ライフサイエンスコーパス: climatic

1 l contributors to maize yield under changing climatics.

2 ansforms the hydrologic(1,2), ecologic(3,4), climatic(5) and socio-economic(6-8) functions of river c

3 iple, simultaneous environmental changes, in climatic/abiotic factors, interacting species, and direc

4 erature has focused on genomic signatures of climatic adaptation, but little is known about how plast

5 zing the value of integrative assessments of climatic adaptive traits for accurate estimation of popu

6 ct of interannual and long-term (>3 decades) climatic and anthropogenic change affecting Borneo's coa

7 redict their structure from past and present climatic and anthropogenic factors.

8 Given future changes in climatic and atmospheric processes, climate and ecologic

9 rve as biomarkers for reconstructing Earth's climatic and biogeochemical evolution.

10 marine sediments has the potential to record climatic and biotic changes in the pelagic community wit

11 assessments of contaminants interacting with climatic and biotic stressors.

12 rogen (N) and phosphorus (P) concentrations, climatic and catchment characteristics for up to 1406 la

13 lerances, a fuller understanding of how past climatic and ecological changes impacted those animals a

14 The history of human responses to climatic and ecosystem changes in Arabia can provide imp

15 phological heterogeneity we investigated how climatic and edaphic factors affect tropical forest dive

16 mposition was influenced by a complex set of climatic and endogenous variables.

17 n terrestrial biodiversity during periods of climatic and environmental change.

18 Here we show evidence for stable climatic and environmental conditions during the MUPT in

19 d from a perspective that takes into account climatic and environmental conditions favourable for bot

20 rbon dioxide (CO(2) ) seasonal cycle and its climatic and environmental controls across Alaska and no

21 posit a link between the origin of Homo and climatic and environmental shifts between 3 and 2.5 Ma.

22 tion of crop varieties that are resilient to climatic and environmental stressors.

23 nts and organisation of canopy traits across climatic and geochemical conditions remain uncertain.

24 iodiversity is likely to change with ongoing climatic and land-use changes, pointing toward particula

25 ontext, such as those associated with global climatic and land-use changes, will have important long-

26 Here, we investigated potential climatic and landscape drivers of flowering onset, offse

27 ii) measure the spatio-temporal evolution of climatic and natural hazard events recorded, and (iii) e

28 idly adapt is key to survival in the face of climatic and other anthropogenic changes.

29 Harsh climatic and sanitary conditions, poor border controls a

30 are also among the most vulnerable, and that climatic and socio-economic changes will affect them pro

31 overnance, hydropolitical tension and future climatic and socio-economic changes.

32 d use and biomes since 1700, and 16 possible climatic and socio-economic scenarios until the year 210

33 This heterogeneity is impacted by climatic and stochastic forcing, but additional high-res

34 ime shifts can abruptly affect hydrological, climatic and terrestrial systems, leading to degraded ec

35 for bias, to better disentangle broad-scale climatic and urbanization effects on body size.

36 cumentation both attest, moreover, to severe climatic anomalies following the proposed eruptions, lik

37 ed tree mortality, but interactions of these climatic anomalies had the highest and most positive imp

38 and their ability to respond to large-scale climatic anomalies.

39 ests different possibilities for using paleo-climatic, archaeological, and genomic evidence to establ

40 ollution problems at a time when episodes of climatic aridity were prevalent.

41 d global patterns of diversification and its climatic association.

42 To characterize the genetic basis and climatic associations of natural variation in seed chill

43 ion years to assess the frequency of and the climatic backgrounds capable of triggering large NADW re

44 rassland fire dynamics are subject to myriad climatic, biological, and anthropogenic drivers, thresho

45 with the environment are crucial to address climatic challenges and assist the breeding of novel cul

46 the response of the terrestrial biosphere to climatic change and other anthropogenic forcing.

47 te how mean climatic conditions and rates of climatic change impact parasitoid insect communities in

48 n cloud-to-ground lightning frequency due to climatic change will alter tree mortality rates; project

49 Schelling, Climatic Change, 33, 303-307 (1996); J.

50 Virgoe, Climatic Change, 95, 103-119 (2008)].

51 h Himalaya (HKH) are changing rapidly due to climatic change, but an overlooked component is the subn

52 onse of floral pigmentation to anthropogenic climatic change, suggesting that global change may alter

53 olonization in the island may be affected by climatic changes and/or other anthropogenic influences.

54 Climatic changes can induce geographic expansion and alt

55 persistence of lineages, shaped by long-term climatic changes interacting with topographically dynami

56 It is conceivable that climatic changes may be beneficial in one season but res

57 studies on the biological effects of future climatic changes rely on seasonally aggregated, coarse-r

58 rall, our results help identify the specific climatic changes that cause extinction and the processes

59 laeolithic in Europe was a time of extensive climatic changes that impacted on the survival and distr

60 water availability may be highly impacted by climatic changes that increase soil and atmospheric mois

61 at there is a fine-resolution variability in climatic changes, driven primarily by interactions betwe

62 his pandemic was linked to recent historical climatic changes.

63 s century) driving widespread ecological and climatic changes.

64 hip where volcanic degassing triggers global climatic changes.

65 f the increased rate and intensity of global climatic changes.

66 The observed behavior of climatic complexity could be explained by the changes in

67 atological space and differ significantly in climatic composition.

68 Under current climatic conditions (2002-2012), we predict that harmful

69 ate that biotic factors can ameliorate harsh climatic conditions along high-latitude/altitude limits.

70 n in penguins was largely driven by changing climatic conditions and by the opening of the Drake Pass

71 flourishing of the oasis, facilitated by wet climatic conditions and higher river flows that favored

72 Here, we investigate how mean climatic conditions and rates of climatic change impact

73 Arabidopsis accessions to adapt to different climatic conditions and year-on-year fluctuations.

74 Human activity is changing climatic conditions at an unprecedented rate.

75 Predictions of future climatic conditions at local scales, the most relevant t

76 ggesting that these forests are experiencing climatic conditions beyond their adaptative limits.

77 erbivore exclusion and alterations in future climatic conditions can negatively impact soil net N(min

78 rience lower and more unreliable rainfall as climatic conditions change over the next century.

79 Their prompt settlement under climatic conditions differing drastically from that of t

80 need to more accurately estimate the future climatic conditions experienced by organisms and equips

81 ng which the pandemics emerged, the modelled climatic conditions for B. tabaci improved significantly

82 hat the requirement to cooperate under harsh climatic conditions generates social competition for rep

83 Yet, fluctuating climatic conditions have been shown to also promote coop

84 Climatic conditions in regions with the highest burned a

85 models suggest the possibility of Earth-like climatic conditions on Venus for much of its earlier his

86 Uncertainties over future climatic conditions pose significant challenges when sel

87 d this effect was consistent for edaphic and climatic conditions representative of 52% of the rainfed

88 that crop management adaptation to changing climatic conditions strengthen agroecosystem resistance

89 It remains unclear under what climatic conditions these species could maintain competi

90 s highlight the increasing novelty of annual climatic conditions viewed through a multivariate lens a

91 tion that is adapted to a wide range of agro-climatic conditions(2).

92 ed for their adaptations to local biotic and climatic conditions, but more recently, the species has

93 ic compounds, being related to the different climatic conditions, especially water status.

94 rn Europe during a period of highly variable climatic conditions, including interglacial and glacial

95 in Arctic communities because of challenging climatic conditions, limited options for the transportat

96 First, by manipulating climatic conditions, such as temperature, humidity, etc.

97 ccounting for evolution in socioeconomic and climatic conditions, we estimate future interregional vi

98 ions are experiencing significant changes in climatic conditions, which may induce strong shifts in t

99 ng flowering under current and future hotter climatic conditions.

100 l group sizes experienced similar effects of climatic conditions.

101 might have struggled under more challenging climatic conditions.

102 ide, various soil and plant descriptors, and climatic conditions.

103 ecosystem states under episodically extreme climatic conditions.

104 shaping species' poleward range boundaries, climatic constraints are often assigned greater importan

105 nmental measurements were used to assess the climatic constraints on turgor-driven growth.

106 ross different ecological, anthropogenic and climatic contexts.

107 boveground net primary production and assess climatic controls among biomes.

108 c debt with two classes of intervention: (i) climatic credits that pay some of the debt, reducing the

109 n plants and animals, using phylogenetic and climatic data for 19 plant clades and 17 vertebrate clad

110 Many organisms are accumulating climatic debt as they respond more slowly than expected

111 inrichs question our interpretation that the climatic debt in understory plant communities is locally

112 is especially evident in the ocean, whereas climatic debt may be accumulating on land.

113 opose a simple budget framework to integrate climatic debt with two classes of intervention: (i) clim

114 es and propose an alternative way to analyze climatic debt.

115 patterns of spatial variation and potential climatic dependence.

116 These results provide evidence that climatic differences may contribute to differences in ed

117 unity structure, and increased taxonomic and climatic differentiation of the species inhabiting the t

118 The imprint of this climatic dipole is manifest for years postfire, as evide

119 endrochronological records to correlate this climatic dipole with short-term postfire juvenile recrui

120 withdrew from this region due to a dramatic climatic downturn.

121 ecisions differed noticeably from the purely climatic driven phases with smaller percentages of advan

122 TWSDI) that decomposes the anthropogenic and climatic-driven components of GRACE observations.

123 summer precipitation was the most important climatic driver (r = 0.67, p < 0.001), responsible for 3

124 This study unequivocally illustrates how a climatic driver can influence local-scale demographic pr

125 avelled the full mechanistic path by which a climatic driver, the Atlantic trade winds, determines th

126 The climatic drivers and genomic basis of seed mass variatio

127 oss Mexico and southern USA, to identify the climatic drivers of (changes in) bat migration phenology

128 lower mean annual temperature were the main climatic drivers of higher decomposition rates, while bi

129 Using a sliding window approach, we assess climatic drivers of phenology in all three trophic level

130 cific characteristics than local or regional climatic drivers.

131 cells, across the Americas and determine key climatic drivers.

132 erpret these differences in vulnerability to climatic drought and climate change.

133 We found that in addition to climatic drought severity (i.e., rainfall), subsurface p

134 ogenetic diversity over time during a recent climatic drying trend.

135 Yet how these climatic effects compare to other anthropogenic forcings

136 We simulate the climatic effects of six war scenarios on fish biomass an

137 and inter-annual variability associated with climatic effects on hydrology.

138 a with adjustments for nutrient loadings and climatic effects; (3) to estimate APPP from model predic

139 velop an alternative approach to delimit the climatic envelope of the two biomes in Africa using tree

140 human presence was facilitated by favourable climatic episodes.

141 nd in the frequency and intensity of extreme climatic events [1].

142 Extreme climatic events including marine heatwaves (MHWs) are be

143 ent chronologic precision to document abrupt climatic events on a centennial-millennial time scale.

144 Characterising how climatic events were expressed in local environments is

145 ribing sensitivity to climate and to extreme climatic events) and reproductive success in Norway spru

146 otas have been shaped by past geological and climatic events.

147 l contribute to these extinctions is extreme climatic events.

148 to build health system resilience to extreme climatic events.

149 hese patterns with the available genetic and climatic evidence.

150 Favoring a non-climatic explanation, we propose instead that the abando

151 rrying capacity of forests as they adjust to climatic extremes and changing disturbance regimes.

152 r global plant trait relationships extend to climatic extremes, and if these interspecific relationsh

153 ntly associated with top-down effects, while climatic factors are stronger determinants of microbiome

154 Climatic factors can increase the strength, variability,

155 ward and upward with climate change, but non-climatic factors complicate these predictions.

156 Climatic factors explain variation in rates better than

157 While climatic factors explained variation in breeding density

158 sserines surpass latitude and its underlying climatic factors in explaining global patterns of appare

159 Whereas regional climatic factors may generate population synchrony (i.e.

160 e of expansion was far from homogeneous, and climatic factors may have driven a marked slowdown obser

161 uce juvenile susceptibility to predation and climatic factors overwinter.

162 of different regions, constituent fluxes and climatic factors to carbon cycle IAV.

163 y considering socioeconomic, ecological, and climatic factors we highlight the importance of a noneur

164 Climatic factors, such as the drought index and growing

165 dies that simultaneously manipulate multiple climatic factors, which will enable us to generate more

166 rhinoceros was impacted by human arrival and climatic fluctuations [2].

167 ighlights how species respond differently to climatic fluctuations and further illustrates the potent

168 listic evolutionary responses to Pleistocene climatic fluctuations have shaped patterns in genetic di

169 By doing so, we aim to detect possible climatic fluctuations that may have led to the abandonme

170 s into and out of refugia during Pleistocene climatic fluctuations.

171 Climatic forcing arose only when susceptible availabilit

172 Fonio diversity is shaped by climatic, geographic, and ethnolinguistic factors.

173 rchaeological sites that are located along a climatic gradient in Western Greenland.

174 creasing postfire albedo along a south-north climatic gradient was offset by a nearly opposite gradie

175 ments in terms of water stress across a wide climatic gradient, indicating that subsurface hydrology

176 sity showed a large decrease along a wet-dry climatic gradient.

177 shifting in these facets of diversity along climatic gradients in response to climate change.

178 ity respond to a changing environment across climatic gradients is essential for effective long-term

179 erved spatial variation (where, for example, climatic gradients result in spatial variations equivale

180 ealm where barriers (oceanographic currents, climatic gradients) have not yet been broken.

181 relationship and its stability along global climatic gradients.

182 We find a decade-long negative climatic impact that intensifies with soot emissions, wi

183 Brown carbon (BrC) has significant climatic impact, but its emission sources and formation

184 Climatic impacts are especially pronounced in the Arctic

185 eless, the more widespread environmental and climatic impacts of this large eruption are not well kno

186 The NAO spatial structure and associated climatic impacts over Europe are not stationary making i

187 With AAMA-based case studies, we document climatic influences on the migration phenology of eagles

188 h early metabolic evolution may cause strong climatic instability, a low CO:CH(4) atmospheric ratio e

189 ests and show that thermophilization and the climatic lag in forest plant communities are primarily c

190 arbon accumulation in relation to a suite of climatic, landscape and local factors.

191 with the development of new high-resolution climatic layers for Antarctica, to better understand how

192 limitations caused by reproductive costs and climatic limiting conditions.

193 ost strongly related physiological traits to climatic limits among angiosperms, but not among conifer

194 d which physiological traits explain species climatic limits among temperate rainforest trees in a re

195 sistance is the most useful predictor of the climatic limits of angiosperm trees.

196 f dry matter content did not explain species climatic limits.

197 traits were most strongly related to species climatic limits.

198 Each SD increase from the climatic mean decreases county-level fishing employment

199 , we identify a north-south dipole in annual climatic moisture deficit anomalies across the Interior

200 has triggered both rapid adaptation to a new climatic niche and acquisition of herbicide resistance,

201 These results support the tolerance and climatic niche conservatism hypotheses for climate-diver

202 Climatic niche is negatively associated with diversifica

203 , suggesting that geographic range edges and climatic niche limits correspond less frequently than we

204 The climatic niche model was corroborated with independent o

205 We used CLIMEX, a process-oriented climatic niche model, to explore if this pandemic was li

206 Here, we test ten predictions about climatic-niche evolution in plants and animals, using ph

207 However, it remains unclear if climatic-niche evolution is similar in plants and animal

208 ts suggest that there are general 'rules' of climatic-niche evolution that span plants and animals, d

209 Climatic niches are essential in determining where speci

210 For example, in both groups, climatic niches change at similar mean rates and species

211 cross vascular plants, we tested whether the climatic niches of polyploid species are more differenti

212 ated than their diploid relatives and if the climatic niches of polyploid species differentiated fast

213 latory signals that are distinguishable from climatic noise.

214 The Miocene Climatic Optimum (MCO, 14-17 Ma) was ~3-4 degrees C warm

215 Species radiation during the Mid-Eocene Climatic Optimum also coincided with several morphologic

216 ies that existed in Beringia during the MIS3 climatic optimum when the mammoth was alive.

217 Earth's climate has cooled since the Miocene Climatic Optimum, leading to growth of the Antarctic ice

218 Our findings suggest that the climatic oscillations during the Pleistocene have driven

219 Our analyses confirm extensive climatic overlap of forest and savanna, supporting the a

220 In Alpine regions changes in seasonal climatic parameters, such as temperature, rainfall, and

221 vironmental deteriorations such as prolonged climatic perturbations and oceanic anoxia, related to th

222 direct impacts, is expected to cause global climatic perturbations through injections of soot into t

223 ast 640,000 years suggests pacing by Earth's climatic precession, with each glacial-interglacial peri

224 een the daytime and night-time will skew the climatic pressures placed on them, and this could have p

225 t corals can help build past (century-scale) climatic profiles, and better understand coral persisten

226 mazon fishes, coupled with dam locations and climatic projections (2070s), we (a) evaluated the poten

227 de range of grasslands that vary in soil and climatic properties.

228 n) were contingent on site-specific soil and climatic properties.

229 ex is used alongside other environmental and climatic proxies to reconstruct Late Upper Palaeolithic

230 ill only include a tiny fraction (4%) of the climatic refugia of KMD, the fate of the species will be

231 communities were more stable under changing climatic regimes, with lower variations in temporal dyna

232 ence patterns across a relatively homogenous climatic region.

233 sed on average by 0.3 km/year and cumulative climatic resistance increased for ~83% of the continent.

234 We explain the lagged climatic response by a shift in the dominant mode of atm

235 rigin affect local and global hydrologic and climatic responses.

236 to locations where they are more exposed to climatic risk than at their origin locations.

237 high-elevation aquatic insects can mitigate climatic risks via these pathways is largely unknown.

238 s under a rapidly changing environmental and climatic scenario.

239 d in our model, deterioration risk under all climatic scenarios was best reduced by increasing the co

240 Strong climatic seasonality and drought in both dry and wet sea

241 esponses to climate change in areas of lower climatic seasonality, and in areas where a greater propo

242 mnosperms, observations from sites with high climatic seasonality, especially precipitation seasonali

243 stigate phenotypic plasticity as a target of climatic selection, hypothesizing that lineages that evo

244 the range of baleen whales, mirroring known climatic shifts and identifying new habitats that will r

245 ossible relationships between geographic and climatic space, suggesting that geographic range edges a

246 ater cycling with important implications for climatic stability at global scales.

247 vironment, even in areas with high levels of climatic stress.

248 ke dwarf mistletoe can amplify the impact of climatic stressors of trees, contributing to the vulnera

249 vegetation carbon allocation under increased climatic stressors, it is crucial to treat growth respon

250 al Africa, the estimated geographic range of climatic suitability for malaria transmission is more se

251 Climatic suitability modeling indicates that, depending

252 ting niche modelling approach to project the climatic suitability of 11 triatomine species under curr

253 We also determined the climatic suitability of two temperate species (T. infest

254 spersal (winds experienced at the strait and climatic suitability) against genetic differentiation be

255 traints (winds experienced at the strait and climatic suitability).

256 mulate future spread of the disease based on climatic-suitability modeling and radial expansion of th

257 implies a weakening negative feedback on the climatic system and increased societal dependence on fut

258 t, long-term behavior of AMV is unknown, but climatic teleconnections to regions beyond the North Atl

259 down along three axes when crossing the same climatic threshold.

260 Climatic, topographic, geological, social, and morpholog

261 arning techniques and a comprehensive set of climatic, topographic, soil, and remote sensing data to

262 This climatic transition is coincident with a documented shif

263 terial diversity hotspots; located mainly in climatic transition zones that are sensitive to potentia

264 net diversification, probably in response to climatic transitions or ecological opportunity.

265 ive remediation strategies in face of future climatic uncertainties.

266 Determining when climatic uncertainty breeds social discord or promotes c

267 Vp (wind pollination and seed dispersal) and climatic variability (variability of summer precipitatio

268 Most studies quantifying the impacts of climatic variability and warming on crop production have

269 ities might have started to overtake natural climatic variability as the dominant controls of dust st

270 These findings underscore the importance of climatic variability at multiple spatiotemporal scales i

271 ate stations showed intensifying aridity and climatic variability in many of these sensitive regions.

272 nderstanding of the global processes driving climatic variability in the region.

273 temporal extent to which recurring modes of climatic variability shape patterns of postfire recovery

274 e sensitivity of carbon supply and burial to climatic variability, with Little Ice Age cooling causin

275 c evolution and dispersal during a period of climatic variability.

276 The association of recorded climatic variables and individual gene expression across

277 test our findings, we assess whether similar climatic variables are associated with host abundances i

278 with elevation or in relation to associated climatic variables in conifers - treeline-dominant Pinus

279 may need to consider the effect of changing climatic variables on future intervention strategies.

280 tainty, especially concerning the impacts of climatic variables on the carbon cycle.

281 AI, soil coarse fragment volume) rather than climatic variables such as mean/standard deviation of te

282 wide), and investigated how K(S) varied with climatic variables, plant functional types, and biomes.

283 r-annual to centennial, and for very diverse climatic variables.

284 m adverse impacts of the marked inter-annual climatic variation that occurred during the study period

285 ale environmental fluctuation (e.g. regional climatic variation).

286 Bee emergence was sensitive to climatic variation, advancing with earlier snowmelt timi

287 y is less sensitive than flower phenology to climatic variation, indicating potential for reduced syn

288 Climatic variations are the major drivers to the IAV of

289 any relationship between biotic changes and climatic warming since the industrial revolution.

290 Our understanding of how projected climatic warming will influence the world's biota remain

291 may have been restricted to brief periods of climatic warming within the LGM, but chronological infor

292 , we analyzed how NDVI was influenced by the climatic water balance (i.e. Standardized Precipitation-

293 However, given the importance of climatic water balance on SIC accumulation, we tested th

294 as enormous variation among years related to climatic water balance.

295 Earth's biota and associated systems: annual climatic water deficit, annual evapotranspiration, avera

296 mixed), soil texture (sand, loam, clay), and climatic zone (arid, semiarid, dry subhumid) were nuance

297 ls in 143 individual soil samples covering 3 climatic zones and 5 different soil types.

298 oned wetland numbers equally between the two climatic zones and between the continents.

299 picting contrasting adaptations to different climatic zones.

300 hose shape and looping direction vary across climatic zones.