ライフサイエンスコーパス: weather

1 of wild pigs coincided with periods of cold weather.

2 l rainfall, even simultaneously under normal weather.

3 scapes are most vulnerable to extreme winter weather.

4 ctors stress, pollen exposure, and change in weather.

5 ocal colonization during the harshest winter weather.

6 iency increased when the plastic surface was weathered.

7 avy metal remediation, and the prevention of weathering.

8 as a reference for the release rate of Na by weathering.

9 rface material by solar heating and/or space weathering.

10 , potentially through changes in continental weathering.

11 substances was investigated for biophysical weathering.

12 mectite precursor, a process akin to reverse weathering.

13 he matching of diesel oil spills affected by weathering.

14 in situ biological contributors to incipient weathering.

15 nces in abundance, recent exposure, or space weathering.

16 on is a novel and unexpected aspect of space weathering.

17 This finding makes opal formed by rocks weathering a new, complementary source of animal fossils

18 monstrated variation in responses to extreme weather across species' ranges, with predicted decreases

19 The precise time window during which spring weather advances phenology varies considerably across ea

20 iderophores and organic acids as biochemical weathering agents was shown.

21 ered bedrock, with intervals of more intense weathering along fractures, documenting the combined inf

22 and 12,000 US school districts with detailed weather and academic calendar information to show that t

23 Weather and climate change are constant and ever-changin

24 Compound events (CEs) are weather and climate events that result from multiple haz

25 host-parasite combinations, compiling local weather and climate records at each location.

26 ical ocean surface temperatures drive global weather and climate(1-5).

27 ur understanding of the ocean's influence on weather and climate.

28 dy was to determine the relationship between weather and demographic rates of Greenland barnacle gees

29 on in maximum COVID-19 growth rates based on weather and demography (17%) and country-specific effect

30 rasshopper abundance, mediated by effects of weather and host plants.

31 c link for the observed relationship between weather and population-level seed production.

32 ic light intervals across a year, because of weather and seasons.

33 Changing weather and social conditions provide in situ cues alter

34 expected to become warmer with more extreme weather and variable precipitation, resulting in shorter

35 lithologies contribute to efficient chemical weathering and carbon sequestration in the Southeast Asi

36 l parameters can vary, such as land area for weathering and CO(2) outgassing fluxes.

37 ir apparent relative surface ages from space weathering and cratering records.

38 Furthermore, to account for weathering and environmental factors, two equations mode

39 observations are likely to also describe the weathering and flow path patterns in other headwater lan

40 ology in the context of landscape evolution, weathering and hydrology.

41 rtance of subglacial aluminosilicate mineral weathering and lack of retention of these species in sed

42 opical mountainous rivers on global silicate weathering and suspended sediment transport.

43 can be applied in other settings to predict weathering and water quality responses to climate change

44 vant inputs (atmospheric deposition, manure, weathering) and outputs (seepage water, biomass harvest)

45 nal opportunities are compromised by extreme weather, and children may suffer delayed cognitive devel

46 ge crop in areas frequented with hot and dry weather, and high temperature.

47 s of floral/nesting resources, insecticides, weather, and honey bee (Apis mellifera) abundance, drive

48 pill samples to determine type and degree of weathering, and (iii) improving the matching of diesel o

49 o be partly driven by a changing climate and weather anomalies.

50 ertainties due to variability of climate and weather are provided where possible.

51 ix trans-Saharan long-distance migrants that weather at the wintering and stopover grounds almost ent

52 geochemistry implies the presence of young, weathered basalts at the site at the time of the impact.

53 In weathered bedrock aquifers, groundwater is stored in por

54 The transition from saprolite to weathered bedrock is more gradational, over a depth rang

55 weathering increases steadily upward in the weathered bedrock, with intervals of more intense weathe

56 anding of biophysical as well as biochemical weathering by S. commune could be reached and unexpected

57 Given the rising risk of extreme weather caused by climate change, enhancement of abiotic

58 net searches for topics included climate and weather change, air pollution, particulates, greenhouse

59 s) trees by monitoring multi-year changes in weather, chlorophyll fluorescence, chloroplast ultrastru

60 he results highlight the association between weather/climate and pollutant accumulation in Arctic foo

61 wever, adjusted for surface availability and weather conditions (0.13 whales per km(2), CV = 0.38), t

62 time), CO(2) supply issues (0.6%) or adverse weather conditions (1.1%).

63 duction are primarily controlled directly by weather conditions (sink limitation), while carbon assim

64 source limitations to tree growth driven by weather conditions and going beyond a simple carbon-medi

65 g increases in resulting HD may be linked to weather conditions and increasing severity has been note

66 ethods to integrate uncertainty about future weather conditions and model parameters.

67 ilure rates, and performance under different weather conditions and payloads.

68 ntial of CAM strongly depends on the daytime weather conditions and that the additional water-saving

69 rature and more extreme and less predictable weather conditions are projected to affect water availab

70 hanges in migration phenology and changes in weather conditions at the wintering, stopover, and breed

71 ut for which empirical evidence is rare: the weather conditions during the first growing season after

72 The effect of weather conditions on transmission dynamics was not cons

73 We then exploit variation in weather conditions to statistically identify the effects

74 kelihood of LDEs, suggesting that persistent weather conditions will occur more frequently.

75 condition per annum was influenced by spring weather conditions, (iii) in both species males that rea

76 pheric warmings can influence surface winter weather conditions, but their timing is difficult to pre

77 ands varied as a function of stand age, fire weather conditions, ecozone, and soil moisture class.

78 We analyzed the interannual variability of weather conditions, gross primary productivity (GPP) and

79 he obtained results indicate that changes in weather conditions, recorded in the period of four years

80 lay in modifying their responses to changing weather conditions.

81 gs, number of pigs in barn, temperature, and weather conditions.

82 future performances under largely uncertain weather conditions.

83 e of various generated cities under the same weather conditions.

84 age and fast water releasing under different weather conditions.

85 een landscape features and decadal trends in weather conditions.

86 flight altitude, seasonality, and associated weather conditions.

87 F must be understood and evaluated under the weathering conditions of geologic disposal, which extend

88 for the effects of environmental (social and weather) conditions during a badger's first year on pace

89 column with plagioclase and alumino-silicate weathering contributing < 5% of the Ca(2+)-Na(+) solutes

90 crease in nutrient delivery from continental weathering, coupled with a possible decrease in upwellin

91 o) at 4 h post fertilization were exposed to weathered crude oil and assessed for visual function usi

92 nstrates selection for hypersensitivity to a weather cue, high temporal variability, and high synchro

93 Here we detail a land-based enhanced weathering cycle utilizing magnesite (MgCO(3)) feedstock

94 hrough the water-mediated carbonate-silicate weathering cycle, atmospheric CO(2) partial pressure (pC

95 Using current, fine-scaled weather data and global reports of infections, we develo

96 Analysis of weather data conducive for infection, between 2010 and 2

97 The use of DL has advantages over weather data since it can be determined in advance just

98 level using building energy models, outdoor weather data, and building characteristic data.

99 onthly activity of sCoVs using site-specific weather data.

100 enudation flux that is derived from silicate weathering-decreased, sustained by an increase in erosio

101 this, PTHM were traced to geogenic sources (weathering, dissolution, leaching) and anthropogenic emi

102 ited States, combined with discussion of the weather drawn from over 2 billion social media posts.

103 isconceptions about the way that climate and weather drive exposure and transmission have adversely s

104 ndows during which inter-annual variation in weather drives phenological shifts and the consequences

105 crises can also arise that labs may have to weather during their lifetime.

106 odel the impacts of these mismatches, direct weather effects and density dependence on local-scale ap

107 ind strong support for lasting planting year weather effects in restored tallgrass prairies, thereby

108 y similar source diesels, (ii) investigating weathering effects on spill samples to determine type an

109 pyrite oxidation-including oxygen sources-in weathering environments remains elusive.

110 Land-based enhanced rock weathering (ERW) is a biogeochemical carbon dioxide remo

111 Enhanced silicate rock weathering (ERW), deployable with croplands, has potenti

112 t on chick survival: Even a single inclement weather event can reduce offspring survival by >50%.

113 utrient supply during the year of an extreme weather event relative to its historical context.

114 The effect of an extreme weather event was especially magnified among landlocked

115 acing higher summer temperatures and extreme weather events are becoming more common.

116 ty as the frequency and intensity of extreme weather events are predicted to increase.

117 As the world warms and extreme weather events become more common, this diagnostic analy

118 Extreme weather events have become a dominant feature of the nar

119 nted a robust yield estimation under extreme weather events in 2012, which reduced the root-mean-squa

120 Extreme weather events in Asia have been occurring with increasi

121 oss of Arctic sea ice to midlatitude extreme weather events is applied to the 21st-century intensific

122 ically improbable, yet profound 'black swan' weather events is logistically difficult.

123 We showed that invasive rabbits and extreme weather events reduce reproductive output in albatrosses

124 hange and spatial co-localisation of extreme weather events since 1961.

125 In many regions across the globe, extreme weather events such as storms have increased in frequenc

126 we gain insight into the types of disruptive weather events that will become more prevalent as partic

127 ching offspring are now exposed to inclement weather events twice as often as they were in the 1970s.

128 ase in the frequency and intensity of severe weather events, and changes in distribution and health o

129 ges including temperature elevation, extreme weather events, and rising air pollution.

130 nthropogenic movement, natural dispersal and weather events, as well as genetic factors linked to shi

131 e SSTs and the frequency of extreme seasonal weather events, epizootics causing MMEs are likely to in

132 The NRE is impacted by extreme weather events, including recent increases in precipitat

133 e temperatures and more frequent and extreme weather events, pressure from biotic stresses will becom

134 e increased frequency of extreme climate and weather events.

135 ance can support risk reduction from extreme weather events.

136 anges may have been transient Neoproterozoic weathering events whose biogeochemical consequences were

137 ition probability before and after simulated weathering events.

138 Recent weather extremes including the unprecedented heat wave i

139 d product substantially biases the impact of weather extremes on agricultural income and the potentia

140 ticipate how diverse species will respond to weather extremes spanning weeks to months.

141 utes included hog density, environmental and weather factors such as vegetation, wind speed, temperat

142 urred during a period of unusually inclement weather, famine, and disease in the Mediterranean region

143 We show that this weathering feedback ought to produce a log-linear relati

144 sider the effects of global warming, extreme weather, flooding and other consequences of climate chan

145 We find that the global silicate weathering flux remained constant, even as the global si

146 xtended by limitation of the global silicate weathering flux.

147 idizing microorganisms control global pyrite weathering fluxes despite their ability to catalyze the

148 o Southern Oscillation (ENSO), might have on weathering fluxes.

149 nization of health findings with traditional weather forecasting efforts could be critical in the dev

150 ther terrestrial planets such as Mars, where weathering-formed opal occurs.

151 evertheless, the magnitude and allocation of weathered fractions under abiotic and biotic treatments

152 Our results highlight that extreme weather has variable and potentially strong implications

153 Weather has weak and spatially variable effects on survi

154 Our findings suggest that changes in weather (i.e., increase of temperature and humidity as s

155 conditions, though the degree to which these weather impacts are related to site-specific factors suc

156 Understanding extreme weather impacts on staple crops such as wheat is vital f

157 ortant implications for nowcasting of severe weather in the Sahel and potentially in other MCS hotspo

158 Both may contribute to biochemical weathering in addition to enzymatic functions.

159 We analyzed weathering in shale, the most common rock exposed at Ear

160 Extreme weather, including heat waves, droughts, and high rainfa

161 Chemical weathering increases steadily upward in the weathered be

162 y implement adaptation practices to mitigate weather-induced stresses in the most vulnerable cropland

163 y analyses heat impacts on wheat using daily weather information and a dryland wheat dataset for 71 c

164 outcomes in the adoption of microfinance and weather insurance.

165 mained constant, even as the global silicate weathering intensity-the fraction of the total denudatio

166 ial freshwaters due to glacial melt-enhanced weathering is likely a globally relevant phenomenon, wit

167 ganic carbon burial, in addition to silicate weathering, is necessary to account for the positive del

168 Here, we investigated weather knockdown of ARID1B, one of two mutually exclusi

169 However, shallow complex structures and weathering layers at near surface not only severely dist

170 r traffic system, like human interaction and weather, lead to a very complicated, high-dimensional, n

171 We find that although variations in weather may be important for endemic infections, during

172 Projected increases in extreme weather may change relationships between rain-related cl

173 Weather may marginally affect COVID-19 dynamics, but mis

174 an airless body, or any surface where other weathering mechanisms may be ruled out.

175 couples a global climate model to a silicate weathering model with spatially resolved lithology.

176 ing a coupled climate and carbonate-silicate weathering model, we quantify the likely scatter in pCO(

177 ironmental solution via predictable regional weather modification and carbon storage.

178 atmospheric CO(2) At the same time, regional weather modification methods, like cloud seeding, are be

179 rmances were investigated using pristine and weathered MPs (polyethylene (PE) and polystyrene (PS) mi

180 g the interaction mechanisms, the removal of weathered MPs was optimized.

181 As PyOM is weathered, NH(3) retention increases sixfold, with more

182 However, weather not only impacts the quantity produced, but also

183 ind speed and solar radiation at the Baoshan weather observing station, are identified and used to bu

184 res have large climate impacts affecting the weather of the Northern Hemisphere.

185 Space weathering of Bennu surface materials does not simply pr

186 ompartmentalization of major elements during weathering of granite, rhyolite, schist and basalt was r

187 Accelerated weathering of limestone (AWL) has been proposed as a too

188 n alkalinity, which indicates the successful weathering of limestone and the long-term storage of the

189 70 kmol(c) ha(-1) y(-1), yet consistent with weathering of marine shale.

190 robial phosphate sinks and enhanced chemical weathering of phosphate minerals under relatively CO(2)-

191 Fe(II)]-oxidizing bacteria in biogeochemical weathering of subsurface Fe(II)-silicate minerals at the

192 es indicate a sudden enhancement in chemical weathering of the continental crust during the early Cam

193 The flux of solutes from the chemical weathering of the continental crust supplies a steady su

194 water twice during formation and subsequent weathering of the Crato Formation.

195 ica-rich fluids derived from the continental weathering of the volcanic host rocks.

196 Weathering of these enriched source rocks mobilizes and

197 rge literature has documented the effects of weather on agricultural yields.

198 t land cover moderates the impacts of winter weather on population dynamics of wintering birds, and (

199 e studies should investigate implications of weathering on end consumer products containing additives

200 : see text] Pyrite oxidation during chemical weathering on land consumes [Formula: see text] and gene

201 As weather once considered extreme occurs more frequently,

202 g population and infrastructures, are either weather or cryosphere-related.

203 Apart from the effects of the weathering, our results suggest a second-order modulatio

204 ted to examine putative correlations between weather parameters during April-September and the amount

205 cal locations of varying soil properties and weather parameters was determined.

206 ments for longitudinal gene expression data, weather pattern changes over time, and growth curves.

207 The allergist's approach to weather pattern changes should be integrated and anticip

208 Climate change is known to affect regional weather patterns and phenology; however, we lack underst

209 Notably, the increasingly extreme weather patterns associated with ongoing anthropogenic c

210 The alteration in weather patterns expected due to climate change will aff

211 an rabbits Oryctolagus cuniculus and extreme weather patterns on breeding probability and success.

212 oach to label thousands of daily large-scale weather patterns over North America in the outputs of a

213 s for improving yield of crops under extreme weather patterns.

214 als of 97 and 99% were measured for PEST and weathered PE, respectively.

215 The removal of pristine versus weathered plastic debris and the impact of plastic parti

216 to spatial and temporal uncertainties in the weather potentially affecting migration timing.

217 We conclude that while delta "weather" (precise configuration) is unpredictable in the

218 Weather primarily affected the sexes at different life-h

219 ent in new packing boxes is disrupted by the weathering process.

220 A variety of climate and weather processes could potentially influence the river

221 occurrences of wind wave, precipitation, and weather processes have distinct regularities.

222 Oil weathering processes change the chemical composition of

223 pendent determination as to which of the two weathering processes contributes to the formation of oil

224 t to the importance of physical and chemical weathering processes in generating nutrients that suppor

225 Weathering processes that changed the surface chemistry

226 lterations to the plastic from environmental weathering processes with success rates of 99, 81, 76, a

227 weathering rates and land-ocean transfer of weathered products.

228 ft comparable biosignatures in the dissolved weathering products.

229 olina, provides unusual access to a complete weathering profile in an Appalachian granitoid.

230 mineralogy and speciation of REE in economic weathering profiles from China to prospective regoliths

231 Weathering proxies indicate that floristic changes occur

232 ne anoxia was induced by a greenhouse-driven weathering pulse, and is compatible with the OAE duratio

233 gration and abundance can be addressed using weather radar analyses.

234 monitored departure of migratory birds using weather radar and simulated their migration trajectories

235 Here we demonstrate that archival weather radar data over a period of ten years can be use

236 Using weather radar data, a unique 23-year (1995-2017) long ti

237 new mining, as well as uncertainties in soil weathering rates and land-ocean transfer of weathered pr

238 Thirdly, the measurements-based weathering rates from subsurface shale are high, amounti

239 ort-term influences on chemical and physical weathering rates, especially, in ENSO-influenced regions

240 diments available for carbonate and silicate weathering reactions that can consume atmospheric CO(2)

241 s due to the overwhelming influence of these weathering reactions.

242 ld trial data, DNA sequences, and historical weather records can be used to tackle the longstanding p

243 tions in France, over 16 years of historical weather records.

244 A concurrent weather regime shift towards warmer, wetter conditions o

245 riod, supporting the possibility that spring weather regime shifts contributed to the increasing popu

246 Many of these events arise from weather regimes that persist over a region for days or e

247 Extreme heat is the leading weather-related cause of death in the United States.

248 Understanding weather-related drivers of crop plant-microbiome relatio

249 pecially sensitive to climate change because weather-related precipitation and evapotranspiration are

250 emonstrates that, contrary to common wisdom, weather-related timing of agent activity and population

251 and freshwater discharge allows estimates of weather-related uncertainties in the forecast.

252 Identification of weather-related yield-limiting conditions and developmen

253 al climate is producing increasingly unusual weather relative to preindustrial conditions.

254 iated with chronic exposure to sustained hot weather remain unclear.

255 Here we use the Weather Research and Forecasting (WRF) model over the we

256 ing several sensitivity experiments with the Weather Research and Forecasting model coupled with Chem

257 Using a chemical transport model-Weather Research and Forecasting model coupled with Chem

258 ation in geospace lies at the heart of space weather research.

259 Comprehensive models of extreme weather risks, exposure, and effects should take individ

260 Early studies of weather, seasonality, and environmental influences on CO

261 Weather shocks may exacerbate vulnerabilities among wome

262 heres (PS-NPs; 20 nm), and water leachate of weathered single-use plastics that contained micro- and

263 t %) but dominate the composition of heavily weathered spilled petroleum.

264 First, the microclimate recorded by a weather station is often quite different to that near th

265 e, by using three types of data (reanalysis, weather station, and remote sensing image data) to asses

266 ons of gridded climate datasets derived from weather stations are often too coarse to capture the con

267 ntrol days at the residential address, using weather stations within 15 km of the residence and 100 m

268 mperature and precipitation data from 62,000 weather stations, and county-level census data on popula

269 te rely on gridded climate data derived from weather stations, which differ from the conditions exper

270 climate data interpolated from standardized weather stations.

271 leaves depending upon geographical location, weather suitability and soil's physiochemical and microb

272 in an area, and use 8 years of data from 12 weather surveillance radars to estimate over 50% SPR dur

273 critical components of the ocean's "internal weather" system.

274 re (SST) is a fundamental driver of tropical weather systems such as monsoon rainfall and tropical cy

275 te changes in the persistence of large-scale weather systems through a pattern-recognition approach b

276 time sequence, suggest enhanced continental weathering that may be attributed to the invasion of bar

277 Flooding due to extreme weather threatens crops and ecosystems.

278 r impact may be-in both space and time, from weather to climate scales.

279 However, local weather, type of arable field and height of the drone ca

280 inked to liver diseases, the question arises weather UDCA holds anti-inflammatory properties on perio

281 due to mismatches in space, scale, time, and weather variable type.

282 to the models with growing season aggregated weather variables and show the strength of Bayesian esti

283 rrelations between statewide collections and weather variables as well as site-level collections and

284 phases of 4469 Scottish Blackface sheep and weather variables during the same period to derive novel

285 dicted impacts of the models with aggregated weather variables.

286 biological control and environmental (i.e., weather) variables.

287 , less have focused on within-growing season weather variation and the interaction between temperatur

288 ocesses and population-specific responses to weather variation influence spatial synchrony at both lo

289 eflect stable animal performance in spite of weather variation.

290 would enhance performance stability against weather volatility without compromising animal growth.

291 Fractured, weathered wall rock around Tavakaiv bodies and intensely

292 reproduction, daily insect availability, and weather, we investigated the complex mechanisms affectin

293 nt probabilistic projections of daily future weather were disaggregated to hourly and used to drive e

294 ncentration, types, polymer composition, and weathering were found among four compartments.

295 Soil-plant cycling and parent material weathering were identified as the most important process

296 untains and consequent increases in silicate weathering, which removes atmospheric carbon dioxide(3,4

297 are likely in more humid climates and summer weather will not substantially limit pandemic growth.

298 ns unknown, as of April 2020, whether summer weather will reduce its spread, thereby alleviating stra

299 an animal fossil preserved in opal formed by weathering with such high-resolution details that even i

300 viously detected in surface water during dry weather, with the effects often exceeding proposed effec

301 primary mediator of crop yield responses to weather within unstable field zones (i.e., zones where y

302 sex, migration strategy, population density, weather, year and agricultural land cover on LDD frequen