ライフサイエンスコーパス: general circulation

1 cytokines was detectable (</=5 ng/ml) in the general circulation.

2 on from the gastrointestinal system into the general circulation.

3 rocoagulant cells and enzymes that enter the general circulation.

4 tics to the local LNs and over time into the general circulation.

5 tters in projection neurons, and through the general circulation.

6 mediators to draining lymph nodes and to the general circulation.

7 to overcome dilution of these signals in the general circulation.

8 w to blood by accumulation of albumin in the general circulation.

9 f the Asian pollutant outflows on the global general circulation and climate.

10 orbed from the lumen of the gut to reach the general circulation and is then distributed to periphera

11 blood-brain barrier, a "barrier" between the general circulation and the CNS.

12 ccurs in the liver before glucose enters the general circulation, and that the glutamate-induced post

13 We identify an ensemble of five general circulation climate models whose output closely

14 acific storm track likely impacts the global general circulation due to its fundamental role in merid

15 ive clouds (DCCs) play a crucial role in the general circulation, energy, and hydrological cycle of o

16 analyzed the rate of virus clearance in the general circulation in rhesus macaques receiving a conti

17 We demonstrate how recent atmosphere-ocean general circulation model (AOGCM) simulations of the cli

18 tudied using an atmosphere and ocean coupled general circulation model (AOGCM).

19 differing climatic conditions generated by a general circulation model (GCM) in "normal" and "hosing"

20 gional climate models (RCMs) are driven with general circulation model (GCM) output--to produce fine-

21 ed a heat map approach along with downscaled general circulation model (GCM) projections of warming a

22 us to calibrate individual ice cores, prior general circulation model (GCM) studies have supported t

23 We first use simulations with an atmospheric general circulation model (GCM) that explicitly simulate

24 of Andean surface uplift with an atmospheric general circulation model (GCM) that tracks oxygen isoto

25 rd Institute for Space Studies (GISS) ModelE General Circulation Model (GCM) to the regional scale us

26 rid-box-scale temperature projections from a general circulation model (HadCM3).

27 ce ocean Hg inputs and losses using an ocean general circulation model (MITgcm) and an atmospheric ch

28 We have incorporated HR into an atmospheric general circulation model (the National Center for Atmos

29 mmer temperature changes by the NCAR CCSM4.0 general circulation model across the Arctic.

30 Comparisons of the data using a general circulation model and a simpler isotopic distill

31 Here we use a fully coupled atmosphere-ocean general circulation model and an ice-sheet model to asse

32 hio current in the North Pacific sector of a general circulation model and dimensional reduction of a

33 EOS-Chem model coupled to meteorology from a general circulation model and focus on impacts to northe

34 ic growth of the inorganic sea salt within a general circulation model and show that a reduced hygros

35 member grand ensemble of simulations using a general circulation model and thereby explicitly resolvi

36 th Atlantic TC activity using the HadGEM2-ES general circulation model and various TC identification

37 r one representative concentration pathway x general circulation model combination, such uncertaintie

38 MLD and chlorophyll simulated with an Ocean General Circulation Model coupled to a biogeochemistry m

39 ns with NSIPP1 (version 1 of the atmospheric general circulation model developed at NASA's Goddard Sp

40 Using the eddy-resolving Ocean General Circulation Model for the Earth Simulator, we ge

41 In an atmospheric General Circulation Model forced by observed sea surface

42 Our general circulation model outcomes did not reveal thresh

43 Using downscaled general circulation model output, we calculate a WNV vec

44 Simulations using a general circulation model reproduce the essential featur

45 th simulations of a coupled ocean-atmosphere general circulation model shows that both natural and an

46 ere we analyse a series of transient Coupled General Circulation Model simulations forced by changes

47 Subsequent general circulation model simulations show that the Sout

48 s demonstrated in a hierarchy of atmospheric general circulation model simulations with altered radia

49 Our general circulation model simulations, which take into a

50 Results from an atmospheric general circulation model support this interpretation an

51 Results from a coupled sea ice-ocean general circulation model supported this hypothesis when

52 nse to this melt water pulse using a coupled general circulation model that explicitly tracks water i

53 Simulation results using an atmosphere-ocean general circulation model that includes estimates of the

54 A general circulation model that simulated changes in sola

55 Using a numerical general circulation model to estimate moist static energ

56 simulations with a coupled atmosphere-ocean general circulation model to identify the impacts of for

57 owth of the East Antarctic Ice Sheet using a general circulation model with coupled components for at

58 Here, we use an isotope-enabled ocean general circulation model with realistic geometry and fo

59 non was reproduced successfully by a coupled general circulation model, Flexible Global Ocean-Atmosph

60 Here we present predictions from a Mars general circulation model, indicating that the observed

61 When we combine these results with a general circulation model, some of the simulations resul

62 present in a fully coupled atmosphere-ocean general circulation model, subject to a freshwater hosin

63 Here we show, using a general circulation model, that substantially more sea-i

64 Here I present simulations with a general circulation model, using elevated carbon dioxide

65 An atmospheric general circulation model, which assimilates data from d

66 echanism using simulations with an idealized general circulation model, with which we show that the e

67 tion, regional climate model nested within a general circulation model.

68 e using both a conceptual model and an ocean general circulation model.

69 easing surface nutrient drawdown in an ocean general circulation model.

70 hich is consistent with leaf physiognomy and general-circulation-model temperature estimates for the

71 We used output from four atmosphere-ocean general circulation models (AOGCMs; CCSM4, HadGEM2-CC, M

72 elie, Antarctica and projections of SIE from General Circulation Models (GCM) of Earth's climate incl

73 projected under five different global-scale General Circulation Models (GCMs) and two Representative

74 General circulation models (GCMs) are the tool for predi

75 erefore of great concern, especially as some general circulation models (GCMs) predict a severe dryin

76 However, general circulation models (GCMs) predict future increas

77 concentrations of atmospheric CO2, high-end general circulation models (GCMs) simulate an accumulati

78 odel Intercomparison Project Phase 5 (CMIP5) general circulation models (GCMs) suggest that warmer wi

79 tomology model with climate projections from general circulation models (GCMs) to predict changes in

80 g coarse resolution climate simulations from General Circulation Models (GCMs) to project future clim

81 General circulation models (GCMs), forced by sea surface

82 al period by an ensemble average of multiple general circulation models (GCMs).

83 Results from two oceanic general circulation models (OGCMs), forced by observed w

84 recipitation predictions from five different general circulation models and atmospheric CO2 concentra

85 g climatic velocities derived from different general circulation models and emissions pathways was le

86 Using two presence-only models, seven General Circulation Models and four emission scenarios,

87 is significantly overestimated in most ocean general circulation models and simpler box models previo

88 Variation among General Circulation Models and Species Distribution Mode

89 the ocean, and they suggest that most ocean general circulation models are overestimating oceanic an

90 We use downscaled outputs from general circulation models coupled with a hydrologic mod

91 General circulation models explain this dichotomy, predi

92 General circulation models have generally excluded the f

93 2005 and 2091-2100) from 29 Atmosphere-Ocean General Circulation Models implemented under CMIP5.

94 the ECHAM-4 model, implying that atmospheric general circulation models like ECHAM-4 can successfully

95 demonstrated in a number of simulations with general circulation models of the coupled ocean-atmosphe

96 Oceans general circulation models predict that global warming m

97 Atmospheric general circulation models represent aerosol-cloud inter

98 es to future climate simulated by a range of general circulation models run under all four representa

99 mprovement Project, and driven by outputs of general circulation models run under representative conc

100 General circulation models show that as the surface temp

101 Current general circulation models suggest that the increase in

102 hypothesis with the output of an ensemble of general circulation models to project the poleward range

103 Atmospheric general circulation models used for climate simulation a

104 sions; Geophysical Fluid Dynamics Laboratory General Circulation Models) on total forest C, tree spec

105 is supported by simulation experiments with general circulation models, additional support from fiel

106 nants for plant water use efficiency and for general circulation models, but a mechanistic understand

107 his time has been simulated with atmospheric general circulation models, but these relatively coarse

108 tion of four sources of variation (choice of general circulation models, emission scenarios and speci

109 les in the Amazon remain poorly simulated in general circulation models, exhibiting peak evapotranspi

110 CP4.5), and pessimistic (RPC8.5)-using three General Circulation Models, for the period 2061-2080.

111 General circulation models, however, simulate SST variab

112 Using an ensemble of general circulation models, we find a robust increase in

113 ts and statistical downscaling from IPCC AR4 general circulation models, we project that gray snapper

114 sed variability in rainfall, a prediction of general circulation models, were assessed in native gras

115 But the resolution of general circulation models, which are traditionally used

116 ries of greenhouse gas emissions, using five general circulation models.

117 e hitherto only been possible with expensive general circulation models.

118 ll patterns of response predicted by several general circulation models.

119 models or the comparison of predictions from general circulation models.

120 challenges conventional projections made by general circulation models.

121 interpretation of optical phase curves with general circulation models.

122 els and climate projections for 2030 from 20 general circulation models.

123 te change because they have not been seen in general circulation models.

124 teins have been found in soluble form in the general circulation of patients with atherosclerosis.

125 ntitatively by comparison with models of the general circulation of the Earth's mantle.

126 c delivery of drugs after injection into the general circulation or lymphatic systems.

127 The fact that MGP is present in the general circulation raises the question of whether ECMM

128 ctures may be sites of GnRH release into the general circulation since these structures were observed