ライフサイエンスコーパス: heat flux

1 rs with a corresponding decrease in sensible heat flux.

2 e cooling and resultant increase in sensible heat flux.

3 resulting in a ~10% increase in net up-fjord heat flux.

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

5 rculation through its regulation of poleward heat flux.

6 deformed terrain and has an anomalously high heat flux.

7 c Deep Water formation and northward oceanic heat flux.

8 wind speed, barometric pressure, and latent heat flux.

9 y slowing down vertical mixing with a latent heat flux.

10 cal factor impacting LST by adjusting latent heat flux.

11 l directions in response to changes in local heat flux.

12 for the effects of microhabitat buffering on heat flux.

13 ogy will place firmer constraints on Venus's heat flux.

14 tes of subsurface ocean mixing and turbulent heat flux.

15 te regime, exhibits a predominantly positive heat flux.

16 ntle boundary and time-dependent mantle-side heat flux.

17 ream areas primarily due to the large latent heat flux.

18 the transient variability of the net surface heat flux.

19 s such as aerodynamic wind and anthropogenic heat flux.

20 of conventional methods for estimating core heat flux.

21 er throughout the year, which reduces latent heat flux.

22 own to decline monotonically with increasing heat flux.

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

24 electric fields perpendicular to an incident heat flux.

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

26 the partitioning between sensible and latent heat fluxes.

27 rove estimates of the global circulation and heat fluxes.

28 de rather than directly through submesoscale heat fluxes.

29 pecially high for summer sensible and latent heat fluxes.

30 sufficient information to estimate the eddy heat fluxes.

31 nd microfluidics for the control of mass and heat fluxes.

32 sea level changes are controlled by surface heat fluxes.

33 2012-2021 made from parametrized net surface heat fluxes.

34 due to the strong surface winds and air-sea heat fluxes.

35 and climate directly by regulating water and heat fluxes.

36 polygonal structures if we assume a smaller heat flux (~0.3 mW m(-2)) at the base of the ice layer t

37 her Bond albedo (0.41 +/- 0.02) and internal heat flux (2.84 +/- 0.20 Wm(-2)) values than previous es

38 rying oxygen concentrations (0, 14, 21%) and heat fluxes (25, 50 kW/m(2)).

39 variations in forcing or in ocean-atmosphere heat fluxes(5,6).

40 We find that air-sea heat flux accounts almost entirely for the net cooling o

41 e for a strongly elevated vertical diffusive heat flux across the base of the mixed layer in the pres

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

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

44 hough the outer-core convection controls the heat flux across the inner core boundary, the internally

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

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

47 particularly in summer afternoons, but these heat fluxes alone are insufficient for producing the obs

48 mportant implications for constraining total heat flux along mid-ocean ridges and for identifying pre

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

50 he ice-sheet margin, and elevated geothermal heat flux along the Iceland hotspot track inland.

51 he spatiotemporal variability of the air-sea heat fluxes along the region's boundary currents, where

52 We find there is an increase in the air-sea heat fluxes along these currents that is a function of t

53 than two-fold difference in the net surface heat fluxes among the models, and this difference is dom

54 eved a 2.5-fold increase in heat dissipating heat flux and accelerated vapor diffusion from the evapo

55 here, which increases both downward sensible heat flux and downwelling long-wave radiation at the sur

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

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

58 -with prediction errors of less than 20% for heat flux and HTC, and over 98% accuracy in boiling regi

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

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

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

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

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

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

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

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

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

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

69 r results are the first to show that air-sea heat flux and wind stress related processes are importan

70 sential to understanding global chemical and heat fluxes and endemic faunal distributions.

71 odels is thus important for simulating ocean heat fluxes and induced melt rates.

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

73 feedback between latent and sensible surface heat fluxes and SST anomalies.

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

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

76 uctivity would critically influence regional heat-flux and thermochemical evolution around CMB, but r

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

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

79 ce temperature gradient, sensible and latent heat fluxes, and convection during cyclones.

80 s study aims to identify patterns of surface heat fluxes, and corresponding surface ocean responses,

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

82 the ice cover, enhance ocean-ice-atmosphere heat fluxes, and make the ice more susceptible to latera

83 re radiation components, latent and sensible heat fluxes, and meteorological conditions were measured

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

85 ch weakens oceanic stratification, amplifies heat fluxes, and reduces sea ice.

86 On annual timescales, however, air-sea heat flux anomalies are mostly altered by atmospheric va

87 On these timescales, air-sea heat flux anomalies are strongly linked to AMOC-driven n

88 Instead, we find that air-sea heat flux anomalies north of any given latitude in the N

89 are strongly linked to AMOC-driven northward heat flux anomalies through the conservation of energy.

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

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

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

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

94 rate, mass burn rate, flame temperature, and heat flux are found to be easily adjusted by varying the

95 mode is considered when the heat source and heat fluxes are constant.

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

97 l ocean model, we demonstrate that ocean-ice heat fluxes are predominantly induced by localized and i

98 entional gases and plasmas, it is known that heat fluxes are proportional to temperature gradients, w

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

100 the direction and amplitude of eddy-induced heat fluxes are significantly influenced by eddy's asymm

101 ment availability, underlying lithology, and heat flux, are lacking.

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

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

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

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

106 is barrier weakens and lateral exchanges and heat flux between the eddy and the surroundings increase

107 ridional gradients as well and the turbulent heat fluxes between the ocean and the atmosphere.

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

109 that newly frozen leads with large sensible heat flux but low latent heat flux tend to dissipate low

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

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

112 nduced MOC is primarily modulated by surface heat flux changes at lower latitudes and by freshwater f

113 Enhancing critical heat flux (CHF) during boiling with structured surfaces

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

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

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

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

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

119 onducted from natural convection to critical heat flux (CHF), and AE signals were externally collecte

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

121 simulations into a fluid model (through the heat flux closure term) using the Fourier neural operato

122 igher heat transfer coefficient even at high heat flux conditions, in which boiling heat transfer is

123 while the width of the MIZ follows vertical heat flux convergence, but with a three-week lag.

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

125 This warming drives upward heat fluxes, destabilizing the atmospheric boundary laye

126 Our shot noise measurements reveal that heat flux displays a crossover between [Formula: see tex

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

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

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

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

131 In particular, a gradually varying heat flux distribution from the substellar to antistella

132 Land surface heat fluxes do precondition the atmosphere for convectio

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

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

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

136 rror) CABLE's previous predictions of latent heat fluxes during periods of water stress at two eddy c

137 ectly and indirectly through (a) exposure to heat flux (e.g., injuries and destructive impacts), (b)

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

139 ce shelves and modifies vertical and lateral heat fluxes, enhancing heat transport into ice shelf cav

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

141 We found that heat flux estimates generally underestimated metabolic r

142 Heat flux estimates were made using two free convection

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

144 osite can manage one fourth of the metabolic heat flux expected for a sedentary individual and can al

145 ergy to power the geodynamo from core-mantle heat flux, followed by a sharp intensity increase as new

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

147 ds of measuring sensible (H) and latent (LE) heat fluxes for a year over a mixed grass prairie ecosys

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

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

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

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

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

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

154 ishing sea ice, driven in part by changes in heat flux from the North Pacific.

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

156 n primarily be sustained by excessive upward heat flux from the sea surface exposed to air in the reg

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

158 ibute the rapid retreat to an enhanced ocean heat flux from warm Circumpolar Deep Water (CDW) reachin

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

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

161 Increased outgoing longwave radiation and heat fluxes from the newly opened waters cause AA, where

162 also acted to increase the surface winds and heat fluxes from the ocean to the atmosphere.

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

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

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

166 ltaneously predicting key boiling parameters-heat flux, heat transfer coefficient (HTC), and boiling

167 skin is primarily responsible for modulating heat flux; here we evaluate the relative regulation of a

168 vestigate the uncertainties of inputs of the Heat-Flux (HFLUX) model.

169 Simulations of heat flux identified different exposure to warming for b

170 mains unclear how ongoing changes in air-sea heat flux impact this transformation.

171 The HI-P junction rectifies heat flux in a single direction, while the LI-P junction

172 t its heat transfer coefficient and critical heat flux in its "switched-on" state.

173 ther show that a declining northward oceanic heat flux in recent decades, which is linked to this sur

174 nges in surface temperature: the net surface heat flux in the models.

175 ervation-based estimates of the past air-sea heat flux in the North Atlantic from reanalysis products

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

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

178 parameterizations of eddy-induced ice-ocean heat fluxes in climate models.

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

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

181 Previous work has shown a reduction in heat fluxes in the interior of the Nordic Seas.

182 ility of the sea surface temperature and net heat fluxes in the Kuroshio Extension, the most signific

183 thermore, the magnitude and sign of the mean heat fluxes in these regimes differs, which dictates the

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

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

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

187 d meridional heat flux similarly doubles the heat flux induced by the symmetric components, highlight

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

189 Additionally, seasonal variations in latent heat flux intensify the heat release during warmer seaso

190 increased, which, together with the air-sea heat fluxes intensity, constrained the depth of convecti

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

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

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

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

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

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

197 Measuring temperature and heat flux is important for regulating any physical, chem

198 This measured heat flux is more than four times higher than other EC c

199 Availability of excessive heat flux is necessary for the maintenance of this feedb

200 This heat flux is probably due to localized tidal dissipation

201 The increased turbulent heat flux is used to increase air temperature and specif

202 ordic and Barents Seas, triggered by air-sea heat fluxes, is an integral component of the Atlantic Me

203 fusivity ([Formula: see text]) and turbulent heat flux (J[Formula: see text]) in the Western Pacific

204 at transport predict that the nondimensional heat flux, known as the Nusselt number (Nu), is proporti

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

206 gross primary productivity (GPP) and latent heat fluxes (LE) against present-day observations.

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

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

209 plain its estimated Bond albedo and internal heat flux, mainly because previous estimates were based

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

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

212 Newtonian Maxwell type and Cattaneo-Christov heat flux model in parabolic trough solar collectors use

213 dditionally, a non-Fourier Cattaneo-Christov heat flux model is utilized to include thermal relaxatio

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

215 radiative slendering sheet with non-Fourier heat flux model.

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

217 Heat flux models have been used to predict metabolic rat

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

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

220 lenge our view on where and how the on-shelf heat flux occurs, suggesting that it is largest where de

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

222 perature span of 5.2 degrees C and a maximum heat flux of 135 milliwatts per square centimeter.

223 boiling tests exhibited a very high critical heat flux of 289 W/cm(2) at a wall superheat of just 2.2

224 An additional endogenic heat flux of 46 +/- 4 milliwatts per square meter is req

225 re used to estimate the adiabatic conductive heat flux of a molten Fe-14 wt% Si-3 wt% S lunar core an

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

227 owave instruments allow us to measure a peak heat flux of about 180 milliwatts per square metre, whic

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

229 io of ~25 for the transmittance, regulates a heat flux of ~36 W/m(2) with an estimated mechanical pow

230 The enhanced latent and sensible heat fluxes of forests have an average cooling effect of

231 the flow, to investigate the role of air-sea heat flux on the cooling of AW.

232 tal thickness is less than 29 km, unless the heat flux on Venus is less than the radiogenic lower bou

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

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

235 ons were significantly correlated with ocean heat flux, open water area, wind velocity and atmospheri

236 points, including points of locally enhanced heat flux or "hot spots." One conclusion is that the fra

237 nts on the ocean vertical diffusivity or the heat flux originating from the silicate core.

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

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

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

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

242 oling-gas injection eliminates the secondary heat-flux peak created by three-dimensional magnetic lob

243 e heterogeneous amplitude and pattern of CMB heat-flux, potentially impacting geodynamo and geomagnet

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

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

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

247 it and an increase in sensible versus latent heat flux quantified local meteorological response to fo

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

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

250 0 was related to solar radiation, horizontal heat flux, relative humidity, wind speed, soil moisture

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

252 ere we reveal interactions between ocean-ice heat fluxes, sea ice cover, and upper-ocean eddies that

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

254 A Heat Flux Sensor (HFS) facilitates the visualization of

255 he break junction technique with a suspended heat-flux sensor, we measured the total thermal and elec

256 In inhomogeneous bundles, the total heat flux shows dependence on the difference between the

257 The total eddy-induced meridional heat flux similarly doubles the heat flux induced by the

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

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

260 alized study of the long standing problem of heat flux suppression relevant to fusion and cosmic plas

261 with large sensible heat flux but low latent heat flux tend to dissipate low clouds.

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

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

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

265 oosting stratification, and lowering oceanic heat fluxes there after 2007, AD+ contributed to slowing

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

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

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

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

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

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

272 We developed a general model of heat flux to evaluate whether water requirements for eva

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

274 Fjord dynamics influence oceanic heat flux to the Greenland ice sheet.

275 n the convective, radiative, and evaporative heat fluxes to and from the scalp in relation to propert

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

277 n the Nordic Seas, and the site of important heat fluxes to the atmosphere.

278 By applying a range of wildfire heat fluxes to variable peatland fuel mixes, this resear

279 d systems that require large time-integrated heat-fluxes to form.

280 y long (~15 kyr) episode of intense poleward heat flux transport prior to the MIS 11c optimum.

281 However, the shoreward heat flux typically far exceeds that required to match o

282 ay towards an operational monitoring of eddy heat fluxes using satellite altimetry and other remote s

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

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

285 00 km wide plume of high temperature, with a heat flux very much larger than predicted from its swell

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

287 y impacted both sites, the composite surface heat flux was larger at the northern site, especially fo

288 ace coupling on the early Earth, when global heat flux was substantially higher, and the lithosphere

289 in the likely crustal thickness and surface heat flux, we find that quartz-dominated rheologies rela

290 ausible estimates of surface temperature and heat flux, we inferred basal temperatures around 200 K:

291 ned, where the density and the divertor peak heat flux were well controlled, with no core impurity ac

292 The ocean-atmosphere CO(2), momentum, and heat fluxes were each closely correlated with the SST.

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

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

295 coastal waters leads to increased shoreward heat flux, which implies a positive feedback in a warmin

296 s is crucial for determining the net surface heat flux, which in turn affects surface temperature and

297 lls, attributable to a reduction in sensible heat flux, which is unlikely to compromise AAHPs operati

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

299 Divertor detachment reduces steady-state heat flux, while resonant magnetic perturbations can sup

300 ffect SST in the ocean area included surface heat fluxes, wind, and precipitation.