ライフサイエンスコーパス: degree Celsius

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

2 and a high working temperature (up to 1,300 degrees Celsius).

3 5 per cent confidence interval: -6.5 to -5.7 degrees Celsius).

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

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

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

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

8 g at a readily accessible temperature of 200 degrees Celsius.

9 esent are controllable typically to within 2 degrees Celsius.

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

11 104 milliwatts per metre per kelvin at 1,000 degrees Celsius.

12 gical winter temperatures exceed minus eight degrees Celsius.

13 efficiency of more than 99.9 per cent at -30 degrees Celsius.

14 m micrometres and excellent stability at 125 degrees Celsius.

15 nt humidity) and more than five hours at 200 degrees Celsius.

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

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

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

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

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

21 mote further efforts to limit warming to 1.5 degrees Celsius(1).

22 n properties at temperatures exceeding 1,000 degrees Celsius(1-3).

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

24 to an equilibrium climate sensitivity of 3.4 degrees Celsius (2.4-4.5 degrees Celsius), a value that

25 ith the traditional consensus range of 2-4.5 degrees Celsius(3,4).

26 consistent with limiting future warming to 2 degrees Celsius(5).

27 hese cells are charged and discharged at -50 degrees Celsius (-60 degrees Celsius) at a C rate of 0.1

28 tic modulus between room temperature and 627 degrees Celsius (900 kelvin), which is, to our knowledge

29 onstraint on global mean LGM cooling of -6.1 degrees Celsius (95 per cent confidence interval: -6.5 t

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

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

32 sensitivity of 3.4 degrees Celsius (2.4-4.5 degrees Celsius), a value that is higher than previous L

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

34 ommit us to surface warming of three to four degrees Celsius above pre-industrial levels by 2100, whi

35 3-5), that at global warming levels around 2 degrees Celsius above pre-industrial levels, West Antarc

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

37 g in the twenty-first century to less than 2 degrees Celsius above preindustrial levels, and to promo

38 e temperature (GMST) goal of not more than 2 degrees Celsius above preindustrial.

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

40 o stabilize at a global warming level of 1.5 degrees Celsius above the pre-industrial level.

41 emperature of 287.7 +/- 1.2 kelvin (about 15 degrees Celsius) achieved at 267 +/- 10 gigapascals.

42 n a multivariable model, measured fever >=38 degrees Celsius (adjusted odds ratio = 4.6, 95% confiden

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

44 ensity and duration will increase to 4.0 0.2 degrees Celsius and 27.0 7.6 days, respectively.

45 nitial PCE after 1,000 hours of ageing at 85 degrees Celsius and 30 per cent relative humidity in air

46 re than six months at ambient conditions (25 degrees Celsius and about 30 per cent humidity) and more

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

48 how global warming can be kept well below 2 degrees Celsius and even 1.5 degrees Celsius, climate po

49 form a solid solution after annealing at 200 degrees Celsius and that the interface between the gold-

50 eriod, will increase from 3.7 0.1 to 5.4 0.8 degrees Celsius and their average duration will increase

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

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

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

54 production under harsh conditions (above 300 degrees Celsius) and transport are typically contracted

55 nlight for more than 1,800 hours at 70 to 75 degrees Celsius, and estimate that the time required for

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

57 y, indicate an abrupt cooling of about three degrees Celsius at the onset of Heinrich Stadial 1.

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

59 d and discharged at -50 degrees Celsius (-60 degrees Celsius) at a C rate of 0.1C, and the NMC811||gr

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

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

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

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

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

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

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

67 he agglomeration of the nanoparticles at 100 degrees Celsius by a factor of five compared with CQD co

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

69 increase more than a hundred-fold over a ten-degree Celsius change.

70 pt well below 2 degrees Celsius and even 1.5 degrees Celsius, climate policy uses scenarios that desc

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

72 from ~1300 meters and deeper suggest an ~0.5 degrees celsius cooling across the Medieval Climate Anom

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

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

75 ains if mean warming is to be limited to 1.5 degrees Celsius ( degrees C) with a probability of 66 to

76 50 per cent state of charge and at minus 30 degrees Celsius, delivering 6.4-12.3 times the power of

77 ed out in water at low temperature (below 50 degrees Celsius) enables access to widely used fluoroche

78 .1% of all stations were greater than 7% per degree Celsius for the 75th, 90th, 99th, and 99.9th perc

79 abbro transition remain at approximately 500 degrees Celsius for 0.1 million years.

80 fficiency after continuously operating at 65 degrees Celsius for 1200 hours under 1-sun illumination.

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

82 1 (MIS11), the global temperature was 1 to 2 degrees Celsius greater(2) and sea level was 6 to 13 met

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

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

85 illion(6) and temperatures were about 2 to 4 degrees Celsius higher than today(7), can improve our un

86 r 2,400 hours of 1-sun operation at about 55 degrees Celsius in air.

87 tested hypothermia, cryopreservation at -80 degrees Celsius in DMSO (dimethyl sulfoxide) and storage

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

89 or approximately 1,500 hours of ageing at 85 degrees Celsius in nitrogen and maintained 88 per cent o

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

91 For every degree Celsius increase in winter soil temperature, stra

92 cent of current global consumption) per one-degree-Celsius increase in global mean surface temperatu

93 cent of current global consumption) per one-degree-Celsius increase in GMST.

94 sed by 1 case per million people for every 5 degrees (Celsius) increase in temperature within the ran

95 of warming of the whole soil profile by four degrees Celsius increased CO(2) emissions by 55 per cent

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

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

98 the Paris Agreement to limit warming below 2 degrees Celsius is satisfied.

99 mean bias by 87 per cent compared with the 0-degree-Celsius isotherm approach.

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

101 n extent until temperatures are at least one degree Celsius lower than pre-industrial levels.

102 A two-standard deviation (1.8 degrees Celsius) lower wrist temperature amplitude corre

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

104 tes, the urban daytime T(w) is 0.17 +/- 0.14 degrees Celsius (mean +/- 1 standard deviation) higher t

105 south to 35 degrees north) cooled by 5.8 0.6 degrees Celsius (mean 95% confidence interval) during th

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

107 ly confined plasmas heated up to 100 million degrees Celsius must be sustained long enough to achieve

108 Moreover, when it is cold enough (below -15 degrees Celsius), nitric acid and ammonia can nucleate d

109 e CLOUD chamber at CERN, that below about +5 degrees Celsius, nitric acid and ammonia vapours can con

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

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

112 now becomes marginally more sensitive to one degree Celsius of warming as climatological winter tempe

113 an discharge has been decreasing by 9.3% per degree Celsius of warming because of increased evapotran

114 here is amplified, averaging 15 per cent per degree Celsius of warming-double the rate expected from

115 consistent with current policies (allowing 3 degrees Celsius of warming) give an abrupt jump in the p

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

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

118 o show that with global warming limited to 2 degrees Celsius or less, Antarctic ice loss will continu

119 ing greenhouse gas concentrations (0.25 0.21 degrees Celsius over the past 6,500 years or so).

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

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

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

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

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

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

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

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

128 ss (-9.1 megagrams of carbon per hectare per degree Celsius), primarily by reducing woody productivit

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

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

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

132 o twofold reductions in RNA copy numbers per degree Celsius relative to 37 C were observed.

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

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

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

136 Considering a 2(1.5) degree Celsius stabilization target, peak costs are grea

137 global mitigation pathways to achieve a 1.5 degree Celsius target.

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

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

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

141 warmer Pliocene Climatic Optimum (about four degrees Celsius warmer than pre-industrial levels)(6), o

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

143 rm Period, which was on average two to three degrees Celsius warmer than the pre-industrial period(5)

144 res SLE using the main projections under 1.5 degrees Celsius warming and 42 centimetres SLE using ris

145 ection exceeding half a metre even under 1.5 degrees Celsius warming.

146 from records having been truncated to whole degrees Celsius when the records were digitized in the 1

147 rmal expansion coefficient (1.2 x 10(-7) per degree Celsius), which ensures excellent structural flex

148 at an optimal reaction temperature (about 70 degrees Celsius), which can be directly achieved by harv

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

150 on budget for limiting global warming to 1.5 degrees Celsius will probably be exhausted within this d

151 transmission electron microscopy (TEM) at 80 degrees Celsius with 'freeze-and-look' TEM, we tracked t

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

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

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

155 harging over a wide temperature range (+/-60 degrees Celsius) without lithium plating, and non-flamma

156 We find that limiting global warming to 1.5 degrees Celsius would halve the land ice contribution to