ライフサイエンスコーパス: storm

1 ding to a potentially catastrophic "cytokine storm".

2 tochastic optical reconstruction microscopy (STORM).

3 me (RI storms) and those that do not (non-RI storms).

4 ther measured abiotic factors (nutrients and storms).

5 inflammatory response typified by a cytokine storm.

6 elevant motion is dissipated in the Brownian storm.

7 ted in an elevated pro-inflammatory cytokine storm.

8 aken the study of lineage diversification by storm.

9 s stronger mixing and heavier rain under the storm.

10 e Caribbean and quickly took the Americas by storm.

11 pisodes and only 1 patient with recurrent VT storm.

12 in BALB/c mice was accompanied by a cytokine storm.

13 km 5-day circumvention of a severe tornadic storm.

14 th radii during the 28 June 2013 geomagnetic storm.

15 to be an important charging mechanism of the storm.

16 barrier disruption and uncontrolled cytokine storm.

17 cular permeability, likely due to a cytokine storm.

18 rs implicated in the TSS-associated cytokine storm.

19 ence probability and strength during oceanic storms.

20 are not very rare compared with less intense storms.

21 g seedlings are physically removed by winter storms.

22 e vast majority (79%) of major storms are RI storms.

23 and are associated primarily with convective storms.

24 anges in the precipitation produced by these storms.

25 Few non-RI storms (6%) become major storms.

26 er coinciding with naturally occurring large storms.

27 nked to the tallest, most intense convective storms.

28 cs, and the frequency and magnitude of large storms.

29 itudes up to 60 kilometres during major dust storms.

30 uxes of sediment triggered by earthquakes or storms.

31 od on average and can reach 100% during peak storms.

32 unding coasts from potentially more powerful storms.

33 ast and compare the deposits of tsunamis and storms.

34 Few non-RI storms (6%) become major storms.

35 ry disease (41% versus 13%; P=0.001), and VT storm (77% versus 43%; P=0.002); had more severe heart f

36 hastic optical reconstruction microscopy (SR-STORM), achieved cross-talk-free three-dimensional (3D)

37 nt) to accurately assess long-term trends in storm activity.

38 Patients with refractory arrhythmic storm admitted between January 2005 and March 2015.

39 e, by imaging through a diffraction grating, STORM algorithms can be modified to extract a full SERS

40 tochastic Optical Reconstruction Microscopy (STORM) algorithms for super-resolved imaging.

41 ea level, as well as increasing frequency of storms, all of which can profoundly impact marine ecosys

42 Three patients (2.9%) died (1 electrical storm and 2 noncardiovascular deaths).

43 territories >24 hr before the arrival of the storm and atmospheric variation associated with it.

44 ients with intractable refractory arrhythmic storm and cardiogenic shock despite optimal medical ther

45 eter ablation is effective in terminating VT storm and eliminating >/=1 inducible VT in the majority

46 Thyroid storm and hyperthyroidism in pregnancy and during the po

47 thetic antenna complex in cyanobacteria, for STORM and SIM imaging.

48 hey are the oceanic analogues of atmospheric storms and are effective transporters of heat, nutrients

49 We examined the association between dust storms and county-level non-accidental mortality in the

50 used to study the relationship between dust storms and daily mortality counts over the whole United

51 The association between dust storms and daily non-accidental mortality in the United

52 to precipitation distribution, such as small storms and dry spell length (DSL), rather than the total

53 ET/P, and summer AET/P, growing season small storms and DSL partially explained growth.

54 tantly "redesigned" to respond to individual storms and evolving land uses.

55 of two decades of data, we find that violent storms and hurricanes contribute less than 1% to long-te

56 hts, heat waves, frosts, precipitation, wind storms and other climate extremes may impact the structu

57 e simulation and prediction of extratropical storms and other extreme events, as well as in the proje

58 l(-) and conductivity associated with winter storms and subsequent melting events, despite the degree

59 ere is sensitive to magnetospheric activity (storms and substorms).

60 rinsic resistance of salt marshes to violent storms and their predictable erosion rates during modera

61 ar how resistant salt marshes are to extreme storms and whether they can survive multiple events with

62 his possibility by super-resolution imaging (STORM) and found that tissues with distinct transcriptio

63 tochastic Optical Reconstruction Microscopy (STORM) and Structured Illumination Microscopy (SIM) have

64 se that undergo RI during their lifetime (RI storms) and those that do not (non-RI storms).

65 h 20 species detected exclusively before the storm, and eight species detected exclusively after.

66 ive pulmonary disease), presentation with VT storm, and use of general anesthesia.

67 Dust storms are associated with increases in lagged non-accid

68 The model also predicts that the NE Atlantic storms are capable of producing boulderites that, when s

69 Owing to recent climate changes, dust storms are increasingly common, particularly in the Midd

70 hat, even in regions where severe convective storms are representative extreme weather events, the he

71 The vast majority (79%) of major storms are RI storms.

72 Sahelian storms are some of the most powerful on the planet, and

73 Microorganisms carried by dust storms are transported through the atmosphere and may af

74 ncrease in severity and frequency of similar storms as anthropogenic climate change progresses, under

75 nia, and septicemia and averted the cytokine storm associated with septic infection but had no effect

76 roughout northeastern Europe; delayed winter storms associated with polar warming have led to later w

77 HD who underwent CSD for refractory VT or VT storm at 5 international centers were analyzed by the In

78 t-side asymmetric blooming shortly after the storms, attributed previously to sub-mesoscale re-strati

79 onical functions to regulation of eicosanoid storm, autophagy, and metabolism.

80 With the progression of the storm, the storm-borne bacterial community showed increasing resemb

81 t of Asian, Saharan, Arabian, and Australian storms, but there has been no recent population-level ep

82 This "genomic storm" can lead to poor outcomes, including Multiple Org

83 ll compartment, high viremia, and a cytokine storm characterize the early days after HIV infection.

84 transport at event scales, and an objective storm classification indicates that this pathway account

85 When potential storm climatology change over the 21st century is also a

86 Here we demonstrate SERS and STORM combined in this way for super-resolved chemical i

87 (RDPs) had earlier and more robust cytokine storms, compared with slow disease progressors (SDPs) (4

88 A recently offered psychosocial perfect storm conceptual model hypothesizes amplified risk will

89 e initial support for a psychosocial perfect storm conceptual model; the confluence of depressive sym

90 ports of inorganic N losses after severe ice-storm damage within the study watershed.

91 taken from the U.S. National Weather Service storm database.

92 field data to argue that this is a cliff-top storm deposit (CTSD).

93 oisotope detection techniques to examine the storm-deposited layer formed in the seawater near the pa

94 ved to contribute to the pathogenic cytokine storm described in severe dengue patients, but the preci

95 plantable cardioverter-defibrillator, and VT storm despite greater antiarrhythmic drug use (P<0.01).

96 scosity, winter calm and summer (iceberg and storm) disturbance and resources.

97 Dust storms do not seem to be an important vector for transpo

98 ding to plasmaspheric erosion as geomagnetic storms do, substorms initiated on the nightside of the E

99 f the N/P stoichiometry of net inputs versus storm drain exports implicated denitrification or leachi

100 High P exports in storm drainage networks and yard waste resulted in net P

101 re compounded by its facilitated routing via storm drains, ditches, and flood channels.

102 ent from vegetated landscapes to streets and storm drains.

103 t-rich leaf litter onto streets connected to storm drains.

104 ger bunches and diminished plant toppling in storms, due to less root damage.

105 suggesting the faster and stronger cytokine storm during AHI could promote disease progression.

106 Geologic evidence for extreme coastal storms during past warm periods has the potential to pro

107 record somewhere each winter.A succession of storms during the 2013-2014 winter led to record floodin

108 Two storms each produced two jets with characteristics not d

109 analyzed sectors-agriculture, crime, coastal storms, energy, human mortality, and labor-increases qua

110 We conclude that dust storms enrich the ambient airborne microbiome with new s

111 fy potential temporal patterns of electrical storm (ES), in which a cluster of ventricular tachycardi

112 tochastic optical reconstruction microscopy (STORM), etc.] has evolved remarkably over the last decad

113 fected by both intensity and duration of the storm event.

114 We suggest that hydrologic events such as storm events and surface snowmelt runoff destabilize sma

115 spended sediment-discharge hysteresis during storm events is commonly used to indicate dominant sedim

116 negligible greenhouse gas production during storm events.

117 and super-resolved fluorescence microscopy (STORM) experiments, we determined that the average persi

118 ntensive farming and weather events, such as storms, flash flooding, and landslides, contribute estro

119 etween increased rates of sea level rise and storm flood heights.

120 ncreasing water shortage, provides a perfect storm for a new era of environmental crises and potentia

121 of a developing country created the "perfect storm" for sustained endemicity of these multidrug-resis

122 umber of days favorable to severe convective storm formation over the Great Lakes, particularly in th

123 Storms from different dust origins exhibited distinct ba

124 results show, for the first time, that dust storms from different sources display distinct bacterial

125 of dust-borne bacterial communities in dust storms from three distinct origins (North Africa, Syria

126 s concerns how lightning is initiated inside storms, given the absence of physical conductors.

127 pitation, vapor pressure deficit, and summer storms had direct effects on summer AET/P, and summer AE

128 three of the six known giant planetary-scale storms have developed in it.

129 In winter 2013/14 a succession of storms hit the UK leading to record rainfall and floodin

130 bserved in the Little Rouge Creek throughout storm hydrographs, with an occasional first flush occurr

131 STORM identified specific markers on the desired epitope

132 omophore, matched the lines in reconstructed STORM images.

133 his method offers significant advantages: 1) STORM imaging affords 20-nm resolution in the xy-plane a

134 STORM imaging of these densely labeled ultrastructures r

135 nuclear pore complex (NPC) and used them in STORM imaging to locate individual NPC proteins with <2

136 ta sets similar to those obtained in PALM or STORM imaging, SRRF achieves resolutions approaching tho

137 tochastic optical reconstruction microscopy (STORM) imaging revealed the structure of dynamic membran

138 of Kupffer cells and the following cytokine storm.IMPORTANCE Immunocompromised human patients can de

139 121 (54%) and was associated with electrical storm in 22 (18%).

140 5+/-9 years; ejection fraction, 34+/-12%; VT storm in 36%).

141 9%; cardiogenic shock in 23%, and electrical storm in 62% of patients) undergoing 74 unstable VT cath

142 s abolished >/=1 inducible VT and terminated storm in 69% and 74% of patients, respectively, although

143 d >/=1 inducible VT in 90% and eliminated VT storm in 78% of patients; however, multiple residual VTs

144 interventions aimed at controlling cytokine storm in AHI may be beneficial to slow eventual disease

145 on assemblages before and after the 2008 ice storm in China, combined with interspecific interactions

146 endothelial barrier disruption and cytokine storm in experimental lung injury.

147 he fields of cell biology and dermatology by storm in providing the first credible evidence that kera

148 USA, caused by an intense period of tropical storms in autumn 2011.

149 n-level epidemiological research on the dust storms in North America.

150 es these models with a database of synthetic storms in Ocean County and estimates a 16% average reduc

151 d does not preclude the impacts of localised storms in sandsheet emplacement or that tsunamigenic ear

152 during spring runoff, and also during autumn storms in the catchment with the large wetland.

153 change have increased the frequency of dust storms in the Middle East.

154 ced [HONO]/[NO2] ratios observed during dust storms in urban areas.

155 -borne disease is characterized by "abortion storms" in ruminants and by hemorrhagic fever, encephali

156 among livestock, characterized by "abortion storms" in which spontaneous abortion occurs in almost 1

157 Tochastic Optical Reconstruction Microscopy (STORM) in mouse cells.

158 Dust storm incidence data, including date and approximate loc

159 The violent winds of these storms induce deep mixing of the upper ocean, resulting

160 o measure responses of lizard populations to storm-induced selection.

161 mpath) and severe (such as TGN1412) cytokine storm-inducing drugs.

162 s-such as temperature, rainfall, and violent storms-influence the nature of societies and the perform

163 foraging behaviours, we disentangled whether storm influences avian reassembly directly via functiona

164 coastal baroclinic processes in forecasts of storm intensity and impacts will be increasingly critica

165 er erosional energy, even without changes in storm intensity.

166 old the key to understanding how the genomic storm is initiated and may lead to a new understanding o

167 mmatory cytokines, but whether this cytokine storm is the main cause of fatality or is a consequence

168 Temperature-Related Incidence of Electrical Storm) is a patient-level, pooled analysis of previously

169 ity of the LMI distribution means that major storms (LMI >96 kt) are not very rare compared with less

170 t likely by reducing TLR4-dependent cytokine storm mediated by damage-associated molecular patterns (

171 A globally important group of intense storms-mesoscale convective systems (MCSs)-poses a parti

172 Furthermore, using super-resolution STORM microscopy, we revealed eukaryotic ribosomes in CB

173 gh-resolution confocal and super-resolution (STORM) microscopy in AD-like mice and human AD tissue.

174 (VTs; cycle lengths, 230-740 ms, arrhythmic storm n=28) and 2 ventricular fibrillation triggers were

175 Thus, superantigens induce a cytokine storm not only by mediating the interaction between MHC-

176 wer pathogenicity by preventing the cytokine storm observed in EBOV infection.

177 Electrical storm occurred in 4 subjects (2.3%).

178 9 procedures, and a ventricular fibrillation storm occurred within 24 hours of ablation in a single p

179 downstream signaling pathways to inhibit the storm of inflammation typically elicited by bacterial LP

180 acterizing the dust-borne microbiome in dust storms of different origins or that followed different t

181 hat such boulders must have been emplaced by storms of greater-than-historical intensity.

182 have been transported by waves generated by storms of historical intensity.

183 d also interacts with climate change-induced storms of increasing severity to eject debris into the o

184 mputational approach to predict 'the perfect storm' of hormone concentration, IKr block and sympathet

185 The impact of dust storms on human health has been studied in the context o

186 ns, indicate more frequent or intense winter storms on the California coast.

187 We evaluated the impact of Saharan dust storms on the local airborne microbiome in a city in the

188 er radar observations of approximately 2,000 storms, on average, each summer that reach the altitude

189 f magnitude lower than methods such as PALM, STORM or STED.

190 The severe geomagnetic effects of solar storms or coronal mass ejections (CMEs) are to a large d

191 dia within 24 hours (ventricular tachycardia storm), or appropriate ICD shock.

192 ry outcome of death, ventricular tachycardia storm, or appropriate ICD shock among patients undergoin

193 eteors and moisture are lifted by convective storms over CEI and the Himalayan foothills and then swe

194 multiple ARDS GWAS genes related to cytokine storm, oxidation, and coagulation in lung microvascular

195 bable cue, radiating >1,000 km from tornadic storms, perceived by birds and influencing bird behavior

196 Storm-petrel reproductive success showed a quadratic res

197 Using a population of Leach's storm-petrels breeding in the Bay of Fundy, we tested wh

198 In contrast to expectation, storm-petrels feeding partially on invertebrates had the

199 tochastic optical reconstruction microscopy (STORM) produce pointillist data sets of molecular coordi

200 These storms produced record rainfall and high water discharge

201 nt may increase nutrient storage and improve storm protection, but cause declines in habitat availabi

202 ons of people, most prominently by providing storm protection, food and fodder.

203 RED-STORM provided new information for subsequent experiment

204 icated by the sparsity of long-term "direct" storm proxies.

205 SIM and STORM reconstructions of Escherichia coli cells harbouri

206 icane activity, but continuous and long-term storm records are needed from multiple sites to assess t

207 Although the storms remain above a warm open sea, the majority of the

208 abilistic statistical spectroscopy tool, RED-STORM (Resolution EnhanceD SubseT Optimization by Refere

209 Current bioassays that detect cytokine storm responses in vitro rely on endothelial cells, usua

210 life support to treat refractory arrhythmic storm responsible for cardiogenic shock in patients resi

211 oreal life support for refractory arrhythmic storm responsible for cardiogenic shock resistant to ant

212 tween clusters of colabeled proteins; and 3) STORM-RLA also calculates the precise distances between

213 the xy-plane and <50 nm along the z-axis; 2) STORM-RLA provides a quantitative assessment of the freq

214 Thus STORM-RLA represents a significant advance in the high-t

215 oscopy-based relative localization analysis (STORM-RLA).

216 size the need to identify key players of the storm's initial wave.

217 ntification of key mediators of the cytokine storm's initial wave.

218 Stage-triggered storm sampling most precisely captured nitrate flux when

219 rval, stage-triggered, and dynamic-discharge storm sampling).

220 ted States, including combined and separated storm sewer systems, will result in varying environmenta

221 ents (basin, bioswale, culvert, grass swale, storm sewer, and pipe underdrain).

222 fication, sea-level rise, intensification of storms, shifts in species distribution, and decreased pr

223 tochastic optical reconstruction microscopy (STORM) shows a tight association of CIZ1 with Xist RNA a

224 Dust storms significantly influence the performances of solar

225 ty measure that combines maximum wind speed, storm size, and background rotation rate.

226 product of the Coriolis parameter and outer storm size.

227 In the months following the storms, some fish demonstrated exploratory trips back to

228 ommon super-resolution techniques such as (d)STORM, STED, and SIM.

229 osome axes in Caenorhabditis elegans through STORM (stochastic optical reconstruction microscopy) and

230 een seismic river noise and discharge during storms, suggesting that flow and erosional processes in

231 extreme precipitation depends on the type of storm supported by the meteorological environment.

232 lood hazard varies in response to changes in storm surge climatology and the sea level.

233 obabilistic projections of the sea level and storm surge climatology to estimate the temporal evoluti

234 astrophic coastal flooding, when wind-driven storm surge inundates large areas, the relative contribu

235 large portion of these losses, and although storm surge is typically the main focus in the media and

236 -1800) and anthropogenic era (A.D.1970-2005) storm surge model results for New York City, exposing li

237 e sea-level projections with wave, tide, and storm surge models to estimate increases in coastal floo

238 le drivers (e.g., extreme coastal high tide, storm surge, and river flow).

239 vel fluctuations caused by tides, waves, and storm surge.

240 ndicate that there will be minimal change in storm-surge heights from 2010 to 2100 or 2300, because t

241 lood hazard in New York City depends on both storm surges and rising sea levels.

242 The storm surges are derived from large sets of synthetic tr

243 the types of storms that create the largest storm surges for New York City.

244 hese foraminifera were transported inland by storm surges to low elevation freshwater lakes during ti

245 We combine modeled storm surges with probabilistic sea-level rise projectio

246 ased proliferation of T cells and a cytokine storm syndrome in vivo.

247 Cytokine storm syndromes, such as familial hemophagocytic lymphoh

248 recasts of extratropical winter cyclones and storm systems and projections of their response to futur

249 fied NoV and Escherichia coli in sewage from storm tank discharges and treated effluent processed by

250 Although the storm terminated at the eastern coast of Greenland in la

251 to increases in the extremes of the types of storms that create the largest storm surges for New York

252 f these cell populations, creates a "perfect storm" that ultimately determines organ cancer risk.

253 is on the principal features of the cytokine storm the mechanisms underlying this intense systemic in

254 With the progression of the storm, the storm-borne bacterial community showed increa

255 Geomagnetic storms, the disturbances of Earth's magnetic field follo

256 mic and societal consequences of severe dust storms, this study complements the multi-model projectio

257 f the LMI distribution reflects two types of storms: those that undergo RI during their lifetime (RI

258 The relevance of dust storms to public health is likely to increase as extreme

259 tochastic optical reconstruction microscopy (STORM) to Xenopus egg extracts and tissue culture cells,

260 n was likely impacted by a northward shifted storm track and higher pressure over the region arising

261 the Alps supporting a southward shift of the storm track during the local Last Glacial Maximum (that

262 t with intensification of the Pacific winter storm track in response to North Atlantic freshwater for

263 rack position, with positive correlations to storm track latitude in eastern Alaska and northwestern

264 re supply and snowpack responded strongly to storm track position, with positive correlations to stor

265 To assess how historical storm track variability affected ecosystem processes, we

266 We calculated correlations between storm track variability and three hydroclimatic variable

267 s were greener in years when the cool-season storm track was shifted to the north.

268 ed with a poleward shift of the mid-latitude storm track.

269 global atmospheric circulation, influencing storm tracks and the size and location of subtropical de

270 From 1980 to 2014, cool-season storm tracks entered western North America between appro

271 the strongest storms will be compensated by storm tracks moving offshore at the latitude of New York

272 lts suggest that projected shifts of Pacific storm tracks over the 21st century would likely alter hy

273 by moderate to high severity wildfires when storm tracks were displaced north, and the average burn

274 ring the cool season via midlatitude Pacific storm tracks, which may experience future shifts in resp

275 ductive following winters with south-shifted storm tracks, while Canadian ecosystems were greener in

276 latitudinal position of cool-season Pacific storm tracks.

277 arth's climate and fuelling the mid-latitude storm tracks.

278 ded to be higher in years with north-shifted storm tracks.

279 hly sensitive to the position of cool-season storm tracks.

280 alization found here, and the segregation of storm types relative to hydrological and ecological flux

281 The typical cytokine storm was present, with levels of interferon gamma, tumo

282 acilitating key ecosystem services including storm water storage and water treatment.

283 acies indicate a paleodepth range from below storm wave base to near-coastal swamp environments.

284 environmental change by dissipating incident storm wave energy and, through accretion, tracking incre

285 sedimentary rocks with cross-lamination and storm-wave generated breccias.

286 disasters associated with floods, wildfires, storm waves, and droughts.

287 tochastic optical reconstruction microscopy (STORM), we observed intimate association of individual m

288 tochastic optical reconstruction microscopy (STORM), we show here that Fam65b oligomers form a circum

289 Dust storms were characterized by a lower abundance of select

290 s dry periods, precipitation-inducing winter storms were steered away from California by a persistent

291 tochastic optical reconstruction microscopy (STORM), which provides information in three dimensions o

292 died after incessant ventricular tachycardia storm, which led to terminal heart failure 2 months post

293 xported only 1/3 of their streamflow during storms, while the reference watersheds exported 2/3 of

294 the predicted strengthening of the strongest storms will be compensated by storm tracks moving offsho

295 In contrast, moderate storms with a return period of 2.5 mo are those causing

296 of T cell pools to set in motion a "cytokine storm" with severe and sometimes life-threatening conseq

297 tochastic optical reconstruction microscopy (STORM) with pair-correlation analysis to show that EGF a

298 stems (MCSs), the largest type of convective storm, with increased frequency and intensity of long-la

299 Central to its pathogenesis is a cytokine storm, with markedly increased levels of numerous proinf

300 method has taken the scientific community by storm, with thousands of labs using it for applications