ライフサイエンスコーパス: drawdown

1 weathering intensity), and more rapid CO(2) drawdown.

2 deep-water column without substantial oxygen drawdown.

3 egion for significant glacial carbon dioxide drawdown.

4 s to increase primary productivity and CO(2) drawdown.

5 d have contributed to glacial carbon dioxide drawdown.

6 cessing, followed by a conventional external drawdown after the dope has left the spinneret.

7 pps Institution of Oceanography (AltSIO)] to drawdown ambient DOC in a coastal ecosystem.

8 that regulates photosynthetic carbon dioxide drawdown and export from surface waters by phytoplankton

9 ave not explicitly represented this internal drawdown and therefore overestimate CO2 available for ca

10 n from the atmosphere and low biological CO2 drawdown are the main causes for the higher CO2, which a

11 We show that drawdowns as small as 0.5 m can stimulate ebullition eve

12 Like drawdown by means of silicate weathering, this source is

13 enhanced rates of atmospheric carbon dioxide drawdown by silicate chemical weathering.

14 ackenzie River, which is three times the CO2 drawdown by silicate weathering in this basin.

15 In these systems, we show that water-level drawdowns can, at least temporarily, greatly increase pe

16 t capacity and lowered its CO2 concentration drawdown capacity in the intercellular airspace and chlo

17 This drawdown could become sequestration because polar contin

18 prominence of Diatoms inferred from silicate drawdown, drive interannual differences in the magnitude

19 ies challenges the notion that episodic pCO2 drawdown drove this major Cenozoic climate transition.

20 ggest that episodes of major atmospheric CO2 drawdown during the last glacial period were linked to i

21 Given that drawdown events of this magnitude are quite common in re

22 Despite incomplete carbohydrate drawdown from defoliation and relatively rapid carbohydr

23 We model the temporal effects of CO2 drawdown from the atmosphere due to chemical weathering

24 t production, by increasing surface nutrient drawdown in an ocean general circulation model.

25 nstant leaf internal [CO2 ], ci , a constant drawdown in CO2 (ca - ci ), and a constant ci /ca .

26 production and associated atmospheric carbon drawdown in large parts of the world's oceans [1, 2].

27 tude is dominated by enhanced photosynthetic drawdown in North America and enhanced respiration in Eu

28 thought to contribute significantly to pCO2 drawdown in the Southern Ocean.

29 Furthermore, this drawdown is driven by plant uptake rather than other con

30 results support available evidence that CO2 drawdown--not gateway opening--caused Antarctic ice shee

31 Approximately 50% of this drawdown occurs in the world's active mountain belts, em

32 iosphere is recorded in fluorescence and the drawdown of [Formula: see text] during summer.

33 ly 3% benthic biomass) suggests an increased drawdown of approximately 2.9x10(6) tonnes of carbon per

34 Although approximately 10% of the ocean's drawdown of atmospheric anthropogenic carbon dioxide may

35 organic carbon correlates with a significant drawdown of atmospheric carbon dioxide (CO2) at that tim

36 gative feedback mechanisms inhibited further drawdown of atmospheric carbon dioxide by high rates of

37 he upper ocean and facilitates the diffusive drawdown of atmospheric CO(2).

38 an circulation crisis facilitated the coeval drawdown of atmospheric CO2 and high-latitude ice sheet

39 not support the suggestion that a long-term drawdown of atmospheric CO2 was the main cause of the cl

40 successfully modeled the persistent vertical drawdown of atmospheric COS using the quantitative relat

41 The drawdown of both carbon dioxide (CO2) and nitrate per mo

42 The drawdown of carbon dioxide began well before the Devonia

43 gest that the mechanisms responsible for the drawdown of CO2 may be more responsive to temperature th

44 localized glacier acceleration, concomitant drawdown of ice from neighboring areas leads to widespre

45 iple canopies, which coincided with moderate drawdown of nonstructural carbohydrate reserves.

46 t concentration of cells, which results in a drawdown of nutrients in oceanic surface waters.

47 C accounts for up to 53% of R as a result of drawdown of organic carbon within Eastern North Atlantic

48 in the Eastern Mediterranean, adding to the drawdown of soil moisture.

49 Although more complete drawdown of surface nutrients by phytoplankton during th

50 /U ratios (from 0.06 to 0.42), indicative of drawdown of U concentrations in seawater.

51 that eutrophication magnifies the effect of drawdown on CH4 emission.

52 erboreal benthos shows a similar increase in drawdown, polar continental shelves would represent Eart

53 ger increases in CH4 emission in response to drawdown (R(2) = 0.84, p < 0.01), suggesting that eutrop

54 Modeled variations in net CO2-drawdown rates are in excellent agreement with contempor

55 xtent to which (and the mechanisms by which) drawdowns short-circuit connections between methanogenes

56 ater pumping in Dhaka has caused large-scale drawdown that extends into outlying areas where arsenic-

57 evated primary production and biological DIC drawdown that reverses in some places the sign of the su

58 c glaciation would have required rapid CO(2) drawdown within the Oi-1 timeframe, to levels lower than

59 This process involves an unusual internal drawdown within the spider's spinneret that is not seen