ライフサイエンスコーパス: heat loss

1 owing to more rapid heating rates and lower heat loss.

2 y balancing the rates of heat production and heat loss.

3 ace in a dose-dependent manner, resulting in heat loss.

4 ue provides an insulating layer that impedes heat loss.

5 using SU-8 on a glass wafer to minimize the heat loss.

6 e that had undergone divergent selection for heat loss.

7 r high heat loss and an inbred line with low heat loss.

8 thermoregulate almost exclusively by varying heat loss.

9 ting 20 mm fiberglass insulation to minimize heat loss.

10 ve to their weight and thus marked radiative heat loss.

11 ssary to maintain homeostasis via conductive heat loss.

12 n unprecedented doubling of mid-winter ocean heat loss.

13 jection while inducing negligible additional heat loss.

14 s on the balance between heat production and heat loss.

15 nsparency window so as to minimize parasitic heat losses.

16 radiation it absorbs overwhelms its internal heat losses.

17 with increased insolation, and reduced ocean heat losses.

18 sent observational evidence that the surface heat loss actually strengthens the front during October-

19 s between a noninbred line selected for high heat loss and an inbred line with low heat loss.

20 iciency system-wide, controlling the rate of heat loss and consequent heat production.

21 heasterly trade winds leads to surface ocean heat loss and convective mixing in the northern Arabian

22 5 billion years (Gyr) as a result of surface heat loss and declining radiogenic heat production.

23 rust more than 1 Myr old) results in greater heat loss and fluid flux than that at ridge crests and p

24 result of a dynamically regulated balance of heat loss and gain, which is not reflected by a simple t

25 ) thermogenesis fails to compensate for body heat loss and heart rate declines, infant pups maintain

26 e to body warming, and when active stimulate heat loss and inhibit heat production.

27 But the mechanisms of interior heat loss and resurfacing are currently unclear, as is t

28 to skin and core cooling, thereby enhancing heat loss and the magnitude of the fall in deep body tem

29 ice decline can substantially alter surface heat loss and thus the ocean and atmosphere(6).

30 on BMR to compensate for increased rates of heat loss and to keep T(b) constant(9-12).

31 sulations are typically used to minimize the heat losses and to confine the heat transport through th

32 diated by a lower sweating rate (evaporative heat loss) and reduced skin blood flow (dry heat loss) f

33 transepidermal water loss and transcutaneous heat loss, and have difficulty maintaining homeostasis.

34 ystem designs may be large, particularly the heat loss associated with pilot scale data resulting in

35 dent increase in metabolic rate results from heat loss at ambient temperatures below thermoneutrality

36 e report a strategy of preventing convective heat loss at the gills during excursions into deep, cold

37 pat4(-/-) mice did not result from increased heat loss, because both cold tolerance and response to a

38 increased hypothermia mediated by increased heat loss, but not by heat production, in SHR.

39 ds ~4x faster than predicted from analogy to heat loss by buoyant convection, a theory frequently emp

40 ostly high optical concentrations leading to heat loss by the hot bulk liquid and heated surfaces or

41 me extend it is beneficial to purposely open heat loss channels in order to establish a larger temper

42 s in atmospheric-storm frequency and surface-heat-loss-driven dense water formation, although the imp

43 e passage of severe storms, and that intense heat loss drove deep overturning within them.

44 ntroduce a theoretical model which considers heat losses due to convection and radiation mechanisms,

45 kin resulting in greater skin blood flow and heat loss during cold exposure.

46 recognized as being subjected to substantial heat loss during its transit towards the polar regions.

47 not be accounted for solely by modulation of heat loss effectors, but also involves other mechanisms.

48 from the core to the periphery, followed by heat loss exceeding metabolic heat production.

49 heat loss) and reduced skin blood flow (dry heat loss) for a given core temperature.

50 esents the primary mechanism for substantial heat loss from Atlantic Water in the Lofoten Basin.

51 It revealed that elevated GST and heat loss from basements are dominant factors in the hea

52 al variability, a greater cumulative oceanic heat loss from ENSO thermal damping reduces stratificati

53 , there is a phase shift in the time of peak heat loss from late April to mid-June, with weaker than

54 ation between the tips and the flame reduces heat loss from the flame to the surrounding environment,

55 carcinoma (HCC) by minimizing flow-mediated heat loss from the tumor.

56 However, spontaneous heat loss from thermally charged phase-change materials

57 mperatures (GSTs) at artificial surfaces and heat losses from basements of buildings, sewage systems,

58 mixed layer and a strengthening of winds and heat losses from the ocean, as driven by the low frequen

59 ce where a direct measurement of Enceladus's heat loss has been made is at the south pole.

60 The QTL for heat loss identified on chromosome 1 in the HB populatio

61 e April to mid-June, with weaker than normal heat loss in austral autumn.

62 prostaglandin E(2) production and increased heat loss in conscious rats.

63 ch on average indicate significant advective heat loss in crust up to 65 Myr old.

64 responses were associated with an increased heat loss in SHR compared to Wistar rats.

65 alinity waters in the Levantine and enhanced heat loss in the Aegean Sea, coupled with surface water

66 The implied heat loss in the deep ocean since 1750 CE offsets one-fo

67 pressure of manganese and the more efficient heat loss in the initial layers.

68 lighting nanoplatforms that prevent magnetic heat loss in the intracellular environment.

69 cold water upwelling and weaker surface net heat loss in the north-eastern MDR were the main drivers

70 ose from sea ice expansion and reduced ocean heat losses in the Nordic and Barents seas, driven by a

71 use of MWs compensates better for the strong heat losses in this reaction, associated with the boilin

72 The winter surface-heat-loss intensification is accompanied by substantial

73 ntle convection, which facilitates planetary heat loss, is manifested at the surface as present-day p

74 or low (SL) stress response from high or low heat loss lines of mice, respectively.

75 were created from lines of mice differing in heat loss measured by direct calorimetry as an indicator

76 mammalian brain controls heat generation and heat loss mechanisms that regulate body temperature and

77 respiratory and metabolic rates and reduced heat loss mediated by hiding the head-the body part with

78 ion measurements and calculations based on a heat loss model.

79 In the rat, approximately 20% of total body heat-loss occurs by sympathetically mediated increases i

80 al average of 50 to 100 mW m(-2) and a total heat loss of 7.5 to 15 terawatts.

81 an accurate determination of the building's heat loss or gain can be achieved, enabling planners and

82 energic agonist midodrine, the inappropriate heat loss over their tail surface was reduced, normalizi

83 tive evidence for additional QTL influencing heat loss, percentage subcutaneous fat, and percentage h

84 Maximal evaporative heat loss potential from the scalp is reduced by the pre

85 g that the physiologic response is to reduce heat loss rather than to generate heat.

86 de new insight into the mechanisms governing heat loss responses and suggest that the age-related dim

87 We have identified that autonomic heat loss responses at rest and during fixed-intensity e

88 eating and infer that ET-1 may attenuate the heat loss responses of cutaneous blood flow, but not swe

89 lts, cyclooxygenase (COX) contributes to the heat loss responses of cutaneous vasodilatation and swea

90 hat the age-related diminished COX-dependent heat loss responses reported in previous studies may be

91 e ageing is known to attenuate COX-dependent heat loss responses.

92 tle's radiogenic contribution to the surface heat loss, set limits on the composition of the silicate

93 ooling occurs via convective and evaporative heat loss, so right-to-left shunted blood flow through a

94 her all reactants are consumed or sufficient heat loss stalls further reaction.

95 ng" of wing-like pectoral fins and minimizes heat loss through a series of counter-current heat excha

96 enesis in brown adipose tissue, and regulate heat loss through modulation of peripheral vasoconstrict

97 del simulates turbulent convection caused by heat loss through the fluid surface, for example during

98 as a low midinfrared emissivity can minimize heat loss to surroundings.

99 e an important new source of turbulent ocean heat loss to the atmosphere in wintertime.

100 lower mid-infrared emissivity, which limits heat losses to surroundings, and butterflies from warmer

101 dent literature implies that rodents prevent heat loss via a broad range of behavioral adaptations in

102 sms (i.e., intracerebral heat production and heat loss via skin surfaces) that underlie MDMA-induced

103 The resulting anomalous surface heat loss was asymmetric, with larger changes in norther

104 Evidence for significant QTL influencing heat loss was found on chromosomes 1, 2, 3, and 7.

105 These heat exchangers substantially reduce heat loss when these whales feed in cold waters.

106 Also, we found that to avoid unsustainable heat loss while swimming, bears employed unusual heterot