ライフサイエンスコーパス: greenhouse gas

1 Methane (CH(4)) is a potent greenhouse gas.

2 atmosphere is a major source of this potent greenhouse gas.

3 s to produce nitrous oxide (N(2)O), a potent greenhouse gas.

4 y component of natural gas (NG), is a potent greenhouse gas.

5 emissions of nitrous oxide (N(2)O), a potent greenhouse gas.

6 to mitigating emissions of methane, a potent greenhouse gas.

7 trification, nitrous oxide, is a significant greenhouse gas.

8 Microbial activity mediates the fluxes of greenhouse gases.

9 Light-duty vehicles emit ~20% of net US greenhouse gases.

10 ditions, increasing emissions of aerosol and greenhouse gases.

11 able syngas and simultaneously mitigate both greenhouse gases.

12 missions and, often, accompanying removal of greenhouse gases.

13 eduction of soil fertility and production of greenhouse gases.

14 olume and high concentrations of atmospheric greenhouse gases.

15 ed organic matter (DOM) in surface waters to greenhouse gases.

16 arms in response to rising concentrations of greenhouse gases.

17 air pollution and an important anthropogenic greenhouse gas(1).

18 ing effect that results from the emission of greenhouse gases(1).

19 onse to increased anthropogenic emissions of greenhouse gases(11), and is projected to warm further.

20 a focus on the food sector-a major source of greenhouse gases [6].

21 lobal mean temperature(4,5) and forcing from greenhouse gases(6).

22 be measured by monitoring changing fluxes of greenhouse gases, adaptation is more complicated to meas

23 As a potent greenhouse gas and an ozone-depleting agent, nitrous oxi

24 obically treated effluent, which is a potent greenhouse gas and is easily stripped out in the aeratio

25 Methane is a powerful greenhouse gas and is targeted for emissions mitigation

26 Nitrous oxide (N(2)O) is a powerful greenhouse gas and ozone depleting substance, but its na

27 Controlling greenhouse gas and toxic/odorous emissions from composti

28 Anthropogenic greenhouse gases and aerosols are associated with climat

29 acial-interglacial variations in atmospheric greenhouse gases and Antarctic climate were reduced in t

30 ion of the emission trading system (ETS) for greenhouse gases and Euro-4 standards for new vehicles e

31 2009 Endangerment Finding for six well-mixed greenhouse gases and find that this new evidence lends i

32 ed and these processes emit large amounts of greenhouse gases and pollution.

33 ow the climate system responds to changes in greenhouse gases and the cryosphere.

34 source of nitrous oxide (N(2) O), a powerful greenhouse gas, and increasing SOC may influence N(2) O

35 Atmospheric methane (CH(4)) is a potent greenhouse gas, and its mole fraction has more than doub

36 steel sector emits 25% of global industrial greenhouse gases, and the U.S. is the world's second-lar

37 ouse gases in the atmosphere increase; (iii) greenhouse gases are a worldwide public bad with emissio

38 algae in BC cycling, and the degree to which greenhouse gases are released following disturbance of B

39 o emit large quantities of methane, a potent greenhouse gas, as the Earth continues to warm.

40 ust be evaluated in context of the full, net greenhouse gas balance.

41 t of their impacts on nitrogen leaching, net greenhouse gas balances (NGHGB) and crop productivity.

42 dditional effects of biochar applications on greenhouse gas balances.

43 The net greenhouse gas benefits of wind turbines compared to the

44 main a major source of uncertainty in global greenhouse gas budgets.

45 nge (including production and consumption of greenhouse gases) but also how they will be affected by

46 Methane (CH(4) ), a potent greenhouse gas, can form in the sediments of these ecosy

47 l fuels produces emissions of the long-lived greenhouse gas carbon dioxide and of short-lived polluta

48 o produce valuable fuels and chemicals using greenhouse gas carbon dioxide as the carbon feedstock.

49 around the dikes and sills releases 18 Gt of greenhouse gases (CH(4) and CO(2)).

50 As a redox-active greenhouse gas, CH(4) degrades water or emits to the atm

51 ectrosynthesis is presented to transform the greenhouse gas CO(2) into an unusually thin walled, smal

52 f renewable fuels from abundant water or the greenhouse gas CO(2) is a major step toward creating sus

53 nd the benefit of converting and cycling the greenhouse gas CO(2) on a large scale.

54 The photocatalytic conversion of the greenhouse gas CO(2) to chemical fuels such as hydrocarb

55 region by 2080-2099 for low, medium and high greenhouse gas concentration trajectories (Representativ

56 responding to low (RCP2.6) and high (RCP8.5) greenhouse gas concentration trajectories(6), predict ma

57 Unlike records of greenhouse gas concentrations and global temperature, in

58 esponse to astronomical forcing depending on greenhouse gas concentrations and polar ice sheet volume

59 eometries, global ice volume and atmospheric greenhouse gas concentrations are scarce.

60 g increases in chemodiversity could increase greenhouse gas concentrations in lake sediments by an av

61 skewed towards lower values (under very high greenhouse gas concentrations, the most likely value is

62 rs, which are plausibly forced by increasing greenhouse gas concentrations.

63 ineering assume that warming owing to rising greenhouse-gas concentrations can be compensated by arti

64 Despite the observed monotonic increase in greenhouse-gas concentrations, global mean temperature d

65 arth exerts a fundamental influence upon the greenhouse gas content of the atmosphere, and hence glob

66 natural gas, and also one of the most potent greenhouse gases contributing to global warming.

67 evaluate impacts of solar geoengineering and greenhouse gas-driven climate change on equal terms, we

68 ar geoengineering may not suffice to counter greenhouse-gas-driven global warming.

69 For greenhouse-gas-driven tropospheric warming, larger noise

70 nge with important implications for modeling greenhouse-gas dynamics of blue C ecosystems.

71 We calculated per capita food system greenhouse gas emission (GHGE) targets derived from the

72 antly reduce air pollution, thereby reducing greenhouse gas emission and improving air quality.

73 is is a promising method because of its zero greenhouse gas emission and its compatibility with all t

74 tion, soil physical-chemical parameters, and greenhouse gas emission are measured and the economic an

75 t low-grade heat recovery can help to reduce greenhouse gas emission as over 70% of primary energy in

76 nt step toward a comprehensive assessment of greenhouse gas emission by aquatic ecosystems.

77 ing it a convenient tool to better constrain greenhouse gas emission from freshwater ecosystems.

78 te measurements in detecting and quantifying greenhouse gas emission from unpredictable events.

79 Greenhouse gas emission intensities for ethanol vehicles

80 Life-cycle greenhouse gas emission reductions for CADO-derived hydr

81 ces, and consumption under moderate and high greenhouse gas emission scenarios.

82 rently exceeds forest gain, leading to a net greenhouse gas emission that exacerbates global climate

83 is a key technological approach to reducing greenhouse gas emission while we transition to carbon-fr

84 h system models considering their effects on greenhouse gas emission, biogeochemical processes, and b

85 A substantial portion of greenhouse gas emissions (GHGE) has been attributed to t

86 We estimate the impact on greenhouse gas emissions (GHGE) of shifting from the cur

87 tions affected income, energy efficiency and greenhouse gas emissions (GHGE).

88 d the energy return on investment (EROI) and greenhouse gas emissions (GHGs) by 20% and 16%, respecti

89 tical for comparing the monetized impacts of greenhouse gas emissions across technologies.

90 fficient, and effective solutions to cut net greenhouse gas emissions and adapt to climate change.

91 ain global warming, we must strongly curtail greenhouse gas emissions and capture excess atmospheric

92 s, world economies are seeking to reduce the greenhouse gas emissions and local air pollution from tr

93 terventions in Greater Mexico City to reduce greenhouse gas emissions and local pollution.

94 decades, but drought risks will be lower if greenhouse gas emissions are cut aggressively.

95 important seasonal process and shows spring greenhouse gas emissions are largely due to production f

96 y below 1.5 degrees C, drastic reductions of greenhouse gas emissions are mandatory but not sufficien

97 Countries generally agree that global greenhouse gas emissions are too high, but prefer other

98 onalized urban food systems by examining the greenhouse gas emissions associated with food transport.

99 ile reducing overall net costs by 26-65% and greenhouse gas emissions by 38-59%.

100 analysis determined the potential to reduce greenhouse gas emissions by 50 to 271% relative to petro

101 o adoption would further limit water use and greenhouse gas emissions by preventing sugarcane expansi

102 king a route to population collapse, if high greenhouse gas emissions continue.

103 ve no means to reconstruct the pacing of LIP greenhouse gas emissions for comparison with climate rec

104 ter use (-65%), nutrient loading (-34%), and greenhouse gas emissions from cultivation (-51%).

105 derestimate both carbon stocks and potential greenhouse gas emissions from land-use conversion.

106 , PRELIM provided results for energy use and greenhouse gas emissions from petroleum refineries with

107 e could mitigate environmental pollution and greenhouse gas emissions from the agricultural sector.

108 -based regulatory program designed to reduce greenhouse gas emissions from the electric power sector

109 del predicting the wind turbines' life cycle greenhouse gas emissions from turbine size.

110 d in the climate system due to anthropogenic greenhouse gas emissions has been taken up by the oceans

111 elihood of current Chinese policies reducing greenhouse gas emissions in accordance with China's Pari

112 Protection Agency maintains an inventory of greenhouse gas emissions in accordance with the Intergov

113 ing how such complex land use change affects greenhouse gas emissions is essential for modelling clim

114 to address global climate change induced by greenhouse gas emissions is increasing.

115 ineering, motivated by concern that reducing greenhouse gas emissions may be insufficient to avoid si

116 ience has outlined targets for reductions of greenhouse gas emissions necessary to provide a substant

117 tilizer value, 79 (45-113) TJ of energy, and greenhouse gas emissions of 6.8 (3.4-10.1) MMT CO(2) equ

118 picture of the consequences of anthropogenic greenhouse gas emissions on future sea-level rise and it

119 more realistic assessment of the life cycle greenhouse gas emissions outcomes, using a case study of

120 Our results indicate that greenhouse gas emissions over this 280-y period result i

121 elf seas could contribute towards a nation's greenhouse gas emissions reduction targets.

122 ied and largely associated with volcanogenic greenhouse gas emissions released by large igneous provi

123 Greenhouse gas emissions results vary from -566 gCO(2) e

124 Hg from thawing permafrost for low and high greenhouse gas emissions scenarios using a mechanistic m

125 ieving much greater reductions in life-cycle greenhouse gas emissions than corn starch ethanol.

126 role in determining the near-term allowable greenhouse gas emissions that will limit future warming

127 development is a significant contributor of greenhouse gas emissions to the atmosphere.

128 ase following the RCP2.6, RCP4.5, and RCP8.5 greenhouse gas emissions trajectories.

129 ond method that combines temporally resolved greenhouse gas emissions with techno-economic analysis.

130 ssions (which account for ~10% of total U.S. greenhouse gas emissions) and corresponds to an emission

131 al system and led to reductions of 29-47% in greenhouse gas emissions, 26-41% in energy consumption,

132 most efforts have been directed to reducing greenhouse gas emissions, complementary strategies are n

133 cores, and BMI; 2) environmental indicators (greenhouse gas emissions, cumulative energy demand, and

134 from additional change due to anthropogenic greenhouse gas emissions, including the 4 per mille init

135 icted rates of warming arising from moderate greenhouse gas emissions, inhibitory effects of climate

136 ation would push back the timeline to reduce greenhouse gas emissions, largely undermining the Paris

137 yntheses link earthworm activities to higher greenhouse gas emissions, less soil biodiversity, and in

138 Given its total contribution to greenhouse gas emissions, the global electric power sect

139 Beyond greenhouse gas emissions, the power sector is also respo

140 00 years at present, but, without mitigating greenhouse gas emissions, this can decrease to 3.5 years

141 Under business-as-usual greenhouse gas emissions, we show that 80% of the coloni

142 ny mining operations could offset net mining greenhouse gas emissions, while simultaneously giving va

143 dustrial levels requires rapid reductions in greenhouse gas emissions.

144 are responsible for more than 80% of global greenhouse gas emissions.

145 ation, but it is also an important source of greenhouse gas emissions.

146 sing approach for producing hydrogen without greenhouse gas emissions.

147 2 mg/kg fuel, corresponding to 1.5% of total greenhouse gas emissions.

148 and chemicals is a major pursuit in reducing greenhouse gas emissions.

149 standards in particular, is the reduction of greenhouse gas emissions.

150 leum fuels, with the potential to reduce net greenhouse gas emissions.

151 cations for nitrogen loss, conservation, and greenhouse gas emissions.

152 s that describe how society could reduce its greenhouse gas emissions.

153 coal-mine methane to recover fuel and reduce greenhouse gas emissions.

154 co-benefit for society in terms of reducing greenhouse gas emissions.

155 ation, explosive conditions in soil gas, and greenhouse gas emissions.

156 ld take action to reduce its contribution of greenhouse gas emissions.

157 ution of SOC, and contribute to reducing net greenhouse gas emissions.

158 infall events as a consequence of increasing greenhouse gas emissions.

159 accounting for 24% of difficult-to-eliminate greenhouse gas emissions.

160 too optimistic, increasing the need to curb greenhouse gas emissions.

161 d management practices that help to minimize greenhouse gas emissions.

162 limate variability, and can be attributed to greenhouse gas emissions.

163 e between good surface water quality and low greenhouse gas emissions.

164 r the twenty-first century assuming unabated greenhouse gas emissions.

165 patible with a transition to global net-zero greenhouse gas emissions.

166 saline aquifers is needed to mitigate global greenhouse gas emissions; monitoring the mechanical inte

167 Diet-related greenhouse-gas emissions, cumulative energy demand, and

168 impact on plant performance and increases in greenhouse gas emitting microbes.

169 Here, we calculate carbon-based greenhouse gas fluxes associated with the NAIP at sub-mi

170 he century (1900-1949), however, a signal of greenhouse-gas-forced change is robustly detectable.

171 er significantly from an expected pattern of greenhouse gas forcing around mid-century (1950-1975), c

172 ern Hemisphere in response to insolation and greenhouse gas forcing is thought to have caused groundi

173 Models that characterize life cycle greenhouse gases from electricity generation are limited

174 is a key process determining the release of greenhouse gases from surface waters and a fundamental c

175 ing Earth's climate sensitivity to increased greenhouse gases from the historical record.

176 not have direct observations of atmospheric greenhouse gases from this period.

177 As countries advance in greenhouse gas (GHG) accounting for climate change mitig

178 an help achieve emission reductions for both greenhouse gas (GHG) and air toxics from O&G production

179 udy fills the information gap, analyzing the greenhouse gas (GHG) and criteria air pollutant (CAP) em

180 endent in each other's water and energy use, greenhouse gas (GHG) and PM(2.5) emissions, and labor an

181 red by coastal wetlands can influence global greenhouse gas (GHG) budgets.

182 ing technologies are important components of greenhouse gas (GHG) emission reduction strategies for l

183 data from 2014, we investigate U.S. refinery greenhouse gas (GHG) emissions (CO(2), CH(4), and N(2)O)

184 effectively moved the mean of the life cycle greenhouse gas (GHG) emissions 38% higher while maintain

185 Greenhouse gas (GHG) emissions affect precipitation worl

186 ehicle fleet model to assess implications on greenhouse gas (GHG) emissions and energy demand.

187 erstand aquaculture's contribution to global greenhouse gas (GHG) emissions and how it can be mitigat

188 , cycling and other active modes) may reduce greenhouse gas (GHG) emissions and improve health.

189 Agriculture is a major contributor to global greenhouse gas (GHG) emissions and must feature in effor

190 roduction (i.e., protein and iron), minimize greenhouse gas (GHG) emissions and resource use (i.e., w

191 Quantifying greenhouse gas (GHG) emissions and setting GHG emissions

192 e, and it is critical to understand how soil greenhouse gas (GHG) emissions and uptake will respond t

193 a factor of 12.7-29.5 under a high-intensity greenhouse gas (GHG) emissions and urban development pat

194 of these alternative cements result in lower greenhouse gas (GHG) emissions as well as other indicato

195 nied by environmental burdens, including the greenhouse gas (GHG) emissions associated with fertilize

196 Since the greenhouse gas (GHG) emissions associated with landfilli

197 , nitrogen fertilizer (Nr) and water use and greenhouse gas (GHG) emissions exist, and could improve

198 Balancing crop production and greenhouse gas (GHG) emissions from agriculture soil req

199 agrass restoration projects and help reverse greenhouse gas (GHG) emissions from global seagrass loss

200 is an effective way to reduce the life cycle greenhouse gas (GHG) emissions from light-duty vehicles.

201 an Africa and estimates changes in preretail greenhouse gas (GHG) emissions if the cold chain develop

202 y for forecasting air quality and estimating greenhouse gas (GHG) emissions in cities.

203 rgets on both direct and indirect (upstream) greenhouse gas (GHG) emissions in order to reconcile tra

204 ntial energy use accounts for roughly 20% of greenhouse gas (GHG) emissions in the United States.

205 Strategies that reduce greenhouse gas (GHG) emissions may also provide signific

206 Greenhouse gas (GHG) emissions of carbon dioxide (CO(2))

207 Across 21 analyzed scenarios, annual greenhouse gas (GHG) emissions of the light-duty vehicle

208 renewable energy, some projects produce high greenhouse gas (GHG) emissions per unit electricity gene

209 hicles in China has led to a net increase in greenhouse gas (GHG) emissions since 2000.

210 al Corporate Average Fuel Economy (CAFE) and greenhouse gas (GHG) emissions standards and the Zero Em

211 cate that China's non-carbon dioxide (CO(2)) greenhouse gas (GHG) emissions will increase rapidly fro

212 To reduce oil consumption and resulting greenhouse gas (GHG) emissions, carbon dioxide can be ca

213 h Columbia (BC), Canada using three metrics: greenhouse gas (GHG) emissions, electricity cost, and ov

214 periment to estimate fossil energy (FE) use, greenhouse gas (GHG) emissions, PM(2.5)-related emission

215 tributes significantly, up to 10%, to global greenhouse gas (GHG) emissions.

216 t with industrial byproducts to reduce their greenhouse gas (GHG) emissions.

217 on of animal protein is associated with high greenhouse gas (GHG) emissions.

218 water and wastewater services contributes to greenhouse gas (GHG) emissions.

219 perceived risks of aquifer contamination and greenhouse gas (GHG) emissions.

220 nal N fertilizer and mitigating soil surface greenhouse gas (GHG) emissions.

221 ts on global gas supply-demand rebalance and greenhouse gas (GHG) emissions.

222 isturbances on carbon accumulation rates and greenhouse gas (GHG) emissions.

223 ucing forest carbon (C) sinks and increasing greenhouse gas (GHG) emissions.

224 he magnitudes, patterns and drivers of these greenhouse gas (GHG) fluxes remain poorly understood.

225 voked to explain non-normal distributions of greenhouse gas (GHG) fluxes, also known as hot spots and

226 soil profile, SI could potentially increase greenhouse gas (GHG) fluxes, particularly N(2)O through

227 cycle assessment to calculate the energy and greenhouse gas (GHG) footprints of irrigation.

228 tic model to quantify the variability in the greenhouse gas (GHG) footprints of product distribution

229 tly by natural decadal variability, but that greenhouse gas (GHG) forcing erodes the pattern and degr

230 Few studies have evaluated the life cycle greenhouse gas (GHG) impacts associated with India's pow

231 ted wood products (HWPs) can affect national greenhouse gas (GHG) inventories, in which the productio

232 pling challenges when utilizing conventional greenhouse gas (GHG) measurement systems.

233 At maximum diversion, the greenhouse gas (GHG) mitigation costs ranged from 30 to

234 ated in biorefineries can also contribute to greenhouse gas (GHG) mitigation goals.

235 ery systems is the most efficient method for greenhouse gas (GHG) mitigation, and its total GHG mitig

236 forest to drainage-based agriculture alters greenhouse gas (GHG) production, but the magnitude of th

237 able Fuel Standard (RFS) program specifies a greenhouse gas (GHG) reduction threshold for cellulosic

238 Landfilling is the most greenhouse gas (GHG)-intensive option, emitting nearly 4

239 thropogenic aerosols, volcanic aerosols, and greenhouse gases (GHG)-relative to each other and to int

240 paper, we compared the well-to-wheels (WTW) greenhouse gases (GHGs) and criteria air pollutant emiss

241 The forcing of rising greenhouse gases (GHGs) is robustly detected and largely

242 nic matter and stimulate the release of soil greenhouse gases (GHGs), but to what extent soil release

243 Increased concentrations of atmospheric greenhouse gases have led to a global mean surface tempe

244 el warming projections, forced by increasing greenhouse gases, have a large inter-model spread in bot

245 umptions concerning the radiative forcing of greenhouse gases, ice sheets and mineral dust aerosols,

246 their chemical structure makes them possible greenhouse gases if their atmospheric lifetimes are long

247 the production or consumption of this potent greenhouse gas in methanogenic and methanotrophic archae

248 Nitrous oxide (N(2)O), a potent greenhouse gas in the atmosphere, is produced mostly fro

249 et some of the warming due to the buildup of greenhouse gases in Earth's atmosphere.

250 g in any one year increases as the levels of greenhouse gases in the atmosphere increase; (iii) green

251 Ruminants contribute to the emissions of greenhouse gases, in particular methane, due to the micr

252 s against eutrophication and society against greenhouse gas-induced warming.

253 erved increase in VPD cannot be explained by greenhouse-gas-induced (GHG) radiative warming alone.

254 rogram to an assessment of the U.S. Regional Greenhouse Gas Initiative (RGGI), the United States' fir

255 The annual greenhouse gas intensity of optimal nitrogen rate decrea

256 ion could modulate the efflux of this potent greenhouse gas into the environment.

257 ent to the 2006 IPCC Guidelines for National Greenhouse Gas Inventories, we incorporate DeltaAGB data

258 tory and the Environmental Protection Agency Greenhouse Gas Inventory (GHGI) with regional airborne e

259 he per-station emission factor used in EPA's greenhouse gas inventory (GHGI).

260 S. Environmental Protection Agency's current greenhouse gas inventory estimate for pipeline mains in

261 gy trapped on Earth by increasingly abundant greenhouse gases is absorbed by the ocean.

262 e the extent to which the warming induced by greenhouse gases is masked by aerosols.

263 f methane (CH(4)), the second most important greenhouse gas, is currently increasing by ~10 million t

264 half the present value, and warming by other greenhouse gases like methane was not a major factor, th

265 preparing reference materials of high impact greenhouse gases, limiting progress toward coherent and

266 ion dominate snow melt period causing larger greenhouse gas losses during spring.

267 le for 70% of global emissions of the potent greenhouse gas methane (CH(4)).

268 As a major greenhouse gas, methane, which is directly vented from t

269 Methane is a potent greenhouse gas; methane production and consumption withi

270 r biodiversity protection and land use-based greenhouse gas mitigation call for increases in the effe

271 Since greenhouse gas mitigation efforts are mostly being imple

272 l life cycle assessment of the potential for greenhouse gas mitigation, including additional effects

273 r enzyme nitrous oxide reductase reduces the greenhouse gas N(2)O to uncritical N(2) as the final ste

274 Assessment of the global budget of the greenhouse gas nitrous oxide ([Formula: see text]O) is l

275 ly recognized as significant sources for the greenhouse gas nitrous oxide (N(2) O).

276 e conversion of the environmentally critical greenhouse gas nitrous oxide (N(2)O) to dinitrogen (N(2)

277 Factors influencing production of greenhouse gases nitrous oxide (N(2)O) and nitrogen (N(2

278 ons from landfilling, but emissions of other greenhouse gases, odorous/toxic species, and reactive co

279 adly assumed that hydropower facilities emit greenhouse gases on par with wind, there is mounting evi

280 of the North Atlantic, caused by increasing greenhouse gases over the 21st century, climate projecti

281 Here, the greenhouse gas payback time for 4161 wind turbine locati

282 The greenhouse gas payback time of wind turbines in northwes

283 nding biogas production systems to help meet greenhouse gas reduction goals.

284 anic and Atmospheric Administration's Global Greenhouse Gas Reference Network.

285 We expanded the Greenhouse gases, Regulated Emissions, and Energy use in

286 assessment methodology ignores the impact of greenhouse gases relative to when they are emitted.

287 g synthetic chemistry, gas valorization, and greenhouse gas remediation.

288 ccumulate C, have a net positive atmospheric greenhouse gas removal effect, and support shoreline acc

289 degrees C, most scenario projections rely on greenhouse gas removal technologies (GGRTs); one such GG

290 than emission factors utilized by the EPA's greenhouse gas reporting program (GHGRP) but less than e

291 mes higher than those inferred from the 2016 Greenhouse Gas Reporting Program (GHGRP).

292 Using Greenhouse Gas Reporting Program data (GHGRP) and Nation

293 Environmental Protection Agency Greenhouse Gas Reporting Program, National Emissions Inv

294 ity of the integration of a dense network of greenhouse gas sensors with a science-driven building an

295 olysis offers an attractive route to upgrade greenhouse gases such as carbon dioxide (CO(2)) to valua

296 N(2)O), like carbon dioxide, is a long-lived greenhouse gas that accumulates in the atmosphere.

297 t a method for leveraging the social cost of greenhouse gases to account for the temporal impacts of

298 mportant source of methane (CH(4)), a potent greenhouse gas, to the atmosphere.

299 ols on clouds offsets an unknown fraction of greenhouse gas warming.

300 able dry reforming catalysts from two potent greenhouse gases which could be of great interest for ma