ライフサイエンスコーパス: carbon budget

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

2 he least constrained component of the global carbon budget.

3 23 +/- 13 g C m(-2) yr(-1) to the three-year carbon budget.

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

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

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

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

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

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

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

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

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

13 re essential for our understanding of global carbon budgets.

14 ertainty in projected changes in terrestrial carbon budgets.

15 w groundwater seepage contributes to aquatic carbon budgets.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

48 The carbon budget leads to cumulative discounted near term r

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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