ライフサイエンスコーパス: greenhouse gas

1 ltivation is a major source of this powerful greenhouse gas.

2 e of nitrous oxide (N2O) emissions, a potent greenhouse gas.

3 reutilization of this environmental harmful greenhouse gas.

4 ides a new high yield route to mitigate this greenhouse gas.

5 and activating an important fuel and potent greenhouse gas.

6 ource of atmospheric methane (CH4), a potent greenhouse gas.

7 to tropospheric ozone, an air pollutant and greenhouse gas.

8 te to biosphere cycling of methane, a potent greenhouse gas.

9 of enhanced infra-red cooling by increasing greenhouse gases.

10 global ice volume and long-lived atmospheric greenhouse gases.

11 through emissions of substantial amounts of greenhouse gases.

12 ry and contribute directly and indirectly to greenhouse gases.

13 n the twenty-first century due to increasing greenhouse gases.

14 antifying the trade-offs between alternative greenhouse gas abatement options.

15 inear dependence on a wide range of isolated greenhouse gas, aerosol, and surface albedo forcings.

16 al radiative forcing impact of anthropogenic greenhouse gases after carbon dioxide, but our understan

17 Besides greenhouse gases, aircraft engines emit black carbon (BC

18 y produced a well-to-wheels (WTW) life cycle greenhouse gas analysis of petroleum-based fuels consume

19 limate as the second strongest anthropogenic greenhouse gas and air quality by influencing tropospher

20 lk supply on food miles, supply chain costs, greenhouse gas and criteria pollutant emissions, economi

21 ethane is the second strongest anthropogenic greenhouse gas and its atmospheric burden has more than

22 In this study, energy consumption, greenhouse gas and noxious emissions for five after-mark

23 Methane (CH4) is a powerful greenhouse gas and plays a key part in global atmospheri

24 shifts were largely driven by anthropogenic greenhouse gas and sulphate aerosol emissions.

25 Methane (CH4) is a potent greenhouse gas and the primary component of natural gas.

26 Concurrently, atmospheric concentrations of greenhouse gases and aerosols have increased due to anth

27 d and vented in the world annually, emitting greenhouse gases and other pollutants with no energy ben

28 ve characteristic effects on the exchange of greenhouse gases, and emphasize the need to project futu

29 induced climate forcings, such as increasing greenhouse gases, and other natural factors such as volc

30 he ocean and atmosphere, air-sea exchange of greenhouse gases, and production of climate-active marin

31 c: their use increases atmospheric levels of greenhouse gases, and their availability is geopolitical

32 ants in air-conditioning systems, are potent greenhouse gases, and their contribution to climate chan

33 om the supply side-through the mitigation of greenhouse gases-and from the demand side-through adapti

34 cently began to develop standard mixtures of greenhouse gases as part of a broad program mandated by

35 ethanotrophic bacteria use methane, a potent greenhouse gas, as their primary source of carbon and en

36 proaches to quantify the global net biogenic greenhouse gas balance between 1981 and 2010 resulting f

37 llenge to determine human impacts on the net greenhouse gas balance of wetlands at the global scale.

38 en studied extensively, but the net biogenic greenhouse gas balance resulting from anthropogenic acti

39 flux always increase the global atmospheric greenhouse gas burden.

40 ge by emitting the majority of anthropogenic greenhouse gases but also are particularly vulnerable to

41 Methane is an important greenhouse gas, but characterizing production by source

42 el is the best way to reduce the emission of greenhouse gases by the scientific community.

43 h resolution measurements of the three major greenhouse gases (carbon dioxide, methane, and nitrous o

44 restrial biosphere can release or absorb the greenhouse gases, carbon dioxide (CO2), methane (CH4) an

45 In addition to reducing greenhouse gases, climate action and policy must therefo

46 osynthesis (MES) of useful products from the greenhouse gas CO2.

47 r influence on the climate via the fluxes of greenhouse gases, CO2, CH4, and N2O.

48 cm, 37-77 cm, and 57-131 cm in 2100 for the greenhouse gas concentration scenarios RCP26, RCP45, and

49 limate models for years 2071-2100, using two greenhouse gas concentration trajectory scenarios each.

50 European economies following three different greenhouse-gas concentration trajectories, ranging from

51 Glacial-state greenhouse gas concentrations and Southern Hemisphere cl

52 response to the gradual rise in atmospheric greenhouse gas concentrations are notoriously difficult

53 rctic warming is expected to increase global greenhouse gas concentrations as permafrost thaw exposes

54 ics, sea-level fall and long-term decline in greenhouse gas concentrations during the late Eocene to

55 time, and global temperature and atmospheric greenhouse gas concentrations have been closely coupled

56 nd waters, thereby contributing to increased greenhouse gas concentrations in the atmosphere.

57 nd in African dust emission and transport as greenhouse gas concentrations increase over the twenty-f

58 potential effects of long-term increases in greenhouse gas concentrations on the ionospheric D-regio

59 re frequent in coming decades as atmospheric greenhouse gas concentrations rise, but the instrumental

60 Dissolved greenhouse gas concentrations were highly variable, but

61 , nonlinear shifts in response to changes in greenhouse gas concentrations, aerosol emissions, or lan

62 However, for Earth-like greenhouse gas concentrations, the variable forcing does

63 We identified distinct zones of elevated greenhouse gas concentrations.

64 al solar irradiance (TSI) and changes in the greenhouse gas content of the atmosphere.

65 Transport emissions of greenhouse gases contribute substantially to regional an

66 We show that short-lived greenhouse gases contribute to sea-level rise through th

67 Although greenhouse gas-driven warming increases potential intens

68 ene-Eocene Thermal Maximum-the largest known greenhouse-gas-driven global warming event of the Cenozo

69 ration is expected to intensify under higher greenhouse gas emission and associated climate change in

70 With the ongoing global effort to reduce greenhouse gas emission and dependence on oil, electrica

71 ential environmental impacts of ZLD, notably greenhouse gas emission and generation of solid waste, a

72 2O represents approximately 6% of the global greenhouse gas emission inventory and the most important

73 those ecosystems as sites for anthropogenic greenhouse gas emission offset projects (sometimes refer

74 sons for mandating independent monitoring of greenhouse gas emission reduction projects.

75 ons from five global circulation models, two greenhouse gas emission scenarios, and two cyanobacteria

76 rojections of total water cycle change under greenhouse gas emission scenarios.

77 al sea-level estimates and applied to future greenhouse gas emission scenarios.

78 dietary intakes, portion sizes, food prices, greenhouse gas emission, acidification and marine eutrop

79 However, the magnitude of greenhouse gases emission derived by application of manu

80 tly considered when setting fuel economy and greenhouse-gas emission standards for passenger cars and

81 d national governmental agreements to reduce greenhouse gas emissions (e.g., the 2015 Paris Agreement

82 identifies a considerable amount of indirect greenhouse gas emissions (up to 58.4%) that are essentia

83 National greenhouse gas emissions accounting typically estimates

84 ns that increase carbon storage and/or avoid greenhouse gas emissions across global forests, wetlands

85 Other indicators such as greenhouse gas emissions also improve, but adequate nitr

86 synthesis is an attractive means of reducing greenhouse gas emissions and a possible stepping-stone t

87 l play a critical role in mitigating current greenhouse gas emissions and facilitating conversion to

88 s, chemicals, and materials aims at reducing greenhouse gas emissions and fossil resource use.

89 ould also simultaneously reduce diet-related greenhouse gas emissions and improve diet-related health

90 bution pipelines is important for minimizing greenhouse gas emissions and optimizing investment in pi

91 hemicals is a promising strategy to mitigate greenhouse gas emissions and simultaneously store solar

92 ntal Protection Agency (EPA) Inventory of US Greenhouse Gas Emissions and Sinks (GHGI) for 2012.

93 ere we analyze output for three scenarios of greenhouse gas emissions and socio-economic growth to es

94 esults opposite to those of standard LCA for greenhouse gas emissions and water consumption, and of d

95 Strong decreases in greenhouse gas emissions are required to meet the reduct

96 reement stipulates that targets for reducing greenhouse gas emissions are strengthened over time, bot

97 e modelled using life tables, and changes in greenhouse gas emissions associated with the production

98 r 50 metals and calculated the corresponding greenhouse gas emissions associated with the supply of l

99 l likely require that transportation-related greenhouse gas emissions begin to decline within the nex

100 e global mortality by 6-10% and food-related greenhouse gas emissions by 29-70% compared with a refer

101 fluids, as currently conceived, could reduce greenhouse gas emissions by 400% (with sequestration cre

102 The INDCs collectively lower greenhouse gas emissions compared to where current polic

103 one potential pathway to decreasing nations' greenhouse gas emissions could involve reducing dispropo

104 billion for RCP4.5, suggesting that reducing greenhouse gas emissions could lessen damages by $1.3 bi

105 bute to further design strategies to control greenhouse gas emissions from agricultural soils or wast

106 hemical solvents is one solution to mitigate greenhouse gas emissions from anthropogenic sources and

107 metal recycling have the potential to reduce greenhouse gas emissions from the metal industry by abou

108 Recent efforts to combat increasing greenhouse gas emissions include their capture into adva

109 y verified by comparison with the California Greenhouse Gas Emissions Measurement (CALGEM) grid-resol

110 rally positive, and can influence life-cycle greenhouse gas emissions of switchgrass ethanol.

111 ntial for significant energy savings and for greenhouse gas emissions reduction.

112 re stabilization target will require steeper greenhouse gas emissions reductions than previously calc

113 ce a substantial decline (-32%) under a high greenhouse gas emissions scenario.

114 will decrease by as much as 50% under a high greenhouse gas emissions scenario.

115 uites of regional climate/pollen models, two greenhouse gas emissions scenarios [Representative Conce

116 tweighting EVs is less effective in reducing greenhouse gas emissions than lightweighting ICEVs, howe

117 Motorised transport is a major cause of the greenhouse gas emissions that are threatening human heal

118 Greenhouse gas emissions were estimated using primary ac

119 climate agreement in Paris aims to mitigate greenhouse gas emissions while fostering sustainable dev

120 ption cause approximately one-third of total greenhouse gas emissions(1-3), and therefore delivering

121 oring high grazing) to global (mitigation of greenhouse gas emissions) interventions for the persiste

122 ld be able to contribute to the reduction of greenhouse gas emissions, ameliorate climate changes, pr

123 y contribute to global warming through their greenhouse gas emissions, and negatively through the acc

124 f climate change, including future landscape greenhouse gas emissions, and provide a means for assess

125 ferences and results for energy consumption, greenhouse gas emissions, and water consumption for 54 L

126 e-cycle assessment (LCA) is used to quantify greenhouse gas emissions, fossil energy demand, and crit

127 In the absence of strong reductions in greenhouse gas emissions, future greenhouse gas forcing

128 ffect of current INDCs on reducing aggregate greenhouse gas emissions, its implications for achieving

129 ace temperature, a consequence of increasing greenhouse gas emissions, progressively raises the modal

130 es are stabilized through the phasing out of greenhouse gas emissions, sea level is still expected to

131 l effects on health, energy consumption, and greenhouse gas emissions, their implications for water c

132 While this has benefits in reducing greenhouse gas emissions, there may be costs to biodiver

133 hange, determined by varying trajectories of greenhouse gas emissions, using five general circulation

134 energy/fuel use, ultimately leading to lower greenhouse gas emissions, while antiwear properties can

135 rating theatres are an appreciable source of greenhouse gas emissions.

136 ergy consumption were the largest sources of greenhouse gas emissions.

137 g metrics of environmental impact, including greenhouse gas emissions.

138 environmental impacts, including significant greenhouse gas emissions.

139 role in regulating global changes caused by greenhouse gas emissions.

140 for other well-established human drivers of greenhouse gas emissions.

141 al area and associated biodiversity loss and greenhouse gas emissions.

142 ant livestock is one of the major sources of greenhouse gas emissions.

143 corresponding to 1% of global anthropogenic greenhouse gas emissions.

144 pect of soils is their potential to mitigate greenhouse gas emissions.

145 ry changes were accompanied by reductions in greenhouse gas emissions.

146 they can increase fuel efficiency and reduce greenhouse gas emissions.

147 he year 2100 that were exacerbated by rising greenhouse gas emissions.

148 sed to predict agricultural productivity and greenhouse gas emissions.

149 supply security and to significantly reduce greenhouse gas emissions.

150 der impact on soil nutrient availability and greenhouse gas emissions.

151 health-care services generates considerable greenhouse gas emissions.

152 ical, but poorly recognized role in regional greenhouse gas emissions.

153 ed to adapt to a changing climate and reduce greenhouse gas emissions.

154 tial energy savings, and global reduction in greenhouse gas emissions.

155 by carbon sequestration, reducing soil-borne greenhouse-gas emissions and increasing soil nutrient re

156 Here inspired by the negotiations for greenhouse-gas emissions reductions, we experimentally s

157 nificantly improve local air quality, reduce greenhouse-gas emissions, and decrease the energy depend

158 rice cropping systems, particularly on their greenhouse gas emitting potential.

159 ugh understanding of the conditions favoring greenhouse gas(es) reductions is essential to achieving

160 e reconstruction with radiative forcing from greenhouse gases estimates an Earth system sensitivity o

161 Site greenhouse gas evaluations were done between Jan 1 and D

162 management have altered terrestrial biogenic greenhouse gas fluxes, and the resulting increases in me

163 ductions in greenhouse gas emissions, future greenhouse gas forcing of potential intensity will incre

164 reases likely exert a positive net radiative greenhouse gas forcing through the 21st century.

165 ctical aspects of the flux quantification of greenhouse gases from local point sources by using in si

166 lved factor in the flux of methane, a potent greenhouse gas, from the ocean.

167 ore, such emissions were omitted from IPCC's greenhouse gas (GHG) accounting procedures.

168 ed; contributing ~1/4 of total anthropogenic greenhouse gas (GHG) burden in 2010.

169 ntually reduce life cycle energy, water, and greenhouse gas (GHG) burdens associated with fracturing.

170 climate is stabilised at current atmospheric greenhouse gas (GHG) concentrations, those warming targe

171 te Average Fuel Economy (CAFE) standards and Greenhouse Gas (GHG) Emission standards are designed to

172 rature analyzing the fuel saving, life cycle greenhouse gas (GHG) emission, and ownership cost impact

173 s a critical avenue in the attempt to reduce greenhouse gas (GHG) emissions and any significant effor

174 ms can increase carbon sequestration, offset greenhouse gas (GHG) emissions and reduce the carbon foo

175 emissions model (COPTEM) that calculates the greenhouse gas (GHG) emissions associated with pipeline

176 ere is growing interest in understanding the greenhouse gas (GHG) emissions associated with the devel

177 ify these losses in relation to land use and greenhouse gas (GHG) emissions associated with the produ

178 ies export much of the harm created by their greenhouse gas (GHG) emissions because the Earth's atmos

179 BAU, OPT gives 16% and 36% reductions in LDV greenhouse gas (GHG) emissions for 2030 and 2050, respec

180 This research evaluates energy use and greenhouse gas (GHG) emissions for three scenarios (synt

181 builds a framework to estimate the lifecycle greenhouse gas (GHG) emissions from China's shale gas sy

182 Modeling efforts focused on future greenhouse gas (GHG) emissions from energy and other sec

183 Over the 21(st) century, greenhouse gas (GHG) emissions from freight are projecte

184 teract the increasing food demand and reduce greenhouse gas (GHG) emissions from the agricultural sec

185 dual fuel HGVs have the potential to reduce greenhouse gas (GHG) emissions from the freight sector.

186 Life cycle greenhouse gas (GHG) emissions from the production of nu

187 espite 20 years of effort to curb emissions, greenhouse gas (GHG) emissions grew faster during the 20

188 The contribution of ruminant livestock to greenhouse gas (GHG) emissions has been investigated ext

189 ontributes considerably to ammonia (NH3) and greenhouse gas (GHG) emissions in Europe.

190 100 countries pledged to reduce agricultural greenhouse gas (GHG) emissions in the 2015 Paris Agreeme

191 We estimate average greenhouse gas (GHG) emissions of 419 and 510 tonne of e

192 l), which evaluates the energy intensity and greenhouse gas (GHG) emissions of current oil sands upgr

193 Accounting for greenhouse gas (GHG) emissions of nations is essential t

194 ntly affects technology mixes and associated greenhouse gas (GHG) emissions of the system under study

195 Life-cycle greenhouse gas (GHG) emissions per kWh electricity produ

196 s to compare modeled emissions using several greenhouse gas (GHG) emissions reporting protocols inclu

197 onditions and uses more water and has higher greenhouse gas (GHG) emissions than most crops.

198 im that these products have lower life cycle greenhouse gas (GHG) emissions than their fossil counter

199 he major contributor to energy intensity and greenhouse gas (GHG) emissions was the production of sul

200 ges may alter the magnitude and direction of greenhouse gas (GHG) emissions, affecting the climate im

201 s require on average only 10% of land, 4% of greenhouse gas (GHG) emissions, and 6% of reactive nitro

202 ts on soil organic carbon (SOC) stocks, soil greenhouse gas (GHG) emissions, and global warming poten

203 As a major contributor to agricultural greenhouse gas (GHG) emissions, it has been suggested th

204 ewable biobased feedstocks, thereby reducing greenhouse gas (GHG) emissions, toxic byproducts, and th

205 (C) and nitrogen (N) cycles and influencing greenhouse gas (GHG) emissions.

206 market and, as such, an important source of greenhouse gas (GHG) emissions.

207 fied natural gas (LNG) exports affect global greenhouse gas (GHG) emissions.

208 Wetlands can influence global climate via greenhouse gas (GHG) exchange of carbon dioxide (CO2 ),

209 ts carbon (C) and N cycling, soil:atmosphere greenhouse gas (GHG) exchange, and functional microbial

210 Greenhouse Gas (GHG) footprints are thus a highly releva

211 an integrated analysis of the variability of greenhouse gas (GHG) footprints of field-grown tomatoes

212 has a profound impact on global atmospheric greenhouse gas (GHG) levels, and yet, strikingly little

213 r environmental impacts as a function of net greenhouse gas (GHG) mitigation: To achieve the same 73%

214 cofired combustion of biomass promise direct greenhouse gas (GHG) reductions for existing coal-fired

215 to analyze the in- and trans-boundary water, greenhouse gas (GHG), and land impacts of city-scale foo

216 Methane is the second most abundant greenhouse gas (GHG), with nearly 60% of emissions deriv

217 The reliability of model projections of greenhouse gas (GHG)-induced future climate change is of

218 hways of emissions scenarios, with different greenhouse gas (GHG)/aerosol forcing ratio and GHG level

219 en deposition (Ndep) can strongly affect the greenhouse gas (GHG; CO2, CH4, and N2O) sink capacity of

220 Greenhouse Gases (GHG) and Land Use (LU) are the major f

221 ment systems may have higher unit energy and greenhouse-gas (GHG) emissions.

222 ission abatement is stable across a range of greenhouse-gas (GHG) tax levels, while resulting food pr

223 Greenhouse gases (GHGs) emissions from streams are impor

224 The paleoclimatic sensitivity to atmospheric greenhouse gases (GHGs) has recently been suggested to b

225 Methane and nitrous oxide are potent greenhouse gases (GHGs) that contribute to climate chang

226 us oxide (N2 O) are the three most important greenhouse gases (GHGs), and all show large uncertaintie

227 We focus on greenhouse gases (GHGs), eutrophication, and land use be

228 one of the largest anthropogenic sources of greenhouse gases (GHGs), with dairy and beef production

229 le conditions for production and emission of greenhouse gases (GHGs).

230 ation enhances linearly with the global mean greenhouse gases(GHGs) radiative forcing and is attribut

231 he terrestrial biogenic fluxes of individual greenhouse gases have been studied extensively, but the

232 Demand for tools to rapidly assess greenhouse gas impacts from policy and technological cha

233 missions into the atmosphere by burying this greenhouse gas in the subsurface.

234 in the flux rates and production pathways of greenhouse gases in these dynamic systems.

235 Greenhouse gas intensity for the annual crops (flux per

236 to form a synthesis gas, converts two major greenhouse gases into a useful chemical feedstock.

237 Independent verification of national greenhouse gas inventories is a vital measure for cross-

238 tes required for compiling accurate national greenhouse gas inventories.

239 on the US Environmental Protection Agency's Greenhouse Gas Inventory and correspond to 1.5% of natur

240 ts such as the United States (U.S.) National Greenhouse Gas Inventory, and regional, state, local, an

241 ot recognized in any regulatory framework or greenhouse gas inventory.

242 ice cover, continued increase in atmospheric greenhouse gases is likely to result in warming and dryi

243 The utilization of methane, a potent greenhouse gas, is an important component of local and g

244 oduction costs of 2.23 euro/L and life cycle greenhouse gas (LC GHG) emissions of 0.49 kgCO2-equiv/L

245 esult suggests that stabilization at today's greenhouse gas levels may already commit Earth to an eve

246 absorbed and metabolized by the animals, the greenhouse gas methane escapes via eructation and breath

247 rates through biological means; however, the greenhouse gas methane has not been used with much succe

248 ble production and consumption of the potent greenhouse gas methane.

249 of volatile organic compounds, including the greenhouse gas methane.

250 d are significant sources of the atmospheric greenhouse gases methane (CH4) and carbon dioxide (CO2).

251 ices exist, the implementation of soil-based greenhouse gas mitigation activities are at an early sta

252 put regardless of crop yield on agricultural greenhouse gas mitigation and accounting.

253 This study paired stormwater and greenhouse gas monitoring with microbial analyses to elu

254 not release detectable amounts of the strong greenhouse gas N2 O.

255 nimum zones are strong sources of the potent greenhouse gas N2O but its microbial source is unclear.

256 n of ammonia and the reduction of the potent greenhouse gas, N2O, to inert N2, respectively.

257 have been reported as sources of the potent greenhouse gas nitrous oxide ([Formula: see text]) to th

258 tes significantly to emissions of the potent greenhouse gas nitrous oxide (N2 O), which is generated

259 The greenhouse gas nitrous oxide (N2O) is considered an inte

260 croorganisms with the capacity to reduce the greenhouse gas nitrous oxide (N2O) to harmless dinitroge

261 cation represent major sources of the potent greenhouse gas nitrous oxide (N2O).

262 potentially acting as a global sink for the greenhouse gas nitrous oxide.

263 hat is a major source and sink of the potent greenhouse gas nitrous oxide.

264 ification - a potential source of the potent greenhouse gas, nitrous oxide (N2 O) - and denitrificati

265 are reasonable when compared with satellite (Greenhouse gases Observing SATellite; GOSAT) and in situ

266 net positive cumulative impact of the three greenhouse gases on the planetary energy budget, with a

267 oxic to humans, plants, and animals and is a greenhouse gas, our findings call for adequate updating

268 otential for a broader inclusion of soils in greenhouse gas policies.

269 ical controls on emissions of this important greenhouse gas preclude prediction of when and where N2O

270 xide (N2 O) is a potent, globally important, greenhouse gas, predominantly released from agricultural

271 Nitrous oxide (N2O) is an important greenhouse gas produced in soil and aquatic ecosystems.

272 biofilters remained aerobic with negligible greenhouse gas production during storm events.

273 aterial, can alter the form and magnitude of greenhouse gas production from permafrost ecosystems.

274 ere carbon (C) cycle, and therefore prevents greenhouse gas production in natural systems.

275 processes can be accompanied by undesirable greenhouse gas production.

276 sions factors, and reported according to the Greenhouse Gas Protocol.

277 in for 2008 and under a compact urban growth greenhouse gas reduction scenario for 2035.

278 Greenhouse gas reduction strategies developed to mitigat

279 potential pathway to mitigate the effects of greenhouse gas release.

280 We attempt to quantify the source of greenhouse gases released during the Paleocene-Eocene tr

281 C); (2) U.S. Environmental Protection Agency Greenhouse Gas Reporting Program (EPA GHGRP); (3) Califo

282 by the Environmental Protection Agency (EPA) Greenhouse Gas Reporting Program (GHGRP).

283 ources Board (CARB) through their respective greenhouse gas reporting programs.

284 Here we highlight 'state of the art' soil greenhouse gas research, summarize mitigation practices

285 that under RCP8.5, a high business-as-usual greenhouse gas scenario, increasing temperatures may alt

286 e to formic acid offers a promising route to greenhouse gas sequestration, carbon abatement technolog

287 ge increase of atmospheric concentrations of greenhouse gases such as CO2 could also destroy the habi

288 Nitrous oxide (N2O) is a potent greenhouse gas that is produced during microbial nitroge

289 carbon source and quantities of CO2 and CH4 greenhouse gases that contributed to global warming are

290 ients, and global-warming potential (GWP) of greenhouse gases (the sum of CH4, CO2, and N2O in CO2 eq

291 esults in some of the highest fluxes of this greenhouse gas to the atmosphere ever reported.

292 for controlling the emission of this potent greenhouse gas to the atmosphere.

293 iments and led to the release of large-scale greenhouse gases to drive the end-Permian extinction.

294 Estuaries are an important source of greenhouse gases to the atmosphere, but uncertainties re

295 lly breaks down will release large pulses of greenhouse gases to the atmosphere.

296 metamorphism, likely liberating the massive greenhouse gas volumes needed to drive extinction.

297 Climate modeling studies indicate that greenhouse gases will force SAM into its positive phase

298 As CH4 is a powerful greenhouse gas with 34 times the warming potential of CO

299 Nitrous oxide (N2 O) is a powerful greenhouse gas with ozone depletion potential.

300 Mitigation of anthropogenic greenhouse gases with short lifetimes (order of a year t