ライフサイエンスコーパス: global warming

1 s is crucial to determining vulnerability to global warming.

2 back-to-back mass bleaching events caused by global warming.

3 o improve risk assessment of toxicants under global warming.

4 a detectable change in extreme storms due to global warming.

5 most potent greenhouse gases contributing to global warming.

6 population adaptability and vulnerability to global warming.

7 a key component to understand the effects of global warming.

8 ations in shaping beliefs and feelings about global warming.

9 eive this risk, which will be exacerbated by global warming.

10 been widely used to assess tree responses to global warming.

11 pear at between approximately 2 and 2.5 K of global warming.

12 t of surface and sub-shelf melting caused by global warming.

13 pecies may influence invasion outcomes under global warming.

14 ritical in predicting ecosystem responses to global warming.

15 s that is 25% larger than in a world without global warming.

16 e compounds will have a negligible impact on global warming.

17 management of the GBR against the effects of global warming.

18 of China at 1.5 degrees C and 2.0 degrees C global warming.

19 l burning is required to limit the extent of global warming.

20 extreme coastal El Nino will increase under global warming.

21 understanding of how species will respond to global warming.

22 Antarctic Ice Sheet for different amounts of global warming.

23 rces could have significant implications for global warming.

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

25 ger, and unexpectedly more destructive under global warming.

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

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

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

29 9 to 2006, resulting in negative feedback to global warming.

30 reach the atmosphere and potentially amplify global warming.

31 d movement of SOC in reducing SOC loss under global warming.

32 an dictate the sensitivity of populations to global warming.

33 when precipitation changes are combined with global warming.

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

35 precipitation loss, tends to increase under global warming.

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

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

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

39 onsidered larval connectivity as affected by global warming.

40 as how internal variability may change with global warming.

41 ibution of mobile stenothermal species under global warming.

42 their loss would trigger strong (about 5 K) global warming.

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

44 ng impacts of chemicals on ecosystems facing global warming.

45 re, at least to some extent, attributable to global warming.

46 t attenuate increases in SOM decay caused by global warming.

47 he end-of-century declines under unmitigated global warming.

48 ortant climate regulation service that slows global warming.

49 not suffice to counter greenhouse-gas-driven global warming.

50 ergenicity of some plants and contributes to global warming.

51 The other reconstruction reveals global warming.

52 upply sustainable liquid fuels and alleviate global warming.

53 net access on the formation of beliefs about global warming.

54 ed to improve the resilience of this crop to global warming.

55 ered as a technological strategy to mitigate global warming.

56 igate the threats to alpine species posed by global warming.

57 context of globalization of N deposition and global warming.

58 to span a large range even at 2 degrees C of global warming (-196 +/- 117 PgC).

59 mangrove SOM decay is affected by predicted global warming (+4 degrees C), sea level changes (simula

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

61 results do not support the current view that global warming alone will lead to a loss in biodiversity

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

63 If global warming amplifies water deficit in drought-prone

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

65 e (N(2) O) emissions from soil contribute to global warming and are in turn substantially affected by

66 Global warming and changes in human land use, such as gr

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

68 With global warming and climate change, breeding crop plants

69 s and (photo)electrocatalysis, may alleviate global warming and energy crises by removing excess CO2

70 ant lessons for a planet facing catastrophic global warming and environmental change.

71 ation models, particularly in the context of global warming and increasing frequency of droughts.

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

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

74 nic CO(2) likely contributed to end-Triassic global warming and ocean acidification.

75 eir non-calcifying relatives under impending global warming and ocean acidification.

76 age of traditional systems, thereby reducing global warming and providing savings on energy costs.

77 highlights an important link between ongoing global warming and public health-one that could be exace

78 records were used to assess the influence of global warming and regional eutrophication, respectively

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

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

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

82 analysis and applying different GHG metrics (global warming and temperature potentials) and time hori

83 ned selective thermal emitter on alleviating global warming and temperature regulating an Earth-like

84 Due to the strong impact of soot on global warming and the aging process of soot particles i

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

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

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

88 uminants has contributed considerably to the global warming and understanding the genomic architectur

89 Global warming and urbanization have a significant impac

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

91 ver geological time, such as global cooling, global warming, and changes in ocean chemistry.

92 constitute a handicap to prevail under rapid global warming, and contribute to explaining local lizar

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

94 bute to eutrophication, reduced air quality, global warming, and odor nuisance.

95 organic carbon caused by volcanic degassing, global warming, and sea-level rise.

96 e are persistent efforts worldwide to combat global warming, and that also includes the commercial fr

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

98 thaw to CO(2) and CH(4) to directly amplify global warming, another part will enter the fluvial netw

99 n such extra tropical forcing mechanisms and global warming are likely to be influential in determini

100 a scenario framework that focuses on capping global warming at a specific maximum level with either t

101 oengineering may not be fail-safe to prevent global warming because CO(2) can directly affect cloud c

102 he degree to which systems thinking predicts global warming beliefs and attitudes (e.g., believing th

103 systems thinking may support the adoption of global warming beliefs and attitudes indirectly by helpi

104 gh systems thinking is positively related to global warming beliefs and attitudes, the relationships

105 tionship between an ecological worldview and global warming beliefs and attitudes.

106 lishment of global climate policies to limit global warming below 1.5-2 degrees C will avoid the exha

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

108 he Paris agreement targeting a limitation of global warming below 2 degrees C by 2100, and possibly b

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 ad consensus that blooms are increasing with global warming, but the impacts of other concomitant env

112 r regions such as the Arctic under sustained global warming, but with complex and not necessarily pre

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

114 To understand how global warming can be kept well below 2 degrees Celsius

115 However, global warming can disrupt connectivity by shortening po

116 The widespread evidence that global warming can increase species sensitivities to che

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

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

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

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

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

122 Global warming compels larger endothermic animals to ada

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

124 Global warming could disturb CA and increase the potenti

125 Increasing SST as a result of global warming could favour the recolonization of the so

126 an Ocean warming, another salient feature of global warming, could increase local rainfall and throug

127 ific consensus further leads to increases in global warming discussion.

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

129 Global warming due to anthropogenic factors can be ampli

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

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

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

133 o climate change and consider the effects of global warming, extreme weather, flooding and other cons

134 drogen and carbon monoxide mixture) from two global warming gases of carbon dioxide and methane via d

135 ractive effects between forest pathogens and global warming, globalization, and land-use changes may

136 cle assessment models to quantify life cycle global warming (GWP), eutrophication (EU) and acidificat

137 d that per capita GDP is lower today than if global warming had not occurred.

138 High ambient temperature attributable to global warming has a profound influence on plant growth

139 Global warming has advanced the timing of biological eve

140 To investigate whether global warming has affected the recent evolution of ineq

141 Global warming has been documented to threaten wild plan

142 The recent trend of global warming has exerted a disproportionately strong i

143 low-level moisture transport intensified by global warming has favored extreme rainfall across the s

144 Global warming has greatly altered winter snowfall patte

145 st represented in our dataset, suggests that global warming has not systematically affected morpholog

146 half century, there is ~90% likelihood that global warming has slowed that decrease.

147 Therefore, increasing iceberg fluxes due to global warming have the potential to increase marine pro

148 on coral reefs, both factors associated with global warming, have rarely been addressed.

149 mean surface air temperature data indicate a global warming hiatus between 1998 and 2012, while its i

150 heir roles in shaping climate trends and the global warming hiatus in the northern hemisphere.

151 urface warming slowdown (GSWS) or so-called "global warming hiatus" since the end of the 20(th) centu

152 n among highly mobile marine ectotherms in a global warming hotspot, few species are fully keeping pa

153 y about facts across different topics (e.g., global warming, immigration), formats (verbal vs. numeri

154 nerally had a larger effect on the estimated global warming impact than the choice of static versus d

155 minimize the total annual cost (TAC) and the global warming impacts (GW) and maximize the circularity

156 g potential (GWP) approaches to estimate the global warming impacts from municipal solid waste landfi

157 Ecological studies of global warming impacts have many constraints.

158 , the standard static approach to estimating global warming impacts may not accurately represent the

159 ing impacts may not accurately represent the global warming impacts of landfills.

160 DOC in the British Isles, to estimate future global warming impacts on THMs formation in DWTPs that u

161 uments increased herbivory during periods of global warming in the deep past.

162 We simulated global warming in the field and found that non-native sp

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

164 nmental factors-e.g., regional conflicts and global warming-increase large-scale migrations, posing e

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

166 While global warming increases the likelihood of hot extremes

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

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

169 Global warming is expected to exacerbate the duration an

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

171 beliefs and attitudes (e.g., believing that global warming is happening, that it is human-caused, et

172 s the scientific consensus that human-caused global warming is happening.

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

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

175 Global warming is having impacts across the Tree of Life

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

177 If global warming is kept below 2 degrees C, less than 2% o

178 provides strong evidence that anthropogenic global warming is not only unparalleled in terms of abso

179 Global warming is one of the greatest threats to the per

180 ere, the East Antarctic Ice Sheet (EAIS), to global warming is poorly understood.

181 Global warming is predicted to cause substantial habitat

182 ported during the past decade has shown that global warming is roughly proportional to the total amou

183 t countries will be significantly reduced if global warming is stabilized below 1.5 degrees C, and in

184 Global warming is thought to affect phytoplankton produc

185 Recent global warming is weakening the annual surface gradient

186 he lower atmosphere, Arctic amplification of global warming is weakening the meridional temperature g

187 cean warming, a consequence of anthropogenic global warming, is changing the global wave climate, mak

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

189 g the Parallel Ice Sheet Model(3-5), that at global warming levels around 2 degrees Celsius above pre

190 To keep global warming <1.5 degrees C as recommended by the Inte

191 While global warming may have contributed, natural influences

192 Our study illustrates how global warming may radically modify the biogeography of

193 d future risk assessment of pesticides under global warming, mechanistic insights and consideration o

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

195 Global warming mitigation efforts reduce the impact on h

196 Global warming mitigation strategies are likely to affec

197 Here we show that both a global warming mode and a cooling mode emerge when perfo

198 .73, 0.71, and 0.87, respectively, while the global warming model had a lower R(2) of 0.48.

199 Due to the global warming, more and more often the red-pink grape v

200 d to probabilistically estimate the level of global warming needed for a September ice-free Arctic, u

201 vaccination, and responses to messages about global warming, nuclear proliferation, and natural disas

202 tors of global heatwave risk associated with global warming of 1.5 and 2 degrees C, specified by the

203 expand on the recent IPCC Special Report on global warming of 1.5 degrees C and review the additiona

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

205 Here, we explore the potential impact of global warming on ectotherm ageing through its effects o

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

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

208 ins unknown whether the long-term impacts of global warming on metabolic rates of phytoplankton can b

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

210 e forests and review the expected impacts of global warming on the profiled mechanisms.

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

212 amounts of carbon dioxide, thus limiting the global warming otherwise expected from postextinction vo

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

214 ighlights the clear need to mitigate against global warming, oversimplification of global change effe

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

216 of using 100 yr and 20 yr static and dynamic global warming potential (GWP) approaches to estimate th

217 by 21% while reducing irrigation by 19% and global warming potential (GWP) by 28%.

218 cost of electricity (LCOE) by 12-41% and the global warming potential (GWP) by 7-77%.

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

220 The global warming potential (GWP) is assessed in relation t

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

222 el is extended to estimate the corresponding global warming potential (GWP) over an analysis period o

223 Net global warming potential (GWP) was calculated.

224 Methane (CH(4)), a potent gas with a global warming potential 86-125x that of carbon dioxide

225 e, recycling, and efficiency, the life cycle global warming potential for LFP ranges from 185 to 440

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

227 zone's GHG emissions had a reduced sustained global warming potential of 264 g m(-2) yr(-1) CO(2)-e o

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

229 The high global warming potential of current refrigerants in cool

230 The fertilizer nitrogen loss and global warming potential of optimal nitrogen rate reduce

231 The 100-year global warming potential of the + C treatment was 6.2% l

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

233 environmental concern because of their large global warming potential(2).

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

235 a over mangrove lifetime (100 year sustained global warming potential).

236 orms the soil amendment scenario in terms of global warming potential, acidification, and eutrophicat

237 most impact categories (e.g., acidification, global warming potential, and carcinogenics).

238 ration profile for accurate estimates of the global warming potential, as well as the utility of a WM

239 per year), and (2) a 3% net decrease in the global warming potential-weighted emission factor (-27 g

240 e they do not require refrigerants with high global warming potential.

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

242 e fertilizer-derived N(2)O emissions and net global warming potential.

243 en concluded that with 100-year time horizon global warming potentials (GWP(100)) equivalent to <0.21

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

245 y, based on the corresponding sustained-flux global warming potentials.

246 is expected to have expanding impacts under global warming predictions.

247 imed to have positive effects for mitigating global warming, preventing soil erosion, and reducing bi

248 r results suggest a possible replacement, as global warming proceeds, of cool-adapted by warm-adapted

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

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

251 Concerns about the effects of global warming provide a strong case to consider how bes

252 consumption and the threatening situation of global warming related to burning fossil fuels.

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

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

255 en conducting acute temperature exposures in global warming research.

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

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

258 increasing surface buoyancy in 21st-century global warming scenarios.

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

260 Although the rapid global warming seen in observations over the past 150 ye

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

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

263 global mean values also explain 98.7% of the global warming spread (GWS).

264 Earth system models (ESMs) project that global warming suppresses biological productivity in the

265 However, with temperature increase due to global warming, temperature cue thresholds are experienc

266 al the Antarctic ozone hole and avoided more global warming than any other treaty.

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

268 efore, as thermal fluctuations escalate with global warming, the feminization of TSD turtle populatio

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

270 Nevertheless, a major component of global warming, the predicted increase in daily temperat

271 Waves (HWs) are expected to increase due to global warming, they are a regional phenomenon that dema

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

273 h applied to a 1.5 degrees C and 2 degrees C global warming threshold suggests self-preservation emis

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

275 ologies offer an important tool to limit the global warming to <2 degrees C.

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

277 ontribute ~10% of mitigation needed to limit global warming to 1.5 degrees C, carbon prices will need

278 rosol-perturbed rainfall patterns, and limit global warming to 2 degrees C.

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

280 The contribution of anthropogenic global warming to this prolonged rainfall deficit has pr

281 tems will be an essential component to limit global warming to well below 2 degrees C in the future.

282 power supply worldwide is required to limit global warming to well below 2 degrees C.

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

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

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

286 Soil degradation due to global warming, water scarcity and diminishing natural r

287 d ecosystem quality, mainly because of lower global warming, water scarcity, and metal contamination

288 To constrain global warming, we must strongly curtail greenhouse gas

289 for future environmental change all involve global warming, whether slow or fast.

290 rld is facing serious biodiversity loss with global warming, which are interconnected.

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

292 ions contribute to the greenhouse effect and global warming, which can lead to undesirable climate ch

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

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

295 gen availability, and body size predict that global warming will limit the aerobic scope of aquatic e

296 ut further increases in SST due to continued global warming will reduce this area by 9%.

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

298 That is, discussing global warming with friends and family leads people to l

299 Discussions of countering global warming with solar geoengineering assume that war

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