ライフサイエンスコーパス: climatic

1 , particularly rates and spatial patterns of climatic alteration, can help assess potential threats.

2 However, the majority of nearest climatic analogs for protected areas are in nonprotected

3 This study presents quantitative analysis of climatic and anthropogenic factors to streamflow alterat

4 tance to simultaneously consider interacting climatic and biogeochemical drivers when assessing fores

5 nuanced evaluation of spatial variability in climatic and biotic shifts is necessary in order to prop

6 andscapes will be concentrated in particular climatic and competitive environments.

7 habitats, and are important archives of past climatic and ecological information.

8 Despite the climatic and ecological significance of this period, the

9 lling - we aimed to explore the influence of climatic and economic factors on the seasonality of H5N1

10 e rings are increasingly used as proxies for climatic and ecophysiological changes.

11 Given a gradient of climatic and edaphic factors, rather than bistability th

12 e-history traits occurring across periods of climatic and environmental change can cause temporal mis

13 bird changed across a period of substantial climatic and environmental change.

14 The chemical findings are corroborated by climatic and environmental reconstruction, together with

15 Here we explored the climatic and geological drivers of a particularly striki

16 e present offers a unique avenue for linking climatic and hydrologic processes to water resource supp

17 odel for the US West Coast based on combined climatic and local variables.

18 We show that periods of favourable climatic and management conditions that facilitate abund

19 We used large-scale climatic and occurrence data of the solitarious phase of

20 is known about how drylands might respond to climatic and population pressures over the 21(st) centur

21 cus acutissima common gardens with different climatic and site conditions.

22 Here we show that, after controlling for climatic and socioeconomic conditions, earthquake severi

23 portance of some key model aspects including climatic and temporal variations, how ENMs may be releas

24 ould take into account the influences of non-climatic and/or biotic factors (e.g., novel pests) on pl

25 volved in a context of important geological, climatic, and environmental variations.

26 f microbiological, genomic, epidemiological, climatic, and ocean sciences.

27 300 mm), we compared spatially explicit 2011 climatic anomalies to our canopy loss maps.

28 ng vulnerabilities associated with increased climatic anomalies under unprecedented warming condition

29 ecological niche modelling predicts suitable climatic areas for the establishment of crow populations

30 raction between seed-source availability and climatic aridity drove substantial variation in the dens

31 years over the last three decades across the climatic aridity gradient of montane conifer forests.

32 ables (e.g., multiplicity of varieties, pedo-climatic aspects, production and storage conditions) inf

33 Climatic, atmospheric, and land-use changes all have the

34 ion of Rushton's controversial theory of the climatic basis of race differences in violent crime.

35 At climatic boundaries where mangroves are expanding and re

36 This study investigated the climatic causes of growth variability of the evergreen d

37 The impact of climatic change along the Antarctica Peninsula has been

38 ralia we find that, for some combinations of climatic change and water demand, the region could exper

39 esponse of oceanic planktonic communities to climatic change has a large influence on the future stab

40 ently reported as a biodiversity response to climatic change.

41 uncertainty in tropical forests responses to climatic change.

42 o explain the genetic imprints of historical climatic changes and geographic barriers within the Braz

43 Rapid climatic changes and increasing human influence at high

44 es result from the interaction between local climatic changes and other abiotic and biotic factors op

45 Projected climatic changes appear especially unfavorable for speci

46 Climatic changes are altering Earth's hydrological cycle

47 ever, inference of risk from purely physical climatic changes is difficult unless set in a meaningful

48 Ocean and surrounding regions are undergoing climatic changes often attributed to "Arctic amplificati

49 These results support the global effects of climatic changes on distribution shifts and stress the i

50 These results suggest that climatic changes played a major role in shaping species'

51 icting how species will respond to the rapid climatic changes predicted this century is an urgent tas

52 which human societies have responded to past climatic changes remains unclear.

53 a coast provides a high-resolution record of climatic changes synchronous with global perturbations r

54 of the current growing area could experience climatic changes that are large enough to render them un

55 unity changes could substantially lag behind climatic changes, hindering our ability to make temporal

56 netic structure is attributed to Pleistocene climatic changes, in which sky-islands acted as long-ter

57 This shift cannot be explained by climatic changes.

58 versity centers may reflect Pleisto-Holocene climatic changes.

59 al performance of trees might be impaired by climatic changes.

60 ities, but also have to adapt to large-scale climatic changes.

61 eir temporal relationships with the Cenozoic climatic changes.

62 eatments should be based on each site's past climatic characteristics.

63 Changes in climatic conditions along geographical gradients greatly

64 te-dependent differences in soil properties, climatic conditions and agronomic operations (e.g. ferti

65 However, fitness is rarely linked to both climatic conditions and movement of hybrid zones, such t

66 g rapid warming, as the area is experiencing climatic conditions approaching those found on milder, p

67 Suitable climatic conditions are predicted to decline acutely in

68 Warmer and drier climatic conditions are projected for the 21st century;

69 significance of this period, the continental climatic conditions associated with it remain unclear.

70 They then examine the ecological and climatic conditions associated with these different soci

71 arine records, the corresponding continental climatic conditions drive the evolution of terrestrial l

72 Retreat was minimal despite oceanic and climatic conditions during the early-Holocene that were

73 ure and genetic diversity, contrary suitable climatic conditions during the last glaciation, and cont

74 The set of "optimal" climatic conditions found in montane cloud forests is si

75 eems to be determined by the extent to which climatic conditions in the new region resemble those of

76 ancient watersheds to constrain Mio-Pliocene climatic conditions in the south-central Andes near 30 d

77 Climatic conditions influence the culture and economy of

78 l populations and unexpectedly suitable agro-climatic conditions initiated this kind of study.

79 ility indicator (SIG) that captures a set of climatic conditions known to influence the ecology of Ae

80 We estimated the projected pace at which climatic conditions may redistribute across NAM (i.e., c

81 have been significantly different under the climatic conditions of the Last Glacial Maximum (LGM), t

82 cord important information about the ambient climatic conditions present during soil formation.

83 ally, for Stipa species we projected current climatic conditions under four climate change scenarios

84 mulation of the breathing cycle in different climatic conditions via computational fluid dynamics.

85 essed, and relationships with geographic and climatic conditions were studied.

86 ost vulnerable in the late 21st century when climatic conditions will be analogous to the most severe

87 gh all study site areas experienced the same climatic conditions, competitive effects created a compl

88 he earthquake, in the context of appropriate climatic conditions, led to an upsurge in Zika virus (ZI

89 earthquake (M7.8), coupled with appropriate climatic conditions, led to significant destruction in E

90 t regions of the earth transition to altered climatic conditions, new methods are needed to identify

91 sion, in the context of conducive/favourable climatic conditions, which are relevant in a climate cha

92 breeds that are presumably adapted to local climatic conditions.

93 's) were examined under three different agro-climatic conditions.

94 nse to annual variation in crop rotation and climatic conditions.

95 igratory populations in response to changing climatic conditions.

96 t sizes, morphology, land cover, biomes, and climatic conditions.

97 animal populations will respond to changing climatic conditions.

98 a rapidly growing population under changing climatic conditions.

99 variable and only partially attributable to climatic conditions.

100 pes under field conditions and under similar climatic conditions.

101 bacterial genome size and local variation in climatic conditions.

102 ct suitable environmental space under future climatic conditions.

103 ely depending on the cultivar, agronomic and climatic conditions.

104 igrants in a new location despite hospitable climatic conditions.

105 ll as what are likely to be species-specific climatic constraints.

106 ese periods coincided with the mild seasonal climatic contrasts and the Mediterranean climate establi

107 forest swamp-peat dome) suggests a potential climatic control on the developmental trajectory of this

108 time-scales requires an understanding of the climatic controls that govern flood occurrence.

109 n the weakening of the geomagnetic field and climatic cooling.

110 link between weakened geomagnetic field and climatic cooling.

111 Next, we used data from the National Climatic Data Center to estimate the monthly average tem

112 sites monitored between 2001 and 2012, with climatic data in order to estimate the local magnitude a

113 ngol invasion, do not offer new or different climatic data, and are supported by anachronistic produc

114 tionships between field estimates and global climatic data.

115 Local climatic debt decreased as the elevation, habitat divers

116 tial tracking of climate change mediated the climatic debt on the local scale.

117 their spatiotemporal divergence - the local climatic debt.

118 These structural and climatic definitions inflate forest estimates across the

119 ferences 46 Precipitation (PPT) is a primary climatic determinant of plant growth and aboveground net

120 face temperature as an indicator of regional climatic development and the supply of pollen and biomar

121 n Federation is a huge country with dramatic climatic differences between regions.

122 gradients by using null models of background climatic differences within and between southern and nor

123 antic/European region, the data also imply a climatic dipole between Europe and East Asia since the c

124 ia, Europe, Australia, and North America) or climatic distinctions.

125 hese findings stress the need to account for climatic-driven hydrological changes in conservation eff

126 erstanding population responses to different climatic drivers along wide latitudinal and altitudinal

127 ize has not been well quantified nor the key climatic drivers convincingly identified.

128 Identifying the climatic drivers of an ecological system is a key step i

129 This leads to unclear climatic dynamics and limited applications.

130 cs are regulated by the complex interplay of climatic, edaphic and biotic conditions.

131 model to correlatively link tree cover with climatic, edaphic, fire and agricultural practices data.

132 These climatic effects on water chemistry are especially stron

133 esults indicate that climate change and mean climatic effects strongly interacted with forest develop

134 ary in 1242 CE, based on a joint analysis of climatic, environmental, and historical data.

135 We investigated which of the climatic, environmental, geographical and/or historical

136 ation and correlation of the onset of the YD climatic episode at 12,800 Cal B.P.

137 recognition as to the importance of extreme climatic events (ECEs) in determining changes in species

138 r conservation management, particularly when climatic events alter species' distributions.

139 These discrete extreme climatic events can constrain populations and space use

140 of these migrations to various cultural and climatic events evident in the archaeological record of

141 century; however, the role played by extreme climatic events on forest vulnerability is still little

142 Extreme biotic and climatic events pose severe hazards to tropical rainfore

143 crease in frequency and intensity of extreme climatic events, resident marine top predators may not o

144 and natural systems, is the most widespread climatic extreme that negatively affects the land carbon

145 Ecological systems sensitive to climatic extremes may benefit from what we term the 'mod

146 iotic stress and consumer pressure caused by climatic extremes, but limited research has explored thi

147 ed changes in the intensity and frequency of climatic extremes, rather than assuming that future mean

148 recent emphasis on the ecological impacts of climatic extremes, the strategies we describe will be ap

149 supply infrastructure designed to cope with climatic extremes.

150 and antecedent wet conditions (proxy for the climatic factor influencing total fuel and fine fuel str

151 zed the daily variability and trends of four climatic factors (reference evapotranspiration, temperat

152 o agro-ecosystems is mediated by broad-scale climatic factors and access to high-quality forage (i.e.

153 elative influence of different components of climatic factors and evaluate the hypothesis that shifti

154 We aimed to assess the link between climatic factors and occurrence of invasive respiratory

155 and place-specific interventions considering climatic factors are critically important.

156 Our findings show that climatic factors can have a substantial influence on inf

157 gether, but nonlinear dynamics of these four climatic factors have not been assessed simultaneously a

158 by identifying ecological, environmental and climatic factors that influenced the prevalence of antib

159 y multiplying fractal dimensions of the four climatic factors) in north China was higher than that in

160 Combining turbidity with seasonal and climatic factors, additional water quality measures, and

161 s, including sociodemographic, regional, and climatic factors, associated with bedroom allergen expos

162 Compared to significant climatic factors, CO2 had on average an approximately th

163 ies' distribution pattern is associated with climatic factors, which are likely related to food avail

164 likely mediated by El Nino's impact on local climatic factors.

165 bution of variability varies among different climatic factors.

166 Our findings indicate that both physical and climatic features are important for explaining the obser

167 Large-scale climatic fluctuations have caused species range shifts.

168 Given that the effects of climatic fluctuations on local ecosystems are complex in

169 t the influence of Andean geography and past climatic fluctuations on the diversification of this gen

170 raphical and environmental factors including climatic fluctuations since the last glacial maximum (LG

171 ions that are more influenced by basin-scale climatic fluctuations than others.

172 and assessed hypotheses for the influence of climatic flux on spatiotemporal variation in abundances.

173 Modeled climatic forcing indicates that tidal restoration to red

174 al phenological responses of plants across a climatic gradient and suggest the possibility of converg

175 se populations of Scots pine along a 2000-km climatic gradient in Europe.

176 To extend this climatic gradient, we also assembled published leaf wate

177 nt species at 18 high-latitude sites along a climatic gradient.

178 species demography varies along elevational climatic gradients across four states in the northeaster

179 itioning patterns vary systematically across climatic gradients remains unknown.

180 onment is critical for reconstructing Asia's climatic history; however, aspects of the plateau's upli

181 Lake Kivu reveals a complex volcanogenic and climatic Holocene history.

182 but anticipation of the scale and extent of climatic impacts on connectivity are required to achieve

183 els resulting from changing demographics and climatic impacts on hydrology that drive nutrient transp

184 al interactions from the broader edaphic and climatic influences on the formation of soil organic mat

185 imate expectations in reference to other non-climatic interacting factors.

186 n environmental conditions and for which the climatic interaction is now quantified.

187 ent (HYDE) land use data in combination with climatic, landform and lithology covariates.

188 rns rather than gradual changes in long-term climatic means.

189 rom land-based weather stations to develop a climatic model to predict the severity of defoliation ev

190 Climatic models were developed to aid land managers in p

191 Climatic modification of LSWT has numerous consequences

192 We conducted daily disease surveillance and climatic monitoring over an 8-year period between Januar

193 increasing distance from geographic range or climatic niche centre (distance-abundance relationships)

194 The results point to climatic niche conservatism between the two clades.

195 of their geographic range or centre of their climatic niche is a key assumption in many existing ecol

196 e environmental space than did the empirical climatic niche model outputs alone for the majority of m

197 genetic variation, phenotypic plasticity and climatic niche modeling to evaluate plant responses and

198 rojections to projections from the empirical climatic niche models alone.

199 s of data including multilocus DNA sequence, climatic niche models and chromosomal features.

200 tional types with projections from empirical climatic niche models for six tree species in northweste

201 ur study reveals the potential for empirical climatic niche models to over-predict suitable environme

202 ry summers would have fewer opportunities to climatic niche partitioning and other processes rather t

203 greater in regions with rainy summers where climatic niche partitioning is more likely.

204 may be determined by the partitioning of the climatic niche, as ectotherms can rely on water availabi

205 trates sympatric parallel diversification in climatic niche, leaf habit, and diversification rates.

206 behaviour to buffer constraints along their climatic niche.

207 eriods to understand whether both subspecies climatic niches differ from each other, what is the curr

208 demographic strategies occur within species' climatic niches, demographic strategies are more constra

209 analyzed these in conjunction with shifts in climatic occupancy and lineage diversification rate.

210 with shifts in either diversification rate, climatic occupancy, or rate of evolution.

211 e WGDs were associated with shifts to colder climatic occupancy.

212 nts, including sociopolitical, economic, and climatic occurrences.

213 ojected them to 2070 and to the mid-Holocene climatic optimum, the world's last major warming event

214 nd magnitude, the impact of the mid-Holocene climatic optimum.

215 e et al.'s global CLASH model overemphasizes climatic origins and underemphasizes economic origins of

216 of P. hwangshanensis during the Pleistocene climatic oscillations could have been the cause of the o

217 y by extrinsic environmental changes such as climatic oscillations in the Quaternary or by intrinsic

218 hat are impacted by similar geographical and climatic parameters.

219 forecast growth trends up to year 2100 using climatic predictions.

220 gic processes, and may be loosely coupled to climatic processes and therefore buffered from climate c

221 rectly altered plankton abundance, bottom-up climatic processes dominate plankton dynamics.

222 ive the surface ocean sulfur cycle and local climatic processes through the production and exchange o

223 sightings are likely related to longer-term climatic processes, and therefore have potential use to

224 e integration of habitat use information and climatic projections may provide insights on the consequ

225 Climatic projections were based on four ensembles CO2 em

226 samifera are partially normalized across its climatic range by the habitat it occupies or by the phys

227 or mycorrhizal association, sample size, and climatic range, foliar delta(15)N in P. balsamifera was

228 e Mediterranean livestock beyond its natural climatic range.

229 Using phylogenetic relatedness, climatic ranges, growth form and mycorrhizal association

230 ed to remain suitable in the future (e.g., a climatic refugia) is in currently protected landscapes (

231 ent experiments, genera affiliated to wetter climatic regimes show higher drought-induced mortality t

232 ate regions, and thus, more studies in other climatic regions are needed.

233 val, occurring in January-February, in the 3 climatic regions for 5 out of the 8 study years.

234 Most peat is found in cool climatic regions where unimpeded decomposition is slower

235 ten rich in V compared to soils of temperate climatic regions.

236 Evidence of climatic regulation of domoic acid in shellfish over the

237 Also, we interpret climatic relocation patterns in terms of associated land

238 implicated or correlated with group-specific climatic requirements.

239 Nine modeling groups simulated agronomic and climatic responses at low-input (Chinoli, Bolivia and Gi

240 understand coral acclimatisation to complex climatic scenarios and may serve as a reservoir of coral

241 tly over and above temporal variation within climatic scenarios, highlighting the need for future stu

242 nd parameterized the model for two different climatic seasons.

243 enetic differentiation due to past divergent climatic selection vs. plastic responses to ongoing clim

244 document the nonlinear relationship between climatic sensitivity and GHG levels over the past four g

245 Climatic sensitivity of the three indicators was assesse

246 re often idiosyncratic and inconsistent with climatic shift predictions.

247 These climatic shifts have been associated with major rearrang

248 The spatial tracking of climatic shifts is frequently reported as a biodiversity

249 ing the exposure of coffee farming to future climatic shifts.

250 ed to have amplified an existing, but subtle climatic signal that was previously absorbed by natural

251 le during the late Paleozoic ice age and the climatic significance of the fossil carbon stored in Ear

252 large reductions in the amount of available climatic space potentially promoting widespread range co

253 narrow elevational ranges, likely reflecting climatic specialization.

254 e applied this approach to assess the future climatic stability and connectivity of Japanese waters a

255 nary speed, environmental predictability and climatic stability hypotheses, but productivity and topo

256 Seedlings may be particularly vulnerable to climatic stress given low stored resources and undevelop

257 HIKV transmission was the combination of the climatic suitability for CHIKV transmission potential an

258 ity for CHIKV transmission potential and the climatic suitability for the presence of Ae. albopictus;

259 side information on dispersal strategies and climatic suitability.

260 ies persistence in the face of deteriorating climatic suitability.

261 to their climate-of-origin or exhibit broad climatic suitability.

262 Climatic surveillance should be used to forecast invasiv

263 Heat and drought are two emerging climatic threats to the US maize and soybean production,

264 loss occurred in areas that passed specific climatic thresholds: warm season anomalies in mean tempe

265 ests that already occur at the edge of their climatic tolerance are most prone to conversion to non-f

266 continental conditions, it encompasses wide climatic, topographic and environmental gradients, and,

267 e population size crashes at major points of climatic upheaval.

268 model species to explore growth responses to climatic variability (seasonal temperature and precipita

269 requires understanding species responses to climatic variability and extremes.

270 frica exhibits one of the largest signals of climatic variability and with a population reliant on ag

271 m to establish this context using historical climatic variability, as a proxy for local adaptation by

272 With increasing climatic variability, it will be particularly important

273 and in particular sunflower, based on annual climatic variability.

274 ng climate change) and (ii) to explore which climatic variables (temperature or precipitation) trigge

275 Climatic variables accounted for 20.68% 44.6% of the dec

276 adients, although the timing and strength of climatic variables affecting growth shifted with latitud

277 el is driven solely by fishing mortality and climatic variables and based on time-series data coverin

278 We found that while climatic variables are associated with seasonal variatio

279 sitoid numbers released, elevation, or local climatic variables at sample locations.

280 Large trees were correlated to a set of climatic variables following a hump-shaped curve.

281 ed several hypotheses for how geographic and climatic variables should affect diversification using a

282 ae and Stipa species occurrences, as well as climatic variables, we predict potential geographical di

283 lf of the northern hemisphere where temporal climatic variance is high.

284 lations in 27 study areas, we determined how climatic variation affected population growth rates and

285 Understanding how climatic variation affects animal populations and commun

286 Thus, understanding the relationship between climatic variation and fire activity is a critically imp

287 Climatic variation played a significant role in explaini

288 cts of stocking and contemporary patterns of climatic variation were strongly related to the spread o

289 ic rates responded in opposing directions to climatic variation, emphasising the need for integrated

290 ce (MARSS) models were fitted, incorporating climatic variation.

291 uture climate, we found that variation among climatic velocities derived from different general circu

292 ties based on spatiotemporal metrics such as climatic velocity.

293 the record of a transient interval of severe climatic warming across the Toarcian Oceanic Anoxic Even

294 iously been shown to respond more rapidly to climatic warming compared to local summer surface air te

295 To generate a realistic climatic warming scenario we used naturalistic outdoors

296 In the context of ongoing climatic warming, certain landscapes could be near a tip

297 rm average climate [i.e. 35-year mean annual climatic water deficit (CWD)] and competition (i.e. tree

298 With increasing climatic water deficit, higher propagule pressure (i.e.,

299 re highly local and depend on the underlying climatic zone.

300 gional evolution of DTR trend over different climatic zones in India using a non-stationary approach