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1 w to blood by accumulation of albumin in the general circulation.
2 cytokines was detectable (</=5 ng/ml) in the general circulation.
3 on from the gastrointestinal system into the general circulation.
4 e through which hormones are released to the general circulation.
5 rocoagulant cells and enzymes that enter the general circulation.
6 adiation is linked with the atmosphere-ocean general circulation.
7 d the energy input by winds into the oceanic general circulation.
8  the release of bioactive osteocalcin in the general circulation.
9 tics to the local LNs and over time into the general circulation.
10 tters in projection neurons, and through the general circulation.
11 mediators to draining lymph nodes and to the general circulation.
12 to overcome dilution of these signals in the general circulation.
13 f the Asian pollutant outflows on the global general circulation and climate.
14           To investigate the response of the general circulation and global transport of heat through
15 orbed from the lumen of the gut to reach the general circulation and is then distributed to periphera
16 blood-brain barrier, a "barrier" between the general circulation and the CNS.
17 ccurs in the liver before glucose enters the general circulation, and that the glutamate-induced post
18 ospinal fluid contents are distinct from the general circulation because of regulation at brain barri
19  wild-type mice, diabetes reduced PMo in the general circulation but increased by fourfold the absolu
20              We identify an ensemble of five general circulation climate models whose output closely
21 c global vegetation models (DGVMs) driven by general circulation climate models.
22 acific storm track likely impacts the global general circulation due to its fundamental role in merid
23 ive clouds (DCCs) play a crucial role in the general circulation, energy, and hydrological cycle of o
24  analyzed the rate of virus clearance in the general circulation in rhesus macaques receiving a conti
25   We demonstrate how recent atmosphere-ocean general circulation model (AOGCM) simulations of the cli
26 tudied using an atmosphere and ocean coupled general circulation model (AOGCM).
27 odel Intercomparison Project phase 6 (CMIP6) General Circulation Model (GCM) ensemble output.
28 differing climatic conditions generated by a general circulation model (GCM) in "normal" and "hosing"
29 gional climate models (RCMs) are driven with general circulation model (GCM) output--to produce fine-
30 ed a heat map approach along with downscaled general circulation model (GCM) projections of warming a
31  us to calibrate individual ice cores, prior general circulation model (GCM) studies have supported t
32 We first use simulations with an atmospheric general circulation model (GCM) that explicitly simulate
33 of Andean surface uplift with an atmospheric general circulation model (GCM) that tracks oxygen isoto
34 rd Institute for Space Studies (GISS) ModelE General Circulation Model (GCM) to the regional scale us
35                            Using an advanced general circulation model (GCM), we demonstrate that an
36 rid-box-scale temperature projections from a general circulation model (HadCM3).
37 ce ocean Hg inputs and losses using an ocean general circulation model (MITgcm) and an atmospheric ch
38  We have incorporated HR into an atmospheric general circulation model (the National Center for Atmos
39 mmer temperature changes by the NCAR CCSM4.0 general circulation model across the Arctic.
40              Comparisons of the data using a general circulation model and a simpler isotopic distill
41 Here we use a fully coupled atmosphere-ocean general circulation model and an ice-sheet model to asse
42 hio current in the North Pacific sector of a general circulation model and dimensional reduction of a
43 EOS-Chem model coupled to meteorology from a general circulation model and focus on impacts to northe
44 ic growth of the inorganic sea salt within a general circulation model and show that a reduced hygros
45 member grand ensemble of simulations using a general circulation model and thereby explicitly resolvi
46 th Atlantic TC activity using the HadGEM2-ES general circulation model and various TC identification
47 r one representative concentration pathway x general circulation model combination, such uncertaintie
48 and high-resolution versions of the CMCC-CM2 General Circulation Model contributing to the HighResMIP
49  MLD and chlorophyll simulated with an Ocean General Circulation Model coupled to a biogeochemistry m
50 ns with NSIPP1 (version 1 of the atmospheric general circulation model developed at NASA's Goddard Sp
51        Both observations and the atmospheric general circulation model experiments suggest that the p
52               Using the eddy-resolving Ocean General Circulation Model for the Earth Simulator, we ge
53                            In an atmospheric General Circulation Model forced by observed sea surface
54  oceans is ~300 y in an ice-atmosphere-ocean general circulation model in Cryogenian paleogeography.
55                                          Our general circulation model outcomes did not reveal thresh
56                             Using downscaled general circulation model output, we calculate a WNV vec
57   Climate forecasts from an Atmosphere-Ocean General Circulation Model projected increased male widow
58                          Simulations using a general circulation model reproduce the essential featur
59 th simulations of a coupled ocean-atmosphere general circulation model shows that both natural and an
60 ere we analyse a series of transient Coupled General Circulation Model simulations forced by changes
61                                   Subsequent general circulation model simulations show that the Sout
62 s demonstrated in a hierarchy of atmospheric general circulation model simulations with altered radia
63 tion (EKF400v2), which uses atmospheric-only general circulation model simulations with assimilated o
64                                          Our general circulation model simulations, which take into a
65                  Results from an atmospheric general circulation model support this interpretation an
66         Results from a coupled sea ice-ocean general circulation model supported this hypothesis when
67 nse to this melt water pulse using a coupled general circulation model that explicitly tracks water i
68 Simulation results using an atmosphere-ocean general circulation model that includes estimates of the
69                                            A general circulation model that simulated changes in sola
70                  We used an isotope-equipped general circulation model to assess the influence of cha
71                            Using a numerical general circulation model to estimate moist static energ
72  simulations with a coupled atmosphere-ocean general circulation model to identify the impacts of for
73                                    We used a general circulation model to show that the highest-eleva
74 wn in observational data and reproduced in a general circulation model where it increases with decrea
75 owth of the East Antarctic Ice Sheet using a general circulation model with coupled components for at
76 fically, we couple paleoclimatic data from a general circulation model with estimates of relative pas
77        Here, we use an isotope-enabled ocean general circulation model with realistic geometry and fo
78    Our suite of DO events, simulated using a general circulation model, accurately captures the ampli
79 non was reproduced successfully by a coupled general circulation model, Flexible Global Ocean-Atmosph
80      Here we present predictions from a Mars general circulation model, indicating that the observed
81         When we combine these results with a general circulation model, some of the simulations resul
82  present in a fully coupled atmosphere-ocean general circulation model, subject to a freshwater hosin
83 lation and Climate of the Ocean-Darwin ocean-general circulation model, surface alkalinity and dissol
84                        Here we show, using a general circulation model, that substantially more sea-i
85 l satellite observations of isotopes using a general circulation model, then investigate the impacts
86            Here I present simulations with a general circulation model, using elevated carbon dioxide
87                                      Using a general circulation model, we demonstrate that VHS 1256B
88                               An atmospheric general circulation model, which assimilates data from d
89 echanism using simulations with an idealized general circulation model, with which we show that the e
90 easing surface nutrient drawdown in an ocean general circulation model.
91  failed El Nino using salinity from an ocean general circulation model.
92 tion, regional climate model nested within a general circulation model.
93 e using both a conceptual model and an ocean general circulation model.
94           Through semi-idealized Atmospheric General-Circulation-Model experiments, we show that the
95 hich is consistent with leaf physiognomy and general-circulation-model temperature estimates for the
96    We used output from four atmosphere-ocean general circulation models (AOGCMs; CCSM4, HadGEM2-CC, M
97 elie, Antarctica and projections of SIE from General Circulation Models (GCM) of Earth's climate incl
98                         Output from numerous General Circulation Models (GCMs) also exhibits positive
99 ns of uncertainty contained in both multiple general circulation models (GCMs) and multi-parameter en
100   A long-standing discrepancy exists between general circulation models (GCMs) and satellite observat
101  projected under five different global-scale General Circulation Models (GCMs) and two Representative
102                                              General circulation models (GCMs) are the foundation of
103                                              General circulation models (GCMs) are the tool for predi
104  The precipitation and temperature data from General Circulation Models (GCMs) for different Shared S
105 e show that most of the latest generation of general circulation models (GCMs) from the sixth phase o
106 erefore of great concern, especially as some general circulation models (GCMs) predict a severe dryin
107                                     However, general circulation models (GCMs) predict future increas
108  concentrations of atmospheric CO2, high-end general circulation models (GCMs) simulate an accumulati
109 odel Intercomparison Project Phase 5 (CMIP5) general circulation models (GCMs) suggest that warmer wi
110 the initial step involves analyzing eighteen General Circulation Models (GCMs) to identify the most s
111 tomology model with climate projections from general circulation models (GCMs) to predict changes in
112 g coarse resolution climate simulations from General Circulation Models (GCMs) to project future clim
113 rojections for the species based on multiple general circulation models (GCMs), emission scenarios, a
114                                              General circulation models (GCMs), forced by sea surface
115 al period by an ensemble average of multiple general circulation models (GCMs).
116                     Results from two oceanic general circulation models (OGCMs), forced by observed w
117 recipitation predictions from five different general circulation models and atmospheric CO2 concentra
118 s important to include both atmospheric only general circulation models and earth system Models in en
119 g climatic velocities derived from different general circulation models and emissions pathways was le
120        Using two presence-only models, seven General Circulation Models and four emission scenarios,
121                                 We integrate general circulation models and geological observations t
122 is significantly overestimated in most ocean general circulation models and simpler box models previo
123                              Variation among General Circulation Models and Species Distribution Mode
124  the ocean, and they suggest that most ocean general circulation models are overestimating oceanic an
125               We use downscaled outputs from general circulation models coupled with a hydrologic mod
126                                              General circulation models explain this dichotomy, predi
127                                              General circulation models have generally excluded the f
128 2005 and 2091-2100) from 29 Atmosphere-Ocean General Circulation Models implemented under CMIP5.
129 on the mean circulation by resolved waves in general circulation models is not yet converging.
130 the ECHAM-4 model, implying that atmospheric general circulation models like ECHAM-4 can successfully
131 demonstrated in a number of simulations with general circulation models of the coupled ocean-atmosphe
132                                              General circulation models predict temperature differenc
133                                       Oceans general circulation models predict that global warming m
134                                 TC-resolving general circulation models project a 36% increase in the
135                                  Atmospheric general circulation models represent aerosol-cloud inter
136 es to future climate simulated by a range of general circulation models run under all four representa
137 mprovement Project, and driven by outputs of general circulation models run under representative conc
138                                              General circulation models show that as the surface temp
139  C), using a multi-model ensemble of coupled general circulation models subjected to anthropogenic fo
140      Our simulations with 2 ocean-atmosphere general circulation models suggest that observed cyclic
141                                      Current general circulation models suggest that the increase in
142 t 10 years, major advances have been made in general circulation models that include water isotopes,
143 ave-driven mixing parameterization for ocean general circulation models that is entirely physics-base
144         Here, we use atmospheric and oceanic general circulation models that reproduce ENSO asymmetri
145 hypothesis with the output of an ensemble of general circulation models to project the poleward range
146                                  Atmospheric general circulation models used for climate simulation a
147     Using large ensembles from seven coupled general circulation models with a total of 414 model run
148 sions; Geophysical Fluid Dynamics Laboratory General Circulation Models) on total forest C, tree spec
149  is supported by simulation experiments with general circulation models, additional support from fiel
150 nants for plant water use efficiency and for general circulation models, but a mechanistic understand
151 his time has been simulated with atmospheric general circulation models, but these relatively coarse
152 tion of four sources of variation (choice of general circulation models, emission scenarios and speci
153 les in the Amazon remain poorly simulated in general circulation models, exhibiting peak evapotranspi
154 CP4.5), and pessimistic (RPC8.5)-using three General Circulation Models, for the period 2061-2080.
155                                              General circulation models, however, simulate SST variab
156                                  Traditional general circulation models, or GCMs-that is, three-dimen
157                Consistent with comprehensive general circulation models, our results explain why mean
158                         Using an ensemble of general circulation models, we find a robust increase in
159 ts and statistical downscaling from IPCC AR4 general circulation models, we project that gray snapper
160 sed variability in rainfall, a prediction of general circulation models, were assessed in native gras
161                        But the resolution of general circulation models, which are traditionally used
162 te change because they have not been seen in general circulation models.
163 e hitherto only been possible with expensive general circulation models.
164 ll patterns of response predicted by several general circulation models.
165 centration pathways (RCPs) according to five general circulation models.
166 models or the comparison of predictions from general circulation models.
167 ries of greenhouse gas emissions, using five general circulation models.
168  challenges conventional projections made by general circulation models.
169  interpretation of optical phase curves with general circulation models.
170 els and climate projections for 2030 from 20 general circulation models.
171 hat baroclinic instability is central to the general circulation of icy moons.
172 teins have been found in soluble form in the general circulation of patients with atherosclerosis.
173 ntitatively by comparison with models of the general circulation of the Earth's mantle.
174 c delivery of drugs after injection into the general circulation or lymphatic systems.
175          The fact that MGP is present in the general circulation raises the question of whether ECMM
176 ctures may be sites of GnRH release into the general circulation since these structures were observed
177  site and reducing the concentrations in the general circulation, thereby avoiding off-target toxic e
178 s the intestinal portal vasculature with the general circulation, using a diverse array of immune cel
179 l gland during the night and released to the general circulation, where it reaches nanomolar concentr
180    Wind is the primary driver of the oceanic general circulation, yet the length scales at which this

 
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