ライフサイエンスコーパス: heat flux

1 ip with a high ( approximately 1,300 W cm-2) heat flux.

2 own to decline monotonically with increasing heat flux.

3 rculation through its regulation of poleward heat flux.

4 deformed terrain and has an anomalously high heat flux.

5 c Deep Water formation and northward oceanic heat flux.

6 uch as 500%, allowing digital control of the heat flux.

7 electric fields perpendicular to an incident heat flux.

8 rs with a corresponding decrease in sensible heat flux.

9 er changes in the sum of latent and sensible heat fluxes.

10 the partitioning between sensible and latent heat fluxes.

11 rove estimates of the global circulation and heat fluxes.

12 and climate directly by regulating water and heat fluxes.

13 r supplied to the geodynamo, measured by the heat flux across the core-mantle boundary (CMB), places

14 weak post-perovskite strongly increases the heat flux across the core-mantle boundary and alters the

15 re we show that a transient increase in core heat flux after an overturn of an initially stratified l

16 imes when the nature of core-mantle boundary heat flux allows the geodynamo to operate at peak effici

17 problem: a large increase in the conductive heat flux along the adiabat (due to the higher conductiv

18 The local heat flux and dryout time scale are measured as the liqu

19 volution will need to incorporate a high CMB heat flux and explain the recent formation of the inner

20 configuration in order to measure the entire heat flux and improve sensitivity.

21 ncreased [CO2 ] resulted in decreased latent heat flux and increased sensible heat flux from both cro

22 l observations, including coherence-enhanced heat flux and negative differential thermal conductance.

23 Both latent heat flux and partitioning are connected to water table

24 uces a 9% enhanced transient eddy meridional heat flux and reconciles a decadal variation of mid-lati

25 , Greenland, and is associated with elevated heat flux and strong wind stress curl.

26 In this way, the cell-heating bees alter the heat flux and temperature distributions in the brood reg

27 concile the discrepancy between the observed heat flux and the heat production of the mid-ocean ridge

28 geomagnetic field, the core-mantle boundary heat flux and the time of formation of the inner core.

29 ctivity of iron alloys defines the adiabatic heat flux and therefore the thermal and compositional en

30 d by two processes: cumulative ocean surface heat fluxes and sea ice formation close to PIIS; and int

31 erature pairs between temperature using zero-heat-flux and arterial temperature and between arterial

32 es C, 61,298 pairs of temperature using zero-heat-flux and esophageal temperature were collected and

33 es the nonlinear response of the energy, the heat flux, and even the one-dimensional energy and heat

34 ct arrangement of tectonic features, intense heat flux, and geyser-like plumes.

35 elop complex surficial geomorphologies, high heat fluxes, and geyser-like activity even if they do no

36 sed on measurements of sensible (H) and soil heat fluxes, and net radiation.

37 ly high, and a significant positive sensible heat flux anomaly developed.

38 urface, but there is no significant sensible heat flux anomaly within the core of the heat wave affec

39 m s(-1)) can drive changes in surface latent heat flux ( approximately +/-14.35 W m(-2)) and thus in

40 ductivity, the regional core-mantle boundary heat flux (approximately 85 +/- 25 milliwatts per square

41 Thermal rectifiers whose forward heat fluxes are greater than reverse counterparts have b

42 sea ice loss and associated upward turbulent heat fluxes are relatively minor in this event.

43 ificial structures that can actively control heat flux at a continuum scale.

44 The heat flux at the VDVF is measured at 487+/-101 MW, compa

45 he CMB, higher than present estimates of CMB heat flux based on mantle convection; the top of the cor

46 tive measurements of the near-field mediated heat flux between a gold coated near-field scanning ther

47 approach to create high-efficiency and high-heat-flux boiling surfaces which are naturally insensiti

48 rates and of input parameters necessary for heat flux calculations, as obtained from four harp seals

49 e regional differences require local surface heat flux changes (+/-4 watts per square meter) much lar

50 a century of research on enhancing critical heat flux (CHF) has focused on altering the boiling surf

51 The critical heat flux (CHF) in boiling and the Leidenfrost point tem

52 ayer showed approximately two times critical heat flux (CHF) increase compared to that of a plain sur

53 Enhancing the critical heat flux (CHF) of industrial boilers by surface texturi

54 ntly, a 2X increase in the boiling critical heat flux (CHF) was observed.

55 ility for the onset of pool boiling Critical Heat Flux (CHF).

56 Estimates of CMB heat flux depend on properties of iron mixtures under th

57 ations measured by spectrophotometry and the heat flux dissipated by oxidation reactions and measured

58 ations measured by spectrophotometry and the heat flux dissipated by oxidation reactions.

59 ental device based on the measurement of the heat flux dissipated during chemical reactions, previous

60 s developed, based on the measurement of the heat flux dissipated during chemical reactions.

61 Further analysis indicates that heat flux dominates the western SPNA OHC, but in the eas

62 surface is unable to compensate with latent heat flux due to water limitation.

63 mplex, dynamic role in ocean circulation and heat fluxes during its initiation, and these processes a

64 riments were also performed to demonstrate a heat flux enhancement up to 3X at the same surface super

65 d and 1,850 triple of temperature using zero-heat-flux, esophageal temperature, and arterial temperat

66 We found that heat flux estimates generally underestimated metabolic r

67 Heat flux estimates were made using two free convection

68 r if it was associated with erroneous latent heat flux estimates.

69 (OGCMs), forced by observed wind stress and heat flux for the years 1992 through 1994, show that oce

70 Based on these calculations, efficient heat flux from a deep magma ocean may have exceeded the

71 ased latent heat flux and increased sensible heat flux from both crops when averaged over 30 years.

72 ata, we develop estimates of the unconverted heat flux from individual U.S. thermal power plants in 2

73 dary is comparable to estimates of the total heat flux from the core but decreases with depth, so tha

74 nductivity of the lower mantle and therefore heat flux from the core.

75 boundary layer forms as a consequence of the heat flux from the Earth's outer core, the origin of an

76 rmore, our results indicate that the surface heat flux from the oceans to the atmosphere may play an

77 lux through the skin and fur, and convective heat flux from the surface of the animal to the environm

78 ated parts of India than it is to changes in heat fluxes from adjacent elevated terrain.

79 odel is more sensitive to changes in surface heat fluxes from non-elevated parts of India than it is

80 diation (R(n)), sensible heat flux (H), soil heat flux (G(0)) and latent heat flux (lambdaET) of a co

81 determine the net radiation (R(n)), sensible heat flux (H), soil heat flux (G(0)) and latent heat flu

82 The plume characteristics and local high heat flux have been ascribed either to the presence of l

83 ntres accounts for about ten per cent of all heat flux in the oceans and controls the thermal structu

84 activity driven by the greater-than-average heat flux in the region.

85 radiative energy between latent and sensible heat fluxes in daytime hours.

86 SSTs are more (less) sensitive to surface heat fluxes in regions with shallow (deep) mixed layer.

87 rom nonequilibrium terms (viscous stress and heat flux) in conventional models, specific hydrodynamic

88 e blackbody emission spectrum, the radiative heat flux increases by orders of magnitude.

89 perturb the system with sea level and ocean heat flux increases to investigate ice-sheet vulnerabili

90 try has been used to understand how changing heat flux influenced Archaean geodynamics, but records o

91 for spreading the hydrothermal chemical and heat flux into the deep-ocean interior and for dispersin

92 The average total urban heat flux into the shallow aquifer in Karlsruhe was foun

93 By modeling the anthropogenic heat flux into the subsurface of the city of Karlsruhe,

94 New estimates indicate that the adiabatic heat flux is 15 to 16 terawatts at the CMB, higher than

95 wo uncertainty in thermal conductivity, core heat flux is 80 to 160 milliwatts per square meter (mW m

96 ell thickness needed to produce the observed heat flux is at least 5 km.

97 This heat flux is probably due to localized tidal dissipation

98 t flux (H), soil heat flux (G(0)) and latent heat flux (lambdaET) of a commercial soybean (Glycine ma

99 ters in tiny areas, representing discretized heat flux lines in local spots.

100 ion in thermal conductivity, or to endogenic heat fluxes locally reaching 1 watt per square meter.

101 ility of the cutaneous sensor using the zero-heat-flux method compared with esophageal or iliac arter

102 noninvasive cutaneous temperature using zero-heat-flux method to esophageal temperature and arterial

103 In this study, we develop an analytical heat flux model to investigate possible drivers such as

104 We conclude that cutaneous heat flux models are too inaccurate and sensitive to sma

105 Heat flux models have been used to predict metabolic rat

106 Conductive heat flux near the core-mantle boundary is comparable to

107 res ('tiger stripes') within an area of high heat flux near the south pole.

108 predictions resulting in an estimated total heat flux of 10.4 TW, which is consistent with modern ge

109 the question: what mechanism transports the heat flux of a solar luminosity outwards?

110 oom temperature) and the potential to pump a heat flux of up to 700 W cm-2; the localized cooling and

111 e one might assume that these larger surface heat fluxes on the equatorward side would tend to damp t

112 nstabilities in fusion reactors impart large heat fluxes onto the surrounding plasma-facing component

113 t latent heat flux over soybean and sensible heat flux over both crops.

114 oist convection driven by increased sensible heat flux over drier soils, and/or mesoscale variability

115 e-level data for all variables except latent heat flux over soybean and sensible heat flux over both

116 agnetic fields, atmospheric jets and emitted heat flux patterns.

117 ermal energy originating from the individual heat flux processes has changed significantly over the p

118 nd 2011, we evaluate long-term trends in the heat flux processes.

119 verlying air (Tw-Ta) as a proxy for sensible heat flux (QH).

120 s comes from accelerated warming and air-sea heat flux rates within all western boundary currents, wh

121 om seasonal to centennial, natural O(2) flux/heat flux ratios are shown to occur in a range of 2 to 1

122 0 was related to solar radiation, horizontal heat flux, relative humidity, wind speed, soil moisture

123 ir bubble dynamics were examined at elevated heat flux, revealing various nucleate boiling phenomena.

124 ospheric adjustment through changing surface heat fluxes, sea surface height and thermocline depth.

125 lux, and even the one-dimensional energy and heat flux spectra.

126 ar mare basalts, plausibly results in a core heat flux sufficient to power a short-lived lunar dynamo

127 s SST gradient forces large-scale changes in heat flux that exacerbate SEIO heatwaves.

128 , it is predominantly via changes in air-sea heat fluxes that human-induced climate forcings, such as

129 Large latent and sensible heat fluxes that warm the atmosphere and cool the ocean

130 cell surface area is constant suggests that heat flux through the cell surface is effectively instan

131 sult in significant lateral heterogeneity of heat flux through the core-mantle boundary.

132 dels that combine calculations of conductive heat flux through the skin and fur, and convective heat

133 blem may be avoided if reliable estimates of heat flux through the skin of the animals are obtained b

134 the present analysis for latent and sensible heat fluxes, thus consistently integrating the analysis

135 s increase latent at the expense of sensible heat fluxes, thus, drastically reducing Bowen ratios.

136 models for the Moon yield insufficient core heat flux to power a dynamo after approximately 4.2 Gyr

137 Through feedbacks involving latent heat fluxes to the atmosphere and marine stratus clouds,

138 pothesis on this timescale, the evolution of heat-flux variations at the core-mantle boundary, induce

139 I find that a simple pattern of heat-flux variations at the core-mantle boundary, which

140 trong middepth warming and enhanced downward heat flux via vertical mixing.

141 mits of agreement for temperature using zero-heat-flux were 0.19 degrees C +/- 0.53 degrees C compare

142 We find an extraordinary large heat flux which is more than five orders of magnitude la

143 mary production, leaf production, and latent heat flux, which were roughly proportional to canopy los