ライフサイエンスコーパス: degree Celsius

1 temperature sensitivity (change in days per degree Celsius).

2 ynthesis at high temperatures (more than 230 degrees Celsius).

3 ty of 1.8 joules per cubic centimetre at 250 degrees Celsius).

4 Clausius-Clapeyron (C-C) relation of 7% per degree Celsius.

5 g scenarios from 1 to 5 degrees C is 10% per degree Celsius.

6 s and to "pursue efforts" to limit it to 1.5 degrees Celsius.

7 g the target of keeping warming well below 2 degrees Celsius.

8 ndicates subsurface warming of up to about 2 degrees Celsius.

9 d to fall below 10(-3) Omega cm(2) above 250 degrees Celsius.

10 he process temperature is in excess of 1,538 degrees Celsius.

11 esent are controllable typically to within 2 degrees Celsius.

12 elatonin synthesis for at least 5 days at 27 degrees celsius.

13 temperature (incidence rate ratio [IRR] per degree Celsius, 1.07 [95% confidence interval [CI], 1.05

14 sitivity of 9 degrees Celsius (range 7 to 13 degrees Celsius, 95 per cent credible interval) change i

15 l warming of 5 degrees Celsius (range 3 to 7 degrees Celsius, 95 per cent credible interval) over the

16 At temperatures above 900 degrees Celsius, a deformed solid matrix with nearly iso

17 obal mean surface temperatures by 0.3 to 4.8 degrees Celsius above pre-industrial values by the end o

18 that if atmospheric warming exceeds 1.5 to 2 degrees Celsius above present, collapse of the major Ant

19 ity and minimum cumulative exposure (MCE) in degrees Celsius along climate trajectories for North Ame

20 western North Atlantic margin by up to eight degrees Celsius and are now triggering the destabilizati

21 ms at holding global warming to well below 2 degrees Celsius and to "pursue efforts" to limit it to 1

22 Celsius occurs within 20 seconds at minus 20 degrees Celsius and within 30 seconds at minus 30 degree

23 ergy intensive (requiring heating to 500-900 degrees Celsius) and does not fully restore performance.

24 an be regulated typically to within +/- 0.25 degrees Celsius, and peak temperatures more than 800 deg

25 hat reveals two abrupt warming events of 4-5 degrees Celsius at the onset of the Bolling and Holocene

26 (alpha-MoC) enables low-temperature (150-190 degrees Celsius), base-free hydrogen production through

27 d drugs between approximately 7% and 22% per degree Celsius below 37degreesC during cooling.

28 , the photonic radiative cooler cools to 4.9 degrees Celsius below ambient air temperature, and has a

29 ly demonstrate radiative cooling to nearly 5 degrees Celsius below the ambient air temperature under

30 hat would report sensitivity not in terms of degrees Celsius, but rather sensing distance.

31 but still imply a median warming of 2.6-3.1 degrees Celsius by 2100.

32 checked, the warming increase may reach 8-10 degrees Celsius by 2300.

33 Intermediate-temperature (400 to 600 degrees Celsius) carbonate-rich fractions of ALH84001 ha

34 es Celsius and within 30 seconds at minus 30 degrees Celsius, consuming only 3.8 per cent and 5.5 per

35 s away from the axis that feeds hot (500-700 degrees Celsius) deep-rooted off-axis flow towards the r

36 ) melting transition occurring at nearly 100 degrees Celsius ( degrees C) has been observed in Langmu

37 50 per cent state of charge and at minus 30 degrees Celsius, delivering 6.4-12.3 times the power of

38 .1% of all stations were greater than 7% per degree Celsius for the 75th, 90th, 99th, and 99.9th perc

39 A79001) revealed low-temperature (200 to 430 degrees Celsius) fractions with a carbon isotopic compos

40 001) surface at atmospheric pressure and 600 degrees Celsius has previously been shown to produce dis

41 Celsius, and peak temperatures more than 800 degrees Celsius have been demonstrated.

42 studies postulated that an increase of five degrees Celsius in intermediate-depth ocean temperatures

43 otion is consistent with a large decrease (5 degrees Celsius) in ocean temperature during the LGM, as

44 Results are odds ratio (OR; per degree Celsius increment within the quartile or median)

45 s similar to the canonical range (1.5 to 4.5 degrees Celsius), indicating that a large fraction of th

46 severe power loss at temperatures below zero degrees Celsius, limiting their use in applications such

47 ase above pre-industrial temperatures of two degrees Celsius, may fail to communicate the urgency of

48 ow that intermediate-temperature (200 to 350 degrees Celsius) molten salts containing caesium or pota

49 the internal warm-up of such a cell to zero degrees Celsius occurs within 20 seconds at minus 20 deg

50 ikes are predicted to increase 12 +/- 5% per degree Celsius of global warming and about 50% over this

51 ydrolysis or thiolysis at temperatures of 40 degrees Celsius or higher, and we have exploited this ac

52 On in vitro incubation at 37 degrees Celsius or higher, the intein mediates efficient

53 e to the pre-industrial period of 2.1 to 4.6 degrees Celsius per CO2 doubling (66 per cent confidence

54 cally significant rate of 0.5 degrees to 0.7 degrees Celsius per decade over the past 30 years.

55 high geothermal gradients (of more than 700 degrees Celsius per gigapascal).

56 an average geothermal gradient of 125 +/- 55 degrees Celsius per kilometre within the hanging wall of

57 a near-surface thermal gradient of 31 +/- 15 degrees Celsius per kilometre.

58 Slow cooling (a few degrees Celsius per minute) resulted in much higher M. t

59 ees Celsius per second during heating and 15 degrees Celsius per second during cooling have been achi

60 Temperature transition rates of 44 degrees Celsius per second during heating and 15 degrees

61 mmit Earth to an eventual total warming of 5 degrees Celsius (range 3 to 7 degrees Celsius, 95 per ce

62 s estimates an Earth system sensitivity of 9 degrees Celsius (range 7 to 13 degrees Celsius, 95 per c

63 ss is replenished on-axis by warm (up to 300 degrees Celsius) recharge flow surrounding the hot therm

64 d in the two-standard-deviation spread (-1.2 degrees Celsius) relative to the raw model projections r

65 y of denaturation of just 2.3 kcal/mol at 10 degrees Celsius so only small changes in energy upon mut

66 tes at relatively high temperatures (200-350 degrees Celsius), so the focus for vehicle and portable

67 ur-long batch-reactor tests conducted at 150 degrees Celsius, using either the zeolite-supported or t

68 At temperatures above 300-450 degrees Celsius, usually found at depths greater than 10

69 mean annual surface air temperature over ten degrees Celsius warmer than during the pre-industrial pe

70 nterstadial), the deep ocean was about three degrees Celsius warmer than shallower waters above.

71 dynamics (MD) simulations at 60, 75, and 100 degrees Celsius, which allows us to explore further the

72 r square centimetre, the cells cycled at 450 degrees Celsius with 98 per cent Coulombic efficiency an

73 g scenario is about 15 per cent warmer (+0.5 degrees Celsius) with a reduction of about a third in th

74 ' cell, that heats itself up from below zero degrees Celsius without requiring external heating devic