ライフサイエンスコーパス: carbon budget

1 largest terrestrial component of the global carbon budget.

2 nge are critical to the future of the global carbon budget.

3 ontent can have a large effect on the global carbon budget.

4 rovide an important constraint on the global carbon budget.

5 es are critical for understanding the global carbon budget.

6 ge since 1750 to close the historical global carbon budget.

7 st remain unextracted to keep within a 1.5 C carbon budget.

8 mportant source of uncertainty in the global carbon budget.

9 nually, accounting for 3.9% of South Korea's carbon budget.

10 PP and Rs to improve estimates of the global carbon budget.

11 large role of coastal regions in the global carbon budget.

12 050 for the food system to remain within its carbon budget.

13 ly alter the dynamics of R(h) and the global carbon budget.

14 exhaustion of a rapidly dwindling remaining carbon budget.

15 ubstantial fraction of the total atmospheric carbon budget.

16 uture evolution in the context of the global carbon budget.

17 ons is critically important to the reservoir carbon budget.

18 and are therefore a key component of China's carbon budget.

19 ared with previous assessments of the global carbon budget.

20 have significant implications for the Amazon carbon budget.

21 ced the impact of N saturation on the global carbon budget.

22 he least constrained component of the global carbon budget.

23 23 +/- 13 g C m(-2) yr(-1) to the three-year carbon budget.

24 on were the two largest fluxes in the annual carbon budget.

25 is thus an important component of the arctic carbon budget.

26 P) is a critical step in closing the Earth's carbon budget.

27 the future evolution of the coastal ocean's carbon budget.

28 l ocean is a dynamic component of the global carbon budget.

29 ly, while still remaining within the overall carbon budget.

30 e system, play a critical role in the global carbon budget.

31 ions of vertical nutrient flux or in oceanic carbon budgets.

32 n be a significant component of regional net carbon budgets.

33 slab subduction and therefore influence deep carbon budgets.

34 mmonly omitted from calculations of mangrove carbon budgets.

35 undwater carbon sources and sinks for global carbon budgets.

36 ed inorganic carbon (DIC) outwelling to blue carbon budgets.

37 the surface ocean's alkalinity and inorganic carbon budgets.

38 y with Paris compliant regional sub-sectoral carbon budgets.

39 of CO(2) that requires inclusion in coastal carbon budgets.

40 ) in saltmarshes) was the major term in blue carbon budgets.

41 vegetation shifts and uncertainty in future carbon budgets.

42 te its substantial contribution to ecosystem carbon budgets.

43 nce of considering groundwater DOM in global carbon budgets.

44 anned point source imagers in closing global carbon budgets.

45 ation, and respiration, and summed them into carbon budgets.

46 icularly WWTPs in intermittent streams, into carbon budgets.

47 , summer, and autumn to species-level annual carbon budgets.

48 l geomorphic processes on freshwater wetland carbon budgets.

49 l for the development of regional and global carbon budgets.

50 as an impact of eutrophication on estuarine carbon budgets.

51 re essential for our understanding of global carbon budgets.

52 ertainty in projected changes in terrestrial carbon budgets.

53 rtance of southern boreal fires for regional carbon budgets.

54 w groundwater seepage contributes to aquatic carbon budgets.

55 land ecosystems and ensure accurate regional carbon budgeting.

56 ase in the unextractable estimates for a 2 C carbon budget(9), particularly for oil, for which an add

57 ospheric carbon dioxide inversion and global carbon budget accounting methods to investigate the evol

58 Carbon budget accounting relies heavily on Food and Agri

59 and-use and cover-change databases in global carbon budget accounting.

60 implications for the accurate development of carbon budgets across the US and around the world.

61 Arctic shrub expansion alters carbon budgets, albedo, and warming rates in high latitu

62 The carbon budget and dynamics of the Earth's interior, incl

63 paths of carbon loss, with implications for carbon budget and energy policies in the United States a

64 oss the world, fair sharing of the remaining carbon budget and health gains will be critical.

65 fferences between estimates of the remaining carbon budget and may provide a basis for reducing uncer

66 the gravitational pump, helping to close the carbon budget and motivating further investigation into

67 for the OUR differences observed between our carbon budget and other published studies from the North

68 challenge in constraining the modern global carbon budget and predicting future carbon-climate inter

69 e and a critical gap in assessing the global carbon budget and predicting future climate [C.

70 understanding of the evolution of the cosmic carbon budget and provides new methodologies for the bot

71 ad mortality of individual trees impacts the carbon budget and sequestration capacity of California f

72 rajectories that do not exceed the remaining carbon budget and support science-based pathways.

73 Here we investigate Amazonia's carbon budget and the main drivers responsible for its c

74 glacial-interglacial transitions, the global carbon budget and thermohaline ocean circulation respond

75 ables us to track estimates of the remaining carbon budget and to understand how these estimates can

76 ent with existing constraints on the Earth's carbon budget and would imply that as much as two thirds

77 on in car use is necessary to meet stringent carbon budgets and avoid high energy demand.

78 [Formula: see text]) are important in global carbon budgets and climate change assessments.

79 leaf traits and fluxes for determining plant carbon budgets and emergent ecosystem properties such as

80 hern Ocean and thus small relative to global carbon budgets and proposed geoengineering plans to sequ

81 iant Pathway including calculations of their carbon budgets and re-alignment pathways.

82 d be accounted for when forecasting mangrove carbon budgets and resistance to sea-level rise.

83 sments of BCP efficiencies as well as global carbon budgets and the interpretation of prior BCP studi

84 rent and strongly impacts the Southern Ocean carbon budget, and Antarctic ice-sheet dynamics across g

85 al Carbon Project (GCP) has published global carbon budgets annually since 2007 (Canadell et al. [200

86 Intertemporal flexibility of the carbon budget approach enables higher near-term emission

87 ll likely deplete a 1.5 degrees C consistent carbon budget around the year 2030, resulting in at leas

88 Here, we present emergent constraints on the carbon budget as a function of global warming, which com

89 reducing the effectiveness of the remaining carbon budget as a means of setting emission reduction t

90 ng in peatlands, which is relevant to global carbon budgets as climate change alters fire regimes wor

91 te the wastewater derived carbon into global carbon budget assessment, as well as to monitor and redu

92 he importance of including stem emissions in carbon budget assessments for mangrove ecosystems, highl

93 ities that is paramount to advance landscape carbon budget assessments.

94 ons will increase estimates of the remaining carbon budget associated with global warming thresholds,

95 ageing at leaf levels, nitrogen transfer and carbon budget at plant levels.

96 Global carbon budgeting, atmospheric data, and forest inventori

97 corresponds to about 35-60% of the remaining carbon budget available until 2050 if the average temper

98 Implications are discussed for carbon budgets based on observed changes in atmospheric

99 sis, respiration, total organic carbon flux, carbon budget, biomass, lipids, protein, and maximum Art

100 ggests less "missing" carbon from the global carbon budget but increasing emissions from tropical lan

101 Decomposition is a large term in the global carbon budget, but models of the earth system that simul

102 astal ecosystems play a major role in marine carbon budgets, but substantial uncertainties remain in

103 also quantified uncertainties in permafrost carbon budget by conducting Monte Carlo simulations.

104 The model generates the carbon budget by differencing carbon export and carbon s

105 Conspicuous deficits in ocean carbon budgets challenge this as a sole particle export

106 role of microbial interactions in mediating carbon budget changes and climate feedback in response t

107 in imbalance resulting from updates to each carbon budget component, leading to a 16% overall reduct

108 ades, assessments of the contemporary global carbon budget consistently report a strong net land carb

109 anic matter, making their role in the global carbon budget disproportionate to land area.

110 ced increased respiration rates and negative carbon budgets due to a 236% increase in total organic c

111 hly uncertain components of the contemporary carbon budget, due in part to the lack of spatially expl

112 bon Project (GCP) compiles an updated global carbon budget each year, synthesizing state-of-the-art e

113 teral hydrologic inflows/outflows in wetland carbon budgets, especially in those characterized by a f

114 The current study presents a 25 year carbon budget estimate for a typical commercial loblolly

115 The remaining carbon budget estimates are varied and nuanced(14,15), a

116 Here using global carbon budget estimates, ground, atmospheric and satelli

117 address some long-standing issues in global carbon budget estimates.

118 nes terrestrial biosphere models with global carbon budget estimates.

119 versity and plays a major role in the global carbon budget, estimates of tree biodiversity originate

120 and call for its consideration in the global carbon budget estimation.

121 y of steel and cement within Paris-compliant carbon budgets, explicitly considering uncertainties in

122 t global emissions and 8.3% of the remaining carbon budget for 2 degrees C.

123 The remaining carbon budget for limiting global warming to 1.5 degrees

124 % and 15% in the current estimated remaining carbon budget for limiting global warming well below 1.5

125 of ecosystem carbon fluxes and to a detailed carbon budget for the 1980s.

126 Our data represent the complete carbon budget for tropical forests measured throughout a

127 (ESMs) continue to diagnose a wide range of carbon budgets for each level of global warming.

128 central process during attempts to establish carbon budgets for lakes and landscapes containing lakes

129 timate mean and likely ranges for cumulative carbon budgets for the Paris targets of 1.5 degrees C an

130 phic processes be considered when developing carbon budgets for these marginal environments.

131 t be detected, and reasonably estimated the "carbon budget" for holding warming below 2 degrees C.

132 ng can significantly affect local and global carbon budgets from increased fire occurrence, influenci

133 a wide range of estimates for the remaining carbon budget has been reported, reducing the effectiven

134 (5), and perhaps two-thirds of the remaining carbon budget if mean warming is to be limited to less t

135 tween these terms, referred to as the global carbon budget imbalance, reflects the aggregate inaccura

136 this question by quantifying the autotrophic carbon budget in 16 forest plots along a 3300 m elevatio

137 can improve our understanding of the global carbon budget in a warming world of changing vegetation

138 Our results can improve estimates of the carbon budget in China's forests and for better understa

139 sitic plants have on their leguminous hosts' carbon budget in terms of effects on host physiology and

140 regional and seasonal carbohydrate and dEPS carbon budgets in coupled physical-biogeochemical models

141 significant role in forest productivity and carbon budgets in future.

142 y important implications for regional annual carbon budgets in glacierized watersheds.

143 egradation of DOC is especially critical for carbon budgets in the Arctic, where thawing permafrost s

144 mismatch, we estimate that wildflower spring carbon budgets in the northeastern United States were 12

145 o the outdoor atmosphere, the indoor organic carbon budget is comparatively understudied.

146 g this proposed method will ensure the Paris carbon budget is met and that progress can be tracked ac

147 Of particular importance for the global carbon budget is net biome exchange of CO2 with the atmo

148 ions, but the impact of deep nitrogen on the carbon budget is small due to enhanced nitrogen availabi

149 Quantifying surface energy and carbon budgets is essential for projecting Earth's clima

150 The carbon budget leads to cumulative discounted near term r

151 cal carbon sink and the global anthropogenic carbon budget left to limit peak global warming below 2

152 ts and suggest that existing landscape-scale carbon budgets may overstate the magnitude of the coasta

153 e variability/anomalies and, thus, the total carbon budgets may vary drastically among years.

154 To address this growing issue, we use a carbon budget model combined with an energy system model

155 To do so, we modified a saltmarsh carbon budget model for application in freshwater coasta

156 Furthermore, the carbon budget model refined in this study can be used to

157 nclusion of this process in global and local carbon budget models.

158 The changes in the carbon budget of Amazonia during 2019-2020 were mainly b

159 h is a critical step towards quantifying the carbon budget of Earth's deep interior.

160 e present a detailed field assessment of the carbon budget of multiple forest sites in Africa, by mon

161 these findings, we suggest that the overall carbon budget of rainforests, summed across terrestrial

162 of seeps located at >20 m water depth in the carbon budget of the Panarea offshore gas release system

163 The carbon budget of the tropics has been perturbed as a res

164 at subdaily time steps in the assessment of carbon budgeting of reservoirs and carbon cycling along

165 e the uptake per unit root length, while the carbon budgets of the plant do not permit greater total

166 climate policies imposed by an intertemporal carbon budget on incremental costs of policies restricti

167 ystematically accounted for in either global carbon budgets or national carbon accounting.

168 is often insufficient to balance mesopelagic carbon budgets or to meet the demands of subsurface biot

169 information, such as a reduced 1.5 degrees C carbon budget, or slower-than-expected low-carbon techno

170 ade, implying a degree of self-regulation of carbon budgets over mesoscales.

171 Our data demonstrate the potential of whole carbon budget perspectives to provide a deeper understan

172 Under a fixed carbon budget, plants must allocate carbon to their mutu

173 contributes to staying within the remaining carbon budget, policy makers are urged to systematically

174 on of phytoplankton production to the global carbon budget, present and future.

175 ic carbon have broad implications for global carbon budget projections.

176 e contribution of N saturation to the global carbon budget remains uncertain due to the complicated n

177 res indicates that global and Southern Ocean carbon budget shifts preceded thermohaline circulation c

178 We constructed a conceptual energetic (carbon) budget showing that microplastic-exposed copepod

179 pita allocation of a remaining 1.5 degrees C carbon budget starting in 1990.

180 bout four times of preindustrial atmospheric carbon budget) stored in the deep mantle and isolated fr

181 bient oxygen have been used to constrain the carbon budget, study photosynthesis, estimate marine pro

182 laboratory observations, and ecosystem-level carbon budgets suggest that community turnover times are

183 climate regulation service, we constructed a carbon-budget supplemented by data from the literature,

184 to land use legacies, but their accumulated carbon budget switched to a carbon sink in the 1960s, se

185 on rates (R) are obtained from a net organic carbon budget that is based on the transport estimates,

186 s CO(2)) thus represent more than the entire carbon budget that remains if mean warming is to be limi

187 metabolism, translocation) disruption of the carbon budget that threatens seagrass health and surviva

188 ctions in carbon sequestration, but complete carbon budgets that include both methane (CH4 ) and late

189 ir Paris Agreement commitments; however, the carbon budgets that informed these commitments were inco

190 carbon, which are constrained by the global carbon budget, the gross fluxes are largely unconstraine

191 to account for the majority of their annual carbon budgets, the 12-month photosynthetic trajectories

192 atural and anthropogenic aerosol loadings on carbon budgets, the likelihood of meeting Paris targets,

193 eased consensus in sub-national and sectoral carbon budgets, the scale of reduction necessary stays u

194 makes it possible to estimate the remaining carbon budget: the total amount of anthropogenic carbon

195 represent up to 13% of humanity's remaining carbon budget through 2050.

196 imates of the sensitivity of the terrestrial carbon budget to climate anomalies in the tropics and th

197 st, we constructed a comprehensive ecosystem carbon budget to track the fate of carbon as the forest

198 2023-2060, meeting a 2 degrees C-compatible carbon budget under the Sustainability Shared Socioecono

199 unted for large proportions of some species' carbon budgets (up to 58% and 19%, respectively).

200 which may be compatible with the 2 degrees C carbon budget using an equal-per-capita approach.

201 erm, which is often ignored, in the peatland carbon budget, we find that it increases the estimate of

202 from the UK Climate Change Committee's Sixth Carbon Budget, were examined using a chemical transport

203 ortion of the electricity sector's remaining carbon budget when added up over time.

204 ccurate prediction of future tropical forest carbon budgets will require accounting for disturbance-r

205 Asia is an important region for the global carbon budget, with 4 of the world's 10 largest national

206 and contributing significantly to the global carbon budget, yet molecular mechanisms of their gene ex