ライフサイエンスコーパス: global warming

1 ng impacts of chemicals on ecosystems facing global warming.

2 stems and species distributions arising from global warming.

3 energy budget and the magnitude of projected global warming.

4 l the vulnerability of aquatic ectotherms to global warming.

5 ger, and unexpectedly more destructive under global warming.

6 OM photomineralization to CO2 production and global warming.

7 cy of deadly heat under specified amounts of global warming.

8 tilapia represents a bellwether organism for global warming.

9 among other agricultural chemicals, and from global warming.

10 be substantial under some projected rates of global warming.

11 tter while dry areas getting drier under the global warming.

12 tropical Pacific as trade winds weaken with global warming.

13 ore inform on how coral reefs may respond to global warming.

14 tterns has intensified in response to recent global warming.

15 ly of the need to address climate change and global warming.

16 ential to determine if species will tolerate global warming.

17 mble those currently expected to result from global warming.

18 stion by-products, which also greatly affect global warming.

19 and atmospheric dust continue to respond to global warming.

20 Southern Oceans during the recent hiatus of global warming.

21 ial function may reduce soil C storage under global warming.

22 may become a prevalent problem in an era of global warming.

23 losses, and amplify the positive feedback to global warming.

24 the atmosphere is one of the main causes of global warming.

25 th speciation rates positively correlated to global warming.

26 ve frequently cited a "pause" or "hiatus" in global warming.

27 es of Caribbean reef rugosity in response to global warming.

28 all number of abrupt shifts and the level of global warming.

29 how a more favorable performance in terms of global warming.

30 ability to both acute and chronic effects of global warming.

31 layers should be of concern in a context of global warming.

32 valent length in the entire record of modern global warming.

33 , whose speed and direction may change under global warming.

34 d from lakes to the atmosphere, exacerbating global warming.

35 n recycling in the marine realm initiated by global warming.

36 d deprivation, which is being exacerbated by global warming.

37 ic are important, and may be contributing to global warming.

38 eed CO2-driven C gains, thereby accelerating global warming.

39 rtain to changing climate oscillations under global warming.

40 caused serious concern of the progression of global warming.

41 frequency and severity of changes related to global warming.

42 ial way to sustain rice production in future global warming.

43 limate change impacts at different levels of global warming.

44 osystems, and malaria at different levels of global warming.

45 rces could have significant implications for global warming.

46 dP/dTs) for both interannual variability and global warming.

47 9 to 2006, resulting in negative feedback to global warming.

48 reach the atmosphere and potentially amplify global warming.

49 an dictate the sensitivity of populations to global warming.

50 when precipitation changes are combined with global warming.

51 o CO2 in surface waters, thereby reinforcing global warming.

52 precipitation loss, tends to increase under global warming.

53 ent, anchovy, is uncertain in the context of global warming.

54 re more clearly linked to sea-level rise and global warming.

55 ebrates (CBVs) and thus directly impacted by global warming.

56 onsidered larval connectivity as affected by global warming.

57 the atmosphere that has led to the so-called global warming.

58 as how internal variability may change with global warming.

59 ibution of mobile stenothermal species under global warming.

60 icles will likely lead to a reduction in net global warming.

61 mpacts to be expected for moderate levels of global warming (+2 K).

62 ensity is widely projected to increase under global warming, a clear framework for predicting accumul

63 as amplified at close to CC following recent global warming, a result that was found to be at odds wi

64 greater means and narrower ranges of future global warming across the major radiative forcing scenar

65 Understanding and predicting how global warming affects the structure and functioning of

66 derive future drought severity given certain global warming amount under this scenario.

67 If global warming amplifies water deficit in drought-prone

68 d lead to the largest mitigation effects for global warming and abiotic depletion.

69 Global warming and AMOC-induced NH cooling are governed

70 was often close to 30 degrees C, due to the global warming and an early harvesting period.

71 mechanisms and for evaluating the effects of global warming and chemical pollution.

72 They contribute directly and indirectly to global warming and climate change and have a major effec

73 luenced by environmental conditions and thus global warming and climate change could affect CPP range

74 Predictions of how global warming and eutrophication will affect metabolic

75 nsights into understanding, for example, how global warming and habitat disturbance contribute to dis

76 e combustion of fossil fuels, which promotes global warming and has deleterious effects on our enviro

77 Global warming and increases in nutrient loadings are tw

78 he change of global-mean precipitation under global warming and interannual variability is predominan

79 pear more skeptical about climate change and global warming and less willing to act against it than l

80 to be more frequent and intense accompanying global warming and may have profound impacts on soil res

81 that biotic responses to both anthropogenic global warming and nitrogen pollution may be attenuated

82 f Calanus spp. is affected by end-of-century global warming and ocean acidification scenarios.

83 very via urine source separation reduced the global warming and ozone depletion potentials but increa

84 Global warming and predation risk can have important imp

85 mplementary insight into the consequences of global warming and predation risk for the physiology and

86 portance of mitigation policies for limiting global warming and reducing the associated health risks.

87 Due to ongoing global warming and rising temperatures, it is likely tha

88 st flooding events indicate that the ongoing global warming and sea-level rise will lead to significa

89 and CH4 into the atmosphere, causing severe global warming and subsequent mass extinction.

90 nct response of droughts of various types to global warming and the asymmetric impact of global warmi

91 ualties, under 1.5 degrees C and 2 degrees C global warming and their scenario dependence using three

92 ent, alongside other renewables, to mitigate global warming and to reduce fossil fuel dependency.

93 ges are part of a long-term process, such as global warming, and are not a response to any single epi

94 response of organized tropical convection to global warming, and challenges conventional projections

95 sectors contributing to oil consumption and global warming, and natural gas (NG) is considered to be

96 creased hygrometric capacity associated with global warming, and unchanged short-term atmospheric con

97 vel rise will keep increasing with continued global warming, and, even if temperatures are stabilized

98 and CH4 greenhouse gases that contributed to global warming are poorly constrained and highly debated

99 Global warming as a consequence of climate change, risin

100 mafrost soils could significantly exacerbate global warming as the active-layer deepens, exposing mor

101 170,000-y ( approximately 170-kyr) period of global warming associated with rapid and massive injecti

102 one of the clearest manifestations of recent global warming associated with rising greenhouse gas con

103 ossils and trace fossils) in response to the global warming associated with the last glacial to inter

104 ation may represent a fundamental pattern of global warming associated with water vapor feedbacks ove

105 l shift to the north under the background of global warming at magnitudes of 2-6 degrees C, indicatin

106 The 2015 Paris Agreement aims to limit global warming below 2 degrees C and pursue efforts to e

107 Restricting global warming below 2 degrees C to avoid catastrophic c

108 l on Climate Change scenario likely to limit global warming below 2 degrees C.

109 very large PV installations will not offset global warming, but could generate enough energy to nega

110 in boreal forests have been associated with global warming, but it is still uncertain whether the de

111 precipitation is projected to increase with global warming, but some areas will experience decreases

112 s are one of the most significant threats to global warming, but the extent to which these shifts kee

113 in the tropics and subtropics in response to global warming, but the physical mechanisms responsible

114 range of proposed methods for counteracting global warming by artificially reducing sunlight at Eart

115 However, global warming can disrupt connectivity by shortening po

116 s induced by, for example, eutrophication or global warming can induce major oxic-anoxic regime shift

117 However, current projections of future global warming caused by CO2 rise generally suggest the

118 Yet, burning coal produces more global warming CO2 relative to all other fossil fuels, a

119 ow carbon renewable natural gas and reducing global warming.Coalbeds produce natural gas, which has b

120 daily PM intake and field-measurement-based global warming commitment (GWC) for the Philips FDCS wer

121 As global warming continues, reef-building corals could avo

122 ocean stratification and near-surface winds, global warming contributes to an amplified surface clima

123 es coexistence, and through such mechanisms, global warming could, in some cases, increase the specie

124 detrimental to crop yields and could lead to global warming-driven reductions in agricultural product

125 Under the projected global warming due to the anthropogenic forcing, the pro

126 ide, and is responsible for about 20% of the global warming effect since pre-industrial times.

127 microorganisms could mitigate or facilitate global warming effects on soil organic matter (SOM) deco

128 A rapid carbon cycle perturbation and global warming event about 56 million years ago at the P

129 imum-the largest known greenhouse-gas-driven global warming event of the Cenozoic-is central to drawi

130 the impact of a well-constrained CO2-induced global warming event on the ecological functioning of do

131 laeocene-Eocene Thermal Maximum (PETM) was a global warming event that occurred about 56 million year

132 cooling due to a collapsing AMOC obliterates global warming for a period of 15-20 years.

133 he most important and negative effect of the global warming for winemakers in warm and sunny regions

134 n using ReCiPe2008, we observe a decrease of global warming, fossil depletion, acidification, ozone d

135 trate that this event was triggered by rapid global warming from anthropogenic plus natural forcing,

136 The recent slowdown in global warming has brought into question the reliability

137 Additionally, global warming has led to the thawing of ancient permafr

138 As global warming has lengthened the active seasons of many

139 How such cooling competes with global warming has long been a topic for speculation, bu

140 ost rapid decline occurred during the recent global warming hiatus period.

141 e, which contributes about 10% to the recent global warming hiatus since 1999.

142 1998, a phenomenon that has been dubbed the global warming "hiatus." Here, we present an updated glo

143 interannual dP/dTs all predict dP/dTs under global warming higher than the ensemble mean dP/dTs from

144 Abiotic depletion, global warming, human toxicity, ecotoxicity, photochemic

145 recovering CO2 leads to 19 and 11 times the global warming impact estimated from a market-based allo

146 The global warming impact ranged from approximately -350 to

147 e this large SOC stock vulnerable to loss by global warming in the 21st century and beyond.

148 pproximately the same range as predicted for global warming in the 21st century.

149 o impacts our understanding of the impact of global warming; in particular, the increase in temperatu

150 As rates of global warming increase rapidly, identifying species at

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

152 ill presumably become much more prevalent as global warming increases further by roughly 2-fold to 5-

153 The results indicate that global warming increases the likelihood of record-breaki

154 Global warming increases the moisture holding capacity o

155 The global warming indicates that the conductive thermal tra

156 egories, including cumulative energy demand, global warming (IPCC 2007), acidification (TRACI), human

157 Global warming is a nonlinear process, and temperature m

158 opical cyclone (TC) destructive potential to global warming is an open issue.

159 Anthropogenic global warming is driven by emissions of a wide variety

160 Global warming is expected to increase both atmospheric

161 beria is highly sensitive to climate change; global warming is expected to push the ecotone northward

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

163 entage of the population that believes that "global warming is happening." This effect is diminished

164 lux in the carbon cycle, yet its response to global warming is highly uncertain.

165 dominantly acts to reduce OLR, the resulting global warming is likely caused by enhanced ASR.

166 Global warming is likely to cause overall drying of land

167 Global warming is predicted to cause substantial habitat

168 ixed layer depth (MLD) in the North Pacific, global warming is robustly expected to decrease MLD.

169 Our findings provide evidence that global warming is strongly reshaping tropical plant dist

170 tions of biodiversity change associated with global warming is that ecological communities comprise b

171 Global warming is widely predicted to reduce the biomass

172 Climate change (global warming) is leading to an increase in heat extrem

173 ent deglaciation, the last major interval of global warming, is unclear due to uncertainties in the t

174 tions because of the limited DCC response to global warming, it may potentially increase the uncertai

175 Eighteen out of 37 events occur for global warming levels of less than 2 degrees , a thresho

176 Eutrophication and global warming make some aquatic ecosystems behave as bi

177 With increasing evidence of global warming, many cities have focused attention on re

178 If higher VPD levels driven by global warming materialize in conjunction with rising se

179 relatively little is known about how future global warming might alter their biodiversity and associ

180 gh their fossil record suggests that current global warming might promote long-term increases in croc

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

182 the development of projects contributing to global warming mitigation.

183 .73, 0.71, and 0.87, respectively, while the global warming model had a lower R(2) of 0.48.

184 Under global warming, new R d estimates amplify modelled respi

185 icular, the ensemble average projects that a global warming of 2 degrees C above present (approximate

186 The net contributions to global warming of the scenarios range from -1550 (saving

187 ents' views on other factors contributing to global warming; of these Land Use and Land Cover Change

188 global warming and the asymmetric impact of global warming on drought distribution resulting in a mu

189 t be able to properly forecast the impact of global warming on ecological processes and propose appro

190 Direct and indirect consequences of global warming on ecosystem functions and processes medi

191 cations to interpretation of the feedback of global warming on hydrological cycle over Asia and North

192 ts to understand the influence of historical global warming on individual extreme climate events have

193 The impact of global warming on insect-borne diseases and on highland

194 e initiation of wildfires, but the impact of global warming on lightning rates is poorly constrained.

195 the region, and rising seas associated with global warming on long timescales and exacerbated by shi

196 t stress and thus will exacerbate impacts of global warming on reefs.

197 orld, and been used to predict the effect of global warming on regional fish production.

198 Identifying the effects of global warming on regional water cycle extremes, such as

199 we quantify uncertainty in the influence of global warming on the severity and probability of the hi

200 Potential consequences of global warming on this system have been recognized for o

201 substantiating concerns about the impact of global warming on water quality.

202 s that the thawing of permafrost either from global warming or industrial exploitation of circumpolar

203 the interdecadal variability in the rate of global warming over the 20(th) century does not necessar

204 ve phase and a resumption of larger rates of global warming over the 2013-2022 period consistent with

205 e model realizations reveals that additional global warming over the next few decades is very likely

206 ls provide the principal means of projecting global warming over the remainder of the twenty-first ce

207 s and other environmental impacts, including global warming, ozone depletion, toxicity, and salinizat

208 the species is vulnerable to the effects of global warming, particularly on the Northeast U.S. Shelf

209 water-use efficiency was improved by 18-63%, global warming potential (GWP of CH4 and N2 O emissions)

210 ate the climate impact of GDI vehicles using global warming potential (GWP) and global temperature po

211 The 100-year Global Warming Potential (GWP) for (CF3)2CFCN was calcul

212 The global warming potential (GWP) for the projects to gener

213 ks, soil greenhouse gas (GHG) emissions, and global warming potential (GWP) in irrigated systems, how

214 Total global warming potential (GWP) of CH4 and N2O emissions

215 ssment of cumulative energy demand (CED) and global warming potential (GWP) of four stationary batter

216 esult, WTL and N deposition both reduced the global warming potential (GWP) of growing season GHG bud

217 could reduce total costs to $0.034 m(-3) and global warming potential (GWP) to 0.051 kg CO2 eq m(-3):

218 ad a strong, positive effect on C emissions; global warming potential (GWP) was >3x larger at 20 degr

219 ) is a potent greenhouse gas with a 100-year global warming potential approximately 300 times that of

220 of HFC-1447fz (ca. 8 days) implies that its global warming potential at a time horizon of 100 year i

221 es of CH4 -C:CO2 -C ratios lead to a greater global warming potential in the fast (step) warming trea

222 th Asia increased substantially, whereas the global warming potential intensity (GWPi) decreased.

223 introducing metric indicators to assess the global warming potential of biogenic CO2 (GWPbio).

224 4.8 (bottom up) based on the GWP100 metric (global warming potential on a 100-year time horizon).

225 impact on long-term soil organic carbon and global warming potential than uncertainty in model struc

226 We recorded a significantly higher net global warming potential under conventional tillage syst

227 Global warming potential was the most significant enviro

228 ironmental screens (critical temperature and global warming potential), we simulate performance in sm

229 orcing per unit of carbon input (the 20-year Global Warming Potential).

230 ested, feed contributed approximately 72% to global warming potential, 72% to acidification potential

231 letion and environmental concerns (including global warming potential, acidification potential, marin

232 lth impacts including human and ecotoxicity, global warming potential, ozone depletion, and acidifica

233 ve this stretch goal and BC's extremely high global warming potential, the short-term climate change

234 mate damage because methane (CH4) has a high global warming potential.

235 e the stratosphere ozone or have significant global warming potential.

236 of stratification on oxygen, nutrients, and global-warming potential (GWP) of greenhouse gases (the

237 all sectors under both 20 year and 100 year global warming potentials (GWP20 and GWP100).

238 siderably increased our understanding of the global warming potentials (GWPs) of multiple individual

239 heric lifetimes, radiative efficiencies, and global warming potentials for these short-lived MPHE iso

240 , and 56 g CO2e/mile with the 100 or 20 year Global Warming Potentials of BC and POC emissions, respe

241 on SOM mineralization, which may exacerbate global warming problems under future climate change.

242 rrent planning effort assumes that each K of global warming produces roughly the same regional climat

243 As global warming progresses, the need for species to compe

244 Since Chaney's report, the range of global warming projections in response to a doubling of

245 states may help to narrow down the range of global warming projections.

246 temperatures, predicting their impact under global warming remains a key challenge for ecological ri

247 Predicting species vulnerability to global warming requires a comprehensive, mechanistic und

248 ng the response of the hydrological cycle to global warming requires predicting not only how global m

249 f the El Nino-Southern Oscillation (ENSO) to global warming requires quantitative data on ENSO under

250 ty wood biochar had even larger benefits for global warming, respiratory effects, and noncarcinogenic

251 ronmental benefits in four categories (smog, global warming, respiratory effects, noncarcinogenics) l

252 To examine global warming's effect on soil organic carbon (SOC) dec

253 temperature in natural fish populations in a global warming scenario.

254 e supporting that soil N availability, under global warming scenarios, is expected to increase strong

255 compromise ecosystem processing depending on global warming scenarios; for example, reducing organism

256 We suggest that extreme CO2-induced global warming selected for taxa with high LMA associate

257 For a given global warming signal produced by a climate model ensemb

258 udinal bias in range shifts that indicates a global warming signal.

259 e show using observations and an ensemble of global warming simulations the combined impact of the El

260 The recent global warming slowdown or hiatus after the big El Nino

261 In the presence of global warming, such deep recirculation of seawater can

262 been impacted by thermal anomalies caused by global warming that induced coral bleaching and mortalit

263 redictability sources emerging during recent global warming, that is, the development of the central-

264 points to two concerns regarding adaption to global warming, the first being that adaptation will not

265 Considering their contribution to global warming, the sources and sinks of methane (CH4) s

266 Projected global warming threatens survival of sea turtles, and th

267 ocumented and urgent aspect of anthropogenic global warming, threatens population and assets located

268 es play a significant role in the context of global warming through emissions of substantial amounts

269 They positively contribute to global warming through their greenhouse gas emissions, a

270 To limit global warming to <2 degrees C we must reduce the net am

271 asibility and potential benefits of limiting global warming to 1.5 degrees C or 2 degrees C above pre

272 eeting discussed the possibility of limiting global warming to 2 degrees C since pre-industrial times

273 incommensurate with efforts to limit average global warming to 2 degrees C.

274 to rethink policies and strategies to combat global warming to at least some degree.

275 the international community pledged to limit global warming to below 2 degrees C above preindustrial

276 eported when the global climate shifted from global warming to global surface warming hiatus after 19

277 The Paris climate agreement aims at holding global warming to well below 2 degrees Celsius and to "p

278 Despite global warming, total Antarctic sea ice coverage increas

279 se in extreme precipitation under continuing global warming towards the IPCC's 1.5 degrees C target,

280 lines of Arabidopsis thaliana to a simulated global warming treatment in the field.

281 ase of Atlantic multidecadal oscillation and global warming trend has provided more favourable backgr

282 55 K/decade during 1860-2005 and follows the global warming trend.

283 With only 1.5 degrees C of global warming, twice as many megacities (such as Lagos,

284 Despite their potential to slow global warming, until recently, the radiative forcing as

285 Climate change, global warming, urban air pollution, energy supply uncer

286 r the net contribution of landfill mining to global warming using a novel, set-based modeling approac

287 ility on changes in ENSO under anthropogenic global warming using the Community Earth System Model (C

288 re the existing global policies on combating global warming via the carbon capture and storage (CCS)

289 any stressors, including toxic chemicals and global warming, which can impair, separately or in combi

290 e effect of TC size change in the context of global warming, which resulted in a significant underest

291 It is widely accepted that global warming will adversely affect ecological communit

292 With increasing evidence that global warming will alter the timing, magnitude and freq

293 The differing responses of taxa to global warming will cause spatial restructuring of the p

294 iotic interactions, the debate about whether global warming will increase or decrease disease transmi

295 ts, we can expect that ongoing and projected global warming will result in increasingly negative Tw-T

296 ifically, conceptual frameworks predict that global warming will severely threaten tropical ectotherm

297 especially CO2 in the atmosphere leading to global warming with undesirable climate changes has been

298 Global warming (with DeltaT approximately 10 K) of the E

299 logical cycle is expected to intensify under global warming, with studies reporting more frequent ext

300 s predict that the AMOC will slow down under global warming, with substantial impacts, but measuremen