

199 ntury, including a poleward shift in the mid-latitude jet(1,2), a positive trend in the Southern Annu

200 orth American grasslands spanning 16 degrees latitude, Kaspari et al. (2020) tested three hypotheses

201 cated that gradual thermal evolution in high-latitude larvae may offset the negative effects of CPF o

202 avian clades are restricted to Earth's lower latitudes, leading to historical biogeographic reconstru

203 generalization is more beneficial at higher-latitude locations remains equivocal.

204 mogenisation of reef functions at these high-latitude locations.

205 s that included covariates for geographical (latitude, longitude, altitude), temporal (year, season)

206 Thus, across latitudes, low-severity fire is an overlooked factor inf

207 ded for several years by other forms of high-latitude magnetic activity, such as coronal bright point

208 High-latitude marine environments are characterized by cold t

209 understanding of how the physiology of high-latitude marine microalgae is regulated over a polar sea

210 degrees C, average development rate of high-latitude Mata Atlantica mosquitoes was accelerated and e

211 suggests that stronger interactions at lower latitudes may contribute to the maintenance of contempor

212 Analyses of biota at lower latitudes may presage impacts of climate change on biota

213 tronger (weaker) South Atlantic mid- to high-latitudes mean sea-level pressure gradient and zonal wes

214 to 40 degrees of both northern and southern latitudes, mostly in areas with a high anthropogenic act

215 ndarily aquatic tetrapods that inhabited low-latitude, nearshore environments during the Triassic.

216 Regardless of latitude, nesting corresponded with a consistent stage o

217 coincided with substantial decreases in mid-latitude net precipitation (precipitation minus evapotra

218 nally limit phytoplankton growth in the High Latitude North Atlantic (HLNA), greatly reducing the eff

219 and anthropogenic stratification of the low latitude ocean.

220 As high-latitude oceans shift into new climate regimes the analy

221 e species' poleward range extent than by the latitude of diet observation.

222 be used as a navigational cue to control the latitude of recruitment in a trans-global migrant, the M

223 s with the spread of H. sapiens into the mid-latitudes of Eurasia before 45 thousand years ago(3).

224 studies, although in recent decades, the mid-latitudes of the Northern Hemisphere have been rapidly w

225 ere more frequently detected in the northern latitudes of the study area after 2010.

226 erate microbial populations within temperate latitudes of the Tasman Sea.

227 t mountain ranges differing in elevation and latitude offer unique thermal environments in which two

228 nd found much greater variability for higher latitude plots with fewer tree species.

229 Meanwhile, at latitudes poleward of 75 degrees , a low-stability layer

230 rease vulnerability to warming, and that low-latitude populations in general may be more vulnerable t

231 suggests that spatio-temporal changes in low-latitude precipitation prompted geographical range disju

232 r cyclones and decreased net terrestrial mid-latitude precipitation.

233 We find that FPE increases with absolute latitude, precipitation and (all else equal) with temper

234 signal, broadly resembling that of other mid-latitudes proxies, may be attributed to the southward sh

235 rn forewarns profound diversity loss of high latitude radiolaria in the near future, which may have c

236 w excellent agreement between amplitudes and latitude ranges of extreme directional changes in a suit

237 10 and 15 Ma, which then extended to higher latitudes, reaching southern Africa ca. 3 Ma.

238 here is this more prevalent than within high latitude regions where peatlands have, over millennia, a

239 te change, particularly in tropical and high-latitude regions.

240 ttributed to long-range transport from lower latitude regions.

241 netic diversity and their consistency across latitude remain little understood.

242 reconstructed temperate climate at this high latitude requires a combination of both atmospheric carb

243 re negatively and positively associated with latitude, respectively.

244 wice greater in major (sub)tropical and high-latitude rivers than in major temperate rivers, with fur

245 est probability of detection at shallow, low-latitude seamounts.

246 al distances of different species at a given latitude, seeds disperse on average more than an order o

247 place our results within the context of high-latitude seeps and suggest they exert evolutionary press

248 ligobrachia haakonmosbiensis like other high latitude seeps, but additionally displays uncharacterist

249 ffects models revealed that for a one-degree latitude shift in isotherm position, cold edges shifted

250 Locations below 40.5 N latitude showed a positive relationship between AOPD and

251 of coral bleaching occurred at tropical mid-latitude sites (15-20 degrees north and south of the Equ

252 d 10 ka ago reduced diversity at mid to high latitude sites due to the gradual closure of forests.

253 Results show that lake latitude, size, total phosphorus and alkalinity affect c

254 sodium percentage) at different longitudes, latitudes, soil depths, and time periods.

255 diversity primarily resulted from higher low-latitude speciation, driven by spatio-temporal variation

256 diolaria, underwent a severe decline in high latitude species richness presaged by ecologic reorganiz

257 eat tolerance; however, this was buffered by latitude-specific thermal adaptation to both mean temper

258 In the interim analyses of the LATITUDE study, the addition of abiraterone acetate plus

259 ial communities, especially in high northern latitudes such as the Arctic.

260 eaching, the Acropora species common at high latitudes, such as A. glauca and A. solitaryensis, showe

261 elevation were observed to increase at lower latitudes, suggesting that parallel expansion of bloom a

262 eric Rossby wave response with mid- and high latitude surface wind anomalies that contribute to the d

263 were more negative in these stressful, high-latitude systems.

264 coral reef fishes transported into temperate latitudes (termed 'vagrant' fishes) can experience winte

265 s, species were more closely-related at high latitudes than at intermediate latitudes, and the streng

266 ally has a deeper low-stability layer at low latitudes than at mid- and high latitudes.

267 lf the world's lake area is in high northern latitudes that are experiencing rapidly-warming temperat

268 les in the F-region electron content at high latitude, the magnetic flux density at geosynchronous or

269 In high-latitudes, the initial positive climate-fire feedback wa

270 emperatures and the wave power in high south latitudes, the most energetic region globally.

271 27% and 66% of lakes will change to a lower latitude thermal region by 2080-2099 for low, medium and

272 For this northern 6 degrees of latitude, these results suggest that the timing of migra

273 e history and hydrodynamics also covary with latitude-these also affect dispersal, precluding any cle

274 sea-ice cover, is tightly connected to lower latitudes through the North Atlantic.

275 period) allows organisms living at temperate latitudes to anticipate environmental changes.

276 ibility of larger hosts and hosts from lower latitudes to Bd was influenced by thermal mismatches.

277 quantify the ability of the regolith at mid-latitudes to capture atmospheric water which is relevant

278 rming and thermosteric sea-level rise at low latitudes to midlatitudes emerged due to heat convergenc

279 ous development of biorepositories from high latitudes to provide essential libraries to improve the

280 oorganism and nutrient deposition from lower latitudes to these same regions.

281 across temperate regions (23.5-60.0 degrees latitude) to changes in air or sea surface temperature.

282 des independent evidence of synchronous high-latitude-to-tropical coupling of climate changes during

283 projected to increase by about 40% at higher latitudes under the 'no mitigation policy' scenario (RCP

284 de (CO(2) ) concentrations may warm northern latitudes up to 8 degrees C by the end of the century.

285 rogen processes in 34 lakes across 5 degrees latitude varying in trophic status, mixing regime, and b

286 rsist in the environment and can reach polar latitudes via a wide range of routes, such as some persi

287 High-latitude warming is capable of accelerating permafrost d

288 ormation considering diel variability across latitudes, we discuss ways to derive a diel variability

289 cted by cooler temperature regimes at higher latitudes were measured in aquaria.

290 eaker temperature gradient led to weaker mid-latitude westerly flow, weaker cyclones and decreased ne

291 Differences were clearest in temperate latitudes, where ectomycorrhizal plant species are more

292 In more northerly latitudes, where immunological naivety is most likely, w

293 llen-based climate reconstructions from high latitudes, which rely heavily on the presence and abunda

294 feed in the Azores on their way to northern latitudes while sei whales migrate through the archipela

295 rture was later for birds breeding at higher latitudes while the duration of all life phases was simi

296 changes in location and strength of the mid-latitude winter storm track.

297 d shell calcification decreased towards high latitude, with mussels producing thinner shells with a h

298 restrial species to track isotherm shifts in latitude, with some species shifting in the opposite dir

299 ophic seawater from the tropics to temperate latitudes, with several displaying substantial climate c

300 own whether avian survival rates covary with latitude worldwide.