ライフサイエンスコーパス: warm

1 ly after the perspiration to keep the wearer warm.

2 the potential genetic consequences of future warming.

3 d unexpectedly more destructive under global warming.

4 eadly heat under specified amounts of global warming.

5 and how die-off risk is affected by climate warming.

6 reported here is not caused by anthropogenic warming.

7 ng an elevational gradient following climate warming.

8 associated with changes in the rate of ocean warming.

9 rest ranges will extend upslope with climate warming.

10 cted continuation of atmospheric and oceanic warming.

11 rost timing that could stem from hemispheric warming.

12 mportant than anammox in response to climate warming.

13 sea urchins will likely decrease with future warming.

14 at may have contributed to accelerate Arctic warming.

15 en amplify the Arctic wintertime ice-surface warming.

16 vapor feedback, yielding a weaker (stronger) warming.

17 ext century as a result of predicted climate warming.

18 speed and direction may change under global warming.

19 essing the impacts of global 1.5/2 degrees C warming.

20 do feedback, and experience greater (weaker) warming.

21 methanogenesis to total CH4 production with warming.

22 lity to assess risks associated with climate warming.

23 t coincided with onset of the industrial-era warming.

24 s trend will continue in response to further warming.

25 ne of the clearest manifestations of climate warming.

26 deed the source of the carbon that drove the warming.

27 ic communities may change under future ocean warming.

28 rom 1994 to 2015, a period of marked climate warming.

29 n Lake Superior due to anthropogenic climate warming.

30 multiple anthropogenic stressors, including warming.

31 rophic collapse even with little atmospheric warming.

32 uld have significant implications for global warming.

33 ing how ecosystem-level processes respond to warming.

34 ystems will respond to increased burning and warming.

35 a much stronger effect on CO2 flux than Air warming.

36 early 2016 that sustained the extreme Arctic warming.

37 mplications for glacial response to Holocene warming.

38 lly acting as a positive feedback to climate warming.

39 ve if interacting taxa respond oppositely to warming.

40 osphere that has led to the so-called global warming.

41 variability well before recent anthropogenic warming.

42 Decade-duration surface soil warming (1-2 degrees C) had no effect on soil respiratio

43 CP 8.5) corresponding to the most pronounced warming (+1.4 to 4.8 degrees C) forecasted mean growth r

44 Stimulation of cumulative 6-year GPP by warming (29%, P = 0.02) and eCO2 (26%, P = 0.07) was pri

45 In addition, growth declines with warming above the temperature optima were driven by redu

46 obal change, the combined influence of ocean warming, acidification, and deoxygenation, poses a serio

47 d of a transient interval of severe climatic warming across the Toarcian Oceanic Anoxic Event or T-OA

48 e gaps between pathogens and their cold- and warm-adapted hosts should occur at relatively warm and c

49 ift in the relative composition of cold- vs. warm-adapted species in a local assemblage [the communit

50 espiration rates increase under experimental warming, although the long-term, multiyear dynamics of t

51 er and 4-5% lower early delivery risk during warm and cold season, respectively.

52 arm-adapted hosts should occur at relatively warm and cold temperatures, respectively.

53 s in humans during exercise brought about by warm and cool fluid ingestion.

54 Fir populations currently subjected to warm and dry conditions will be the most vulnerable in t

55 1045 References 1045 As temperatures warm and precipitation patterns shift as a result of cli

56 The ecophysiological model WARM and sensitivity analysis techniques were used to ev

57 s estimates and are consistent with an early warm and wet climate with active hydrologic cycling invo

58 We established experimentally warmed and nonwarmed common garden plots at Alexandra Fi

59 field experiment to assess the influence of warming and altered precipitation on the temporal stabil

60 ten close to 30 degrees C, due to the global warming and an early harvesting period.

61 sms and for evaluating the effects of global warming and chemical pollution.

62 ficiency, which could arise because of ocean warming and DSL shallowing.

63 (WAP), a region which has experienced rapid warming and ecosystem changes.

64 temperature profiles resulting in increased warming and freeze-thaw cycle (FTC) frequency pose great

65 We hypothesized that night warming and heavy cloudiness would reduce EVI in this mo

66 itivity and in exposure to projected thermal warming and hydrologic change.

67 taxa are relatively buffered from projected warming and hydrologic change.

68 nation of the hydrologic cycle's response to warming and its impacts.

69 luence carbon dynamics during early Holocene warming and late Holocene cooling?

70 ore frequent and intense accompanying global warming and may have profound impacts on soil respiratio

71 soil C input (+20%), but the interaction of warming and N deposition greatly increased the soil C in

72 Due to ongoing global warming and rising temperatures, it is likely that sever

73 4 into the atmosphere, causing severe global warming and subsequent mass extinction.

74 c EAIS response with continued anthropogenic warming and suggest that the EAIS contribution to future

75 Recent warming and summer precipitation has the potential to al

76 st linear relationship between the projected warming and the present-day warm bias enables us to empi

77 , under 1.5 degrees C and 2 degrees C global warming and their scenario dependence using three sets o

78 ongside other renewables, to mitigate global warming and to reduce fossil fuel dependency.

79 Warming and watering treatments each led to large increa

80 gistic interactions between contaminants and warming, and differences in sensitivity across species'

81 cted to precipitation reduction, atmospheric warming, and to both simultaneously.

82 We partitioned community changes into warm- and cold-associated assemblages and found that Eng

83 deglaciation and the Younger Dryas-Preboreal warming are comparable to those of the current anthropog

84 the predicted enriching effects from climate warming are not always realized.

85 ing the early-Holocene that were at least as warm as the present-day.

86 to heat stress, meaning that the same future warming as realized to date could trigger larger increas

87 ) might have been triggered by ongoing rapid warming, as the area is experiencing climatic conditions

88 Warming associated with global climate change is likely

89 Each species was warmed at the rate of 1 degrees C h(-1) and taken to the

90 lings growing in the B4Warmed (Boreal Forest Warming at an Ecotone in Danger) experiment.

91 dying effects of larval exposure to zinc and warming before, during, and after metamorphosis in Ischn

92 In particular, warming begins to negatively impact plant growth at cool

93 en the projected warming and the present-day warm bias enables us to empirically correct future tempe

94 K, resulting mainly from the removal of the warm bias.

95 nce genes in pathogenic bacteria that infect warm-blooded hosts.

96 Given the variation in EM host responses to warming, both within and between ecosystems, better unde

97 arge PV installations will not offset global warming, but could generate enough energy to negate the

98 this ecosystem will likely be exacerbated by warming, but this loss may be counteracted by the rise i

99 describe increases in growth associated with warming by 1 degrees C, with growth rates up to doubled

100 of proposed methods for counteracting global warming by artificially reducing sunlight at Earth's sur

101 Periods of abrupt warming can trigger persistent changes in the state of e

102 owever, current projections of future global warming caused by CO2 rise generally suggest the intensi

103 , as well as with sea-level-rise and surface warming, caused primarily by the deepening of the ocean'

104 marine environment, fish respond quickly to warming, causing community-wide reorganizations, which r

105 In the context of ongoing climatic warming, certain landscapes could be near a tipping poin

106 206.2+/-4.2 Ma) through deep weathering in a warm climate and subsequent partial mobilization of the

107 cts can alter trends in plant responses to a warming climate and that predictions for changes in plan

108 ially sensitive to climate change, because a warming climate is enhancing upslope species migration,

109 for assessing compounding flood hazards in a warming climate.

110 osol strongly absorbs solar radiation, which warms climate.

111 gest complex local environmental response to warm climates in Antarctica and have implications for gl

112 future projections different from these past warm climates?

113 Yet, burning coal produces more global warming CO2 relative to all other fossil fuels, and it i

114 tion of chromatic chips is always better for warm colors (yellows/reds) than cool colors (blues/green

115 PM intake and field-measurement-based global warming commitment (GWC) for the Philips FDCS were a fac

116 en shown to respond more rapidly to climatic warming compared to local summer surface air temperature

117 ly environmental variables: moist soils with warm conditions increase suitability while extreme high

118 cally and rapidly changed in response to the warming conditions occurring in 2014-2016, and could be

119 As thaw in Soil warming continued to increase linearly, ground surface s

120 tratification and near-surface winds, global warming contributes to an amplified surface climate resp

121 the magnitude of metabolic rate responses to warming could emerge depending on global patterns of tem

122 In the warm dense matter regime, experimental data are very sca

123 reased rainfall might enhance EVI, nighttime warming dominated the climate impacts and differentiated

124 ntal to crop yields and could lead to global warming-driven reductions in agricultural productivity.

125 the dependency of wintertime runoff on this warming effect in combination with the effect of urban d

126 end of the temperature spectrum than at the warm end.

127 he Arctic experienced an extremely anomalous warming event after an extraordinary increase in air tem

128 e-Eocene Thermal Maximum (PETM) was a global warming event that occurred about 56 million years ago,

129 ny dogfish with prey species was enhanced by warming, expanding their importance as predators in this

130 rent Biology paper [1], we describe an ocean warming experiment in which we manipulated the temperatu

131 we report results of a two-year whole-stream warming experiment that shifted invertebrate assemblage

132 ons across North America with growth chamber warming experiments, we show that growth and survival in

133 s implied that the positive C fluxes-climate warming feedback was modulated by the changing N and rai

134 ass increased significantly, particularly in warmed, fertilized plots that received additional winter

135 nditions NA species required 84% more spring warming for bud break, EU ones 49% and EA ones only 1%.

136 We theoretically explore consequences of warming for predator-prey dynamics, broadening previous

137 overall electricity consumption under future warming for the world's third-largest electricity market

138 ven potential reductions in PLD due to ocean warming, future marine reserve networks would require mo

139 larval duration (PLD) associated with ocean warming, given current socioeconomic constraints.

140 Cool and warm groups showed opposite associations with temperatur

141 y, all models had negative or no response to warm-growing season temperatures, while tree-ring data s

142 ng in moist acidic tundra, we show that Soil warming had a much stronger effect on CO2 flux than Air

143 Predicting how river ecosystems respond to warming has been hindered by a dearth of information abo

144 Rapid climate warming has resulted in shrub expansion, mainly of erect

145 distribution of these communities and ocean warming has the potential to cause major distributional

146 delayed winter storms associated with polar warming have led to later winter floods around the North

147 system and the simulated magnitude of future warming have the potential to inform projections.

148 d the effects of individual controls such as warming, herbivory, and other disturbances on changes in

149 f seagrass seedlings to adapt and survive to warming, highlighting the potential additive effects tha

150 Warming impairs juniper uptake of deep sources during ex

151 "Arctic amplification" - that is, amplified warming in Arctic regions due to sea-ice loss and other

152 ta from 7 years of experimental Air and Soil warming in moist acidic tundra, we show that Soil warmin

153 e early to mid-twentieth century, as well as warming in recent decades.

154 Med, and also that last interglacial surface warming in the eMed was strongly amplified by water-colu

155 crystalline phases were observed to form on warming in the experiment: Sn, Cs2Se3, Cs4Se16, Cs2Se5,

156 f limited shrub growth sensitivity to summer warming in the High Arctic.

157 Response to warming in the short-term can be either positive or nega

158 ydrogenotrophic methanogenesis but deep peat warming increased the delta(13) C of CH4 suggesting an i

159 Consequently, in a context of global warming, increased frequency of drifting icebergs in pol

160 The lower sensitivity of limber pine to warming indicates a potential for this species to become

161 c ventilation of deep reservoirs rather than warming-induced gas hydrate dissociation in this shallow

162 Climate warming-induced glacier and snow loss clearly imperils t

163 At night, UHI warming intensifies, occurring across a majority (90%) o

164 dex and the associated rate of human-induced warming is compatible with a range of other more sophist

165 ntly, immediate global action to curb future warming is essential to secure a future for coral reefs.

166 Rapid Arctic warming is expected to increase global greenhouse gas co

167 While continued climate warming is expected to increase the carrying capacity of

168 s highly sensitive to climate change; global warming is expected to push the ecotone northwards, at t

169 of county-level opinion about whether global warming is happening.

170 of the population that believes that "global warming is happening." This effect is diminished in area

171 Warming is predicted to alter the structure of natural c

172 n the absence of increasing aridity, climate warming is predicted to generally increase abundances an

173 Ocean surface warming is resulting in an expansion of stratified, low-

174 After 30 minutes of warm ischemia, right kidneys were removed from 30-kg Yor

175 The cold and warm ischemic times improved significantly during the se

176 ally relevant endpoints across a spectrum of warm ischemic times, before and during ex vivo heart per

177 to the rate of ocean warming rather than to warming itself.

178 st the total radiative forcing and resultant warming level, must be considered when assessing the imp

179 ected changes in climate extremes under both warming levels highly depend on the pathways of emission

180 age drives a reduction in yield, or seasonal warming losses, where raised temperature is thought to i

181 lowed by filtration before distribution in a warm, low water age system.

182 es not influence biomass temporal stability, warming lowers stability through reducing the degree of

183 elevation lakes, metabolic rate responses to warming may still be greater there even though metabolic

184 summer warming shows that recent and future warming might promote an expansion of this evergreen dwa

185 During the warm Miocene and Pliocene Epochs, vast subtropical regio

186 value, is an attractive strategy for global warming mitigation and resource utilization.

187 While climate warming occurs over a background of variation due to cyc

188 lso suggests that ice sheets in contact with warming oceans may be vulnerable to catastrophic collaps

189 methane seeps have appeared due to enhanced warming of Arctic Ocean bottom water during the last cen

190 Warming of matrices containing pure triplet p-tolyl(trif

191 t its breeding range revealed that an abrupt warming of sea-surface temperature in the 1990s coincide

192 ce of deep delta(18)Oc likely reflects early warming of the deep northern North Atlantic by approxima

193 ers in W and SE Greenland has been linked to warming of the subpolar North Atlantic.

194 Differential warming of tropical and temperate biomes could result in

195 will likely mediate impacts of anthropogenic warming on biodiversity and ecosystem function across al

196 e, we examine impacts of recurrent sublethal warming on development and survival in ecological projec

197 delling suggest limited impact of short-term warming on gas hydrates deeper than a few metres in the

198 The cumulative effects of climate warming on herbivore vital rates and population dynamics

199 nderstand the influence of historical global warming on individual extreme climate events have increa

200 gion, and rising seas associated with global warming on long timescales and exacerbated by shifts in

201 d may therefore buffer against the impact of warming on marine ecosystems, suggesting a novel mechani

202 nd been used to predict the effect of global warming on regional fish production.

203 To explore potential effects of warming on suppressing pests and controlling herbivory i

204 ntify uncertainty in the influence of global warming on the severity and probability of the historica

205 arable to those of the current anthropogenic warming, our measurements suggest that large future atmo

206 hetic physiology, but the response of GPP to warming over longer timescales could also be shaped by e

207 I estimate that warming over the last 30 y is responsible for 59,300 sui

208 pport the recent claim of a "leveling off of warming" over the past two decades.

209 s them the ability to breathe air to survive warm, oxygen-poor stagnant waters or overland excursion

210 residence times affecting humidification and warming performance at the anterior tract were found und

211 continuous spawning of adults throughout the warm period.

212 onal influence on surface water storage, the warm phase of ENSO preconditions the lower Mississippi R

213 e decomposition of labile SOC was similar in warmed plots compared to the control.

214 e CO2 respiration, was greater in soils from warmed plots.

215 ion between sublimating CO2 ice blocks and a warm, porous, mobile regolith can generate features simi

216 H4 -C:CO2 -C ratios lead to a greater global warming potential in the fast (step) warming treatment.

217 ucing metric indicators to assess the global warming potential of biogenic CO2 (GWPbio).

218 a powerful greenhouse gas with 34 times the warming potential of CO2 , it is critical to understand

219 O2) has the potential to offset the positive warming potential of emitted methane, a process that has

220 tal screens (critical temperature and global warming potential), we simulate performance in small air

221 h at more northerly latitudes as the climate warms, potentially leading to lags in northward range sh

222 well as solid samples decompose rapidly upon warming, producing N2.

223 As global warming progresses, the need for species to compensate o

224 r, we find that the observationally informed warming projection for the end of the twenty-first centu

225 n climate feedbacks as the sole cause of the warming projection spread (WPS).

226 Since Chaney's report, the range of global warming projections in response to a doubling of CO2-fro

227 However, if warming rates are sufficiently fast in higher latitude/e

228 ending on global patterns of temperature and warming rates.

229 t objects and show that objects tend to have warm rather than cool colors.

230 s may be more sensitive to the rate of ocean warming rather than to warming itself.

231 Contrary to expectations, warming reduced Engelmann spruce recruitment at and abov

232 Warming reduced limber pine first-year recruitment in th

233 Nighttime warming reinforced by spatially heterogeneous cloudiness

234 atures, predicting their impact under global warming remains a key challenge for ecological risk asse

235 ng thermal limits by investigating the acute warming response of six Antarctic marine invertebrates:

236 We found that soil warming results in a four-phase pattern of soil organic

237 measured before and after rapid infusion of warmed saline (15 mL kg(-1) , approximately 7 min).

238 To generate a realistic climatic warming scenario we used naturalistic outdoors mesocosms

239 and nutrient uptake responded to a realistic warming scenario.

240 for changes in plant phenology under future warming scenarios should incorporate such effects.

241 areas will be reduced 73-88% by 2050 across warming scenarios, a decline 46-76% greater than estimat

242 eat-polluted area indicate that under future warming scenarios, calcification in heat-tolerant forami

243 rting that soil N availability, under global warming scenarios, is expected to increase stronger in c

244 ation and should occur over a broad range of warming scenarios.

245 s that simulated contemporary conditions and warming scenarios.

246 source and seasonality and local changes in warm-season duration and rainstorm events related to the

247 f moisture and dynamic forcing conducive for warm-season severe weather over China.

248 Recent evidence shows that warm semi-arid ecosystems are playing a disproportionate

249 ubs in response to recent High Arctic summer warming shows that recent and future warming might promo

250 However, daytime, but not nighttime, warming significantly reduced community temporal stabili

251 The last phase coincided with rapid warming since 1985, and shows with 33 m per 1 degrees C,

252 We found that warming slightly increased the soil C input and loss by

253 Conversely, warm spells in winter with rainfall (rain-on-snow) can c

254 The warm SST anomaly further develops due to the SST-sea lev

255 The AMO warm SST anomaly generates an atmospheric teleconnection

256 nto the coupled model that enables anomalous warm SST in the central Pacific.

257 n rational arithmetic require a near-optimal warm start to be practical on large problems (current ME

258 ontrol site, they remained silent during the warming stimuli on the injected site.

259 ed changes in BOLD signal during the dynamic warming stimulus on the control site, they remained sile

260 In response to climate warming, subalpine treelines are expected to move up in

261 g potato cultivars able to grow under future warm summer conditions.

262 Warm summers as well as high seasonal variability in pre

263 igher plant productivity in the increasingly warm summers.

264 Under the 1.5 degrees C warming target as advocated in recent Paris agreement, s

265 ient temperature (22 degrees C), however, at warm temperature both species reduced herbivory with evi

266 (INPs) to induce ice formation at relatively warm temperatures in microfluidic devices.

267 In contrast, warm temperatures without FTCs could lead to divergent r

268 s repeatedly been found to be constrained by warm temperatures, so we used Niche Mapper, a mechanisti

269 l effects of increased disturbance activity, warming temperatures and increased moisture stress on pl

270 rical data to consider the linked effects of warming temperatures on hatchling output and on sex rati

271 icate that more stations exhibit cooling and warming than predicted by random chance and that spatial

272 hology and/or function aimed to humidify and warm the air before it reaches the lungs are of key impo

273 poration-SST effect, and in response to this warming, the surface winds converge towards the subtropi

274 anges induce a subtropical North Pacific SST warming through wind-evaporation-SST effect, and in resp

275 tundra plant show compensatory responses to warming throughout the species' latitudinal range, buffe

276 ernational community pledged to limit global warming to below 2 degrees C above preindustrial (PI) to

277 ed through 2030 for a >66% chance of holding warming to below 2 degrees C.

278 ors (e.g., land cover change and CO2-induced warming) to the 2016 drought.

279 Our nighttime warming treatment increased winter nighttime air tempera

280 global warming potential in the fast (step) warming treatment.

281 Three warming treatments were fully crossed with three drying

282 Tropospheric warming trends over recent 20-year periods are always si

283 s correlated with these springtime patterns: warm tropical Atlantic and cold northeast Pacific sea su

284 Western boundary currents bring warm tropical water poleward and eastward and are charac

285 g the relative importance of circulation and warming unclear.

286 red by lack of understanding of how rates of warming vary across a landscape.

287 Spatial variation in warming was caused primarily by a decrease in daytime cl

288 the well-known synergism between metals and warming was manifested not only during the larval stage

289 th the shortening of lead time between ocean warm water volume (WWV) variability along the equatorial

290 f deep waters and the surface circulation of warm waters around the subpolar gyre.

291 In fine warm weather, the daytime convective atmosphere over lan

292 to the transition in climate from an early, warm, wet environment to today's cold, dry atmosphere.

293 mal compound action potential gets larger on warming, whereas in the presence of bumetanide and amilo

294 tion tripled during the year of experimental warming, while whole-stream N and P uptake rates did not

295 Understanding how climate warming will affect the demographic rates of different e

296 umn (under relatively long photoperiods), so warming will likely delay cessation and extend the growi

297 Our results indicate that warming will negatively affect seagrass seedlings throug

298 ate the broader significance of the enhanced warming, with a retreat of the northern ice margin behin

299 highlight concerns for species with TSD in a warming world and underline the need for research to ext

300 Recently, concerns for species with TSD in a warming world have increased because imbalanced sex rati