ライフサイエンスコーパス: precipitation

1 tainties (buffelgrass patch infill rates and precipitation).

2 ty on cucumber and tomato fruit responded to precipitation.

3 eceded by several months of anomalously high precipitation.

4 sity which can be reached for a given annual precipitation.

5 hanges in cloud cover, specific humidity and precipitation.

6 tropical forests are modulated seasonally by precipitation.

7 itoids, or direct impacts of temperature and precipitation.

8 ienced different levels of long-term average precipitation.

9 rience relatively evenly distributed monthly precipitation.

10 on, instead, experience increased wet season precipitation.

11 (r(2) = 0.77-0.85; p < 0.1), controlling for precipitation.

12 erbaceous and woody plants to alterations in precipitation.

13 s the loss of dissolved phosphate to apatite precipitation.

14 rate of increase diminishes with increasing precipitation.

15 evolutionary diversity of communities at low precipitation.

16 ing water extraction followed by acetic acid precipitation.

17 acid treatments followed by stepwise ethanol precipitation.

18 ly large ranges, prone to high variations in precipitation.

19 d negatively correlated with 24-h cumulative precipitation.

20 se pre-2000 circulation trends have affected precipitation(12-14), and potentially ocean circulation

21 Fruit-NPP was positively related to summer precipitation 2 yr before (R(2) = 0.85), and negatively

22 d dry conditions (2013 and 2015) and extreme precipitation (2014).

23 .7%), elevated CO(2) (+19.6%), and increased precipitation (+73.1%) but inhibited by increased drough

24 tions (from 1850 to 2100) of temperature and precipitation across the ranges of more than 30,000 mari

25 events in the equatorial Pacific Ocean alter precipitation across the tropics.

26 There has been evidence that anomalous precipitation affects Antarctic ice mass loss estimates,

27 In addition, with precipitation alteration, the magnitude of root response

28 ound productivity increases with mean annual precipitation, although the rate of increase diminishes

29 ng-standing recognition of the importance of precipitation amount and variability for most terrestria

30 growing season rainfall over a wide range of precipitation amounts, from extreme wet to dry condition

31 d that FPE increases with absolute latitude, precipitation and (all else equal) with temperature.

32 1993 are characterized by both below average precipitation and above average temperature.

33 -EPS) was recovered, fractionated by ethanol precipitation and analysed by NMR and methylation analys

34 ary production values were most sensitive to precipitation and aridity in dryland and grassland ecosy

35 Precipitation and atmospheric circulation are the couple

36 ause auroras are produced mainly by electron precipitation and because electrons are the main current

37 ity changes, sample deformation, and mineral precipitation and dissolution.

38 has a limited impact on the balance between precipitation and evaporation.

39 ized drought index (such as the Standardized Precipitation and Evapotranspiration Index, SPEI; Vicent

40 ), Na(+)) and suspended sediment yields with precipitation and extent of forest cover, whereas we obs

41 seasons with extreme drought (2012), extreme precipitation and flood (2014) and moderate drought cond

42 eather events, including recent increases in precipitation and flooding associated with tropical cycl

43 ied the relationship between temperature and precipitation and Greenland barnacle goose survival and

44 LTD, followed by precipitation and IDMS, allows for efficient differentia

45 impacts on fire, including higher basin-wide precipitation and increased drought frequency and severi

46 As climate change has reduced precipitation and increased temperature and drought, bar

47 Higher mean annual precipitation and lower mean annual temperature were the

48 ITGB1, JNK, and ENT1 by ZIP4 using chromatin precipitation and luciferase reporter assays.

49 Rather, temperature, precipitation and negative density dependence strongly i

50 forests on river flow is sensitive to annual precipitation and potential evapotranspiration, but resp

51 emperature, diurnal temperature range (DTR), precipitation and relative humidity were associated with

52 l intensity and characteristics of monsoonal precipitation and runoff is poorly understood.

53 ime, preventing the catastrophic outgassing, precipitation and sample degradation observed when the d

54 ental limits, which are primarily related to precipitation and seasonality, with a secondary contribu

55 oned into aqueous and ethanol fractions by a precipitation and sedimentation-based technique and prof

56 mperatures drive losses more than changes in precipitation and solar radiation, leading to strongest

57 flower colouration, followed by mean annual precipitation and solar radiation.

58 In this study, electrochemically induced precipitation and stabilization of fresh urine was succe

59 th and phase determine regional temperature, precipitation and storm tracks.

60 Integrating the effects of projected precipitation and temperature changes on groundwater inf

61 , we analyze recent historical and projected precipitation and temperature data for the Grand Canyon

62 cate multi-decadal cyclical patterns in both precipitation and temperature for most of the time perio

63 oundwater DOC increases following changes in precipitation and temperature in key areas relying on gr

64 Downscaled and bias-corrected precipitation and temperature output from 97 CMIP5 globa

65 inated functional axes to adapt to different precipitation and temperature regimes.

66 quate in length to capture the full range of precipitation and temperature variability and by the une

67 orest biome, including observed responses to precipitation and temperature.

68 bution (three states), we find evidence that precipitation and temperatures in the planting year (2-1

69 in collection systems by forcing controlled precipitation and to inhibit urea hydrolysis during stor

70 The revealed precipitation and transformation pathways of Co (Fe) sul

71 ation of savannas directly (i.e., increasing precipitation) and indirectly (e.g., decreasing disturba

72 to reach inhibitory concentrations, without precipitation, and completely inhibit SRM activity.

73 Our data revealed that temperature, precipitation, and elevation consistently correlate with

74 s to investigate the effects of temperature, precipitation, and ultraviolet (UV) light on community t

75 The Amazon river basin receives ~2000 mm of precipitation annually and contributes ~17% of global ri

76 ly high rainfall variability using a 32-year precipitation-ANPP dataset from the same site as our exp

77 Summer temperature and precipitation appeared to be important drivers shaping p

78 r human population density and higher annual precipitation are associated with delayed flowering offs

79 that live-cell PCR and LiCl-isopropanol DNA precipitation are ideal to prepare DNA for sequencing an

80 ope data indicate a biogenic origin for iron precipitation around chert granules on the shallow shelf

81 ary to this prevailing view, using diffusion-precipitation assays, native state MS, isothermal titrat

82 High winds and precipitation associated with storms can affect lakes vi

83 ment of the catalyst and Li(+) leads to LiOH precipitation at the cathode.

84 influenced species' distributions more than precipitation at weekly and monthly scales, while precip

85 The scenario with increased precipitation (based on a regional model projection) led

86 The scenario with decreased precipitation (based on global circulation model project

87 Precipitation-based isolation method exhibited the highe

88 species' extinction risk as temperatures and precipitation begin to exceed species' historically obse

89 troscopy pinpointed that magnesium carbonate precipitation begins at 1.5 monolayers of adsorbed H(2)O

90 Precipitation being the most influential determinant of

91 2)O film thickness is required for carbonate precipitation, but a mechanistic understanding is lackin

92 pid adjustment contributes to a reduction in precipitation, but has a limited impact on the balance b

93 Local sea surface warming tends to increase precipitation, but this local control is difficult to di

94 rests that differed in long-term mean annual precipitation by 25% (three dry forests with MAP < 1,250

95 global mean temperature by 1.8 degrees C and precipitation by 8%, for at least 5 y.

96 hensive overview of the occurrence of TFA in precipitation by a systematic and nation-wide field moni

97 n ethanol or glacial acetic acid followed by precipitation by addition of excess water.

98 the simultaneous salting-out effect (induced precipitation by decreasing solubility) that PILs exert

99 Here, we show that early warning of salt precipitation can be achieved through geophysical remote

100 Typhoon-related precipitation can produce flooding that is often only pr

101 ze bacterial communities involved in CaCO(3) precipitation; challenge the maxim that biogenic activit

102 hese findings suggest that root responses to precipitation change may critically influence root produ

103 The effect size of precipitation changes on nirS and nosZ showed a U-shape

104 earlier soil moisture recession, but summer precipitation changes remain highly uncertain.

105 spite limited evidence for robust changes in precipitation, changes in ecological drought are robust

106 llected wet-only and bulk rainfall from four precipitation chemistry monitoring stations, primarily l

107 ongitudinal variability in river conveyance, precipitation climatology, flows and sediment connectivi

108 emically induced reactions and/or continuing precipitation continue in darkness or in deeper water du

109 From 1979 to 2017, accumulated Antarctic precipitation contributes to significant ice mass loss a

110 arctic ice mass loss estimates, and thus the precipitation contribution should be understood and cons

111 tic ice mass over recent decades and examine precipitation contributions over this period.

112 s deforming via diffusion creep, dissolution-precipitation creep and grain boundary sliding.

113 Using 100-year historic daily precipitation data from six stations of forest lands alo

114 eratures, cloud cover, specific humidity and precipitation decreased.

115 ual precipitation is low, and sensitivity to precipitation decreases as catchment aridity increases.

116 Our study implies that if effective precipitation decreases in the future, the carbon uptake

117 91-2014) capturing temperature increases and precipitation decreases.

118 ely tightly grouped and highly distinct from precipitation delta(2)H values, likely due to human-spec

119 trolled by the isotopic composition of local precipitation (delta(18)O(precipitation)) that depends o

120 ong-term exposure to heat, frost, radiation, precipitation, deposition of aerosols and particles, att

121 Precipitation, desorption, and diffusion processes are i

122 for extensive time-periods, necessitating a precipitation-driven hydrological cycle.

123 rowing-season temperature and growing-season precipitation drove global variation in K(S) independent

124 tion period and increased with above-average precipitation during juvenile rearing.

125 The absence of starch co-precipitation during RNA extraction resulted in enhanced

126 understanding of biologically-mediated iron precipitation during the Archean by illustrating that it

127 r, annual mean temperature, water vapor, and precipitation during the coldest quarter.

128 ations, productivity declined with increased precipitation during the fall spawning and early incubat

129 ssure deficit, high solar radiation, and low precipitation during the wet season were driving factors

130 ure (e.g. temperate/continental regions) and precipitation (e.g. tropical savannas).

131 strate EndoVIPER-seq (Endonuclease V inosine precipitation enrichment sequencing) as a facile and eff

132 ll be sensitive to reduced or delayed summer precipitation, especially if coupled to snow drought and

133 rends in temperature, relative humidity, and precipitation estimated from 31 climate models account f

134 could lead to significant reductions in the precipitation-evaporation balance of the southern tropic

135 he climatic water balance (i.e. Standardized Precipitation-Evapotranspiration Index, SPEI), using mon

136 Extreme precipitation events affect water quantity and quality i

137 collecting aerially deposited microbes after precipitation events and subjecting soil mesocosms to ei

138 well-developed understanding of how wind and precipitation events can alter lake physical processes a

139 extreme (Hurricane Florence, September 2018) precipitation events on NRE PicoP abundances and composi

140 reasing the magnitude and frequency of large precipitation events, or deluges.

141 ing and improving resiliency against extreme precipitation events.

142 MGAT4D-L interacted with MGAT1 in co-immuno-precipitation experiments.

143 We show that accumulated (time-integrated) precipitation explains most inter-annual anomalies of An

144 ss spectrometry multi-method based on an ACN-precipitation extraction was developed for the analysis

145 their ability to simulate regional and local precipitation extremes and related processes inhibit dec

146 By mapping observed temperature and precipitation extremes onto each atmospheric regime, we

147 ns, such as central Vietnam, the majority of precipitation falls outside the summer monsoon period.

148 ational estimate is an 80 per cent change in precipitation for every gram per kilogram change in the

149 EV isolations by precipitation from basal culture medium or apical surfac

150 ate processes controlling stable isotopes in precipitation from central Vietnam by combining moisture

151 Precipitation from ethanol resulted in a network with a

152 In contrast, precipitation from glacial acetic acid resulted in a hig

153 e show that aspartic acid inhibits aragonite precipitation from seawater in vitro, at the pH, saturat

154 e approach of combining radar technology and precipitation gauge measurements to quantify the spatial

155 For the cases presented, precipitation gauges measured increases between 0.05 and

156 easured increases between 0.05 and 0.3 mm as precipitation generated by cloud seeding passed over the

157 nsforms seasonal patterns of temperature and precipitation, germination success at marginal temperatu

158 nes harbor polymorphisms associated with the precipitation gradient, including orthologs of genes tha

159 tail how evolutionary diversity varies along precipitation gradients by bringing together a comprehen

160 ly determined by a temperature gradient, but precipitation gradients may be more important within the

161 ypothesis that diversifying selection across precipitation gradients, acting on ancestral cereal grai

162 al races and is correlated to proxies of the precipitation gradients.

163 used here can be applied to a wide range of precipitation-hardened alloys and different additive man

164 Precipitation has received little attention in glacial e

165 erannually depleted oxygen isotope ratios in precipitation have been linked to the summer monsoon str

166 val ciliary injection and mutton fat keratic precipitation in all eyes.

167 heat treatment, can trigger nickel-aluminium precipitation in an iron-nickel-aluminium alloy in situ

168 future projections of less sea ice and more precipitation in Arctic Alaska.

169 2 yr before (R(2) = 0.85), and negatively to precipitation in May (R(2) = 0.83) in the fruit years.

170 ally with deeper water, below-wave base iron precipitation in micritic iron formations.

171 ve demonstrated increasing trends in extreme precipitation in North America, and models and theory co

172 tation feedbacks substantially affect annual precipitation in North and South America and Australia m

173 vesicle (sEV) secretion and apatite calcium precipitation in the arterial wall.

174 40.0 per mille indicate at least some pyrite precipitation in the presence of a (34)S-depleted pore w

175 communities respond to temporal patterns of precipitation in water-limited ecosystems is necessary t

176 In particular, precipitation increase consistently enhanced fine-root b

177 elevated carbon dioxide [CO(2) ], increased precipitation, increased drought, increased N deposition

178 Projected precipitation increases likely will not suffice to fully

179 levation-specific changes in temperature and precipitation, indicating diverging phenologies of neigh

180 A precipitation-induced eruption trigger is consistent wit

181 ver over time in response to fluctuations in precipitation inferred from speleothem oxygen and stront

182 Regimes with low seasonality in precipitation, instead, experience increased wet season

183 er, the coastal area also experienced higher precipitation intensity with shorter return period over

184 g factors to this reduced load include lower precipitation intensity, altered tillage practices, and

185 preparing zein networks through antisolvent precipitation, involving dissolution in ethanol or glaci

186 We conclude that precipitation is a highly influential factor on estuarin

187 variation, over regions where climatological precipitation is about one millimetre per day or more.

188 Although precipitation is considered to be the most important dif

189 erpinning responses to temporal variation in precipitation is crucial to anticipate consequences of a

190 Forests affect river flow less when annual precipitation is low, and sensitivity to precipitation d

191 Precipitation is one of the most important factors that

192 temporal variations in TFA concentration in precipitation is scarce.

193 but the importance of their interaction with precipitation is unclear.

194 Interannual changes in precipitation isotopes in central Vietnam are governed b

195 ional evaluation metrics for storm tracks or precipitation itself.

196 importance of physical habitat, streamflow, precipitation, landscape, and biological characteristics

197 e propose here viral mechanisms in carbonate precipitation, leading to stromatolite formation, whereb

198 Using fluid-phase luciferase immune precipitation (LIPS) assays, we characterized IgG, IgM,

199 transformations associated with solid-state precipitation look structurally simple, yet, inexplicabl

200 d to cloud seeding are isolated from natural precipitation (<1 mm h(-1)).

201 were larger at sites with higher mean annual precipitation (MAP) and temperature of the wettest quart

202 u ratio have been prepared via an oxalate co-precipitation method, showing excellent performance for

203 obtained by the isoelectric-ammonium sulfate precipitation method.

204 ea flours by alkaline extraction-isoelectric precipitation method.

205 ate substitution when synthesized by aqueous precipitation methods.

206 icrobial induced calcium carbonate (CaCO(3)) precipitation (MICP) in three ureolytic bacterial strain

207 ple is microbially induced calcium carbonate precipitation (MICP) in which microbial activity leads t

208 cant increasing trends (p <= 0.05) in annual precipitation near the south coastal area of the LMRAV a

209 Uncertainty in precipitation observations(9,10) and limited observation

210 Ba(x)Sr(1-x)SO(4) and no further significant precipitation occurred after 2 days.

211 troduced, based on controlled hydrolysis and precipitation of bovine serum albumin.

212 release channel, combined with the intra-SR precipitation of Ca(2+) salts.

213 iomolecules play key roles in regulating the precipitation of CaCO(3) biominerals but their response

214 solubility in the suspending media to permit precipitation of calcium phosphate.

215 n on the west and is primarily determined by precipitation of driest quarter, annual mean temperature

216 lusions in the ceramics, which suggests that precipitation of fatty acids as calcium salts is an impo

217 formed species occurring during the onset of precipitation of ionic solids from solution.

218 ng acidification of the media, and extensive precipitation of magnesium oxalate dihydrate (glushinski

219 reacting with excreted oxalate resulting in precipitation of magnesium oxalate dihydrate which also

220 and a chemical ordering tendency leading to precipitation of ordered phases such as L1(2) and B2.

221 Methodologies applied for extraction and precipitation of protein were optimized - pH 4 and 12, r

222 We studied photochemically induced precipitation of rare-earth elements (REEs) in water fro

223 lithium fluoride interphase formation, while precipitation of the lithium hydroxide was not observed.

224 The impact of precipitation on the distribution of evolutionary divers

225 he additional live biomass at sites with low precipitation or high ambient soil nitrogen.

226 (p < 0.001; OR = 1.47), high average monthly precipitation (p < 0.001; OR = 1.14), and high surface r

227 tamination was associated with higher weekly precipitation (p < 0.001; OR = 1.44) and higher livestoc

228 r to observations better reproduce important precipitation patterns over highly populated areas such

229 ear 2020-2099 time period indicate projected precipitation patterns similar to recent historical (wat

230 warmer climate in tropical wet forests, and precipitation patterns will define the intensity of CO(2

231 nuclear waste treatment, over pre-determined precipitation periods.

232 d soil CO(2) due to warmer conditions, while precipitation played a critical role in moderating the b

233 effectiveness of implementing an isoelectric precipitation procedure to reduce the residual PEG along

234 vide stronger relationships for constraining precipitation projections under climate change as compar

235 In addition, precipitation projections vary substantially among clima

236 idance, has the potential to derive reliable precipitation projections, although caveats remain and t

237 ative correlations were found with the total precipitation (r between -0.42 and -0.64).

238 y polluted trajectories tend to have lighter precipitation rates, longer average lifetime, and higher

239 bility of common scalants and decreases salt precipitation rates.

240 surface temperature generated in the sodium precipitation reaction and development of software for t

241 and a FA for a Regular Language (RL) uses a precipitation reaction.

242 we present a 12,000 yr continuous U/Th-dated precipitation record from a Guatemalan speleothem showin

243 rt pathways in rocks from CO(2)-induced salt precipitation reduces injectivity and potentially compro

244 limate disruption, including temperature and precipitation regime shifts, has been linked to animal p

245 ng concurrent shifts in CO(2) , temperature, precipitation regimes and nitrogen deposition, yet few s

246 Thus, a shift towards precipitation regimes dominated by fewer but larger rain

247 itation variation in already highly variable precipitation regimes gives rise to a pattern of "season

248 lutionary diversity is found in intermediate precipitation regimes, and that there is a decline in ev

249 Yet, abiotic factors, principally precipitation regimes, shape biogeographical and phenolo

250 ditions favorable for flooding, the enhanced precipitation related to Kelvin waves was found in over

251 nalysis, we showed that LiCl-isopropanol DNA precipitation removed primers and small, nonspecific PCR

252 extraction buffer and solutions used for RNA precipitation resulted in a robust method for extracting

253 armer with more extreme weather and variable precipitation, resulting in shorter iced-over periods an

254 neral, projects an increase in mean seasonal precipitation, runoff, and streamflow.

255 rated using 3 distributed hydrologic models (Precipitation-Runoff Modeling System, Variable Infiltrat

256 In total, 1187 precipitation samples, which were collected over the cou

257 For the oaks, only precipitation seasonality and growing season moisture av

258 ture associated with geographic distance and precipitation seasonality.

259 Using chromatin immune precipitation-seq-based occupancy profiles of H3K4me3 an

260 r nuclear localization, and Chromatin immuno-Precipitation Sequencing analysis showed that the MITF-A

261 Near Antarctica, where precipitation sinks of aerosol are small, the underestim

262 -aspartic acid (Asp) which when added to the precipitation solution of calcium carbonate crystallizes

263 ation, and deprotection followed by a single precipitation step.

264 The principles of in situ precipitation strengthening and local microstructure con

265 elding of pure calcite through the classical precipitation strengthening mechanism, but also enhance

266 GPP was responsive to both winter and summer precipitation such that two distinct GPP maxima were sep

267 nvectively coupled Kelvin waves, large scale precipitation systems propagating at ~12 m/s along the e

268 how that climate variables (e.g. mean annual precipitation, temperature and, key to this study, CO(2)

269 elation between dehydrin gene expression and precipitation, temperature, and day-length.

270 ) soil CO(2) concentration responded more to precipitation than to other meteorological variables (in

271 d outlier SNPs associated with seed mass and precipitation that also carry signatures of selection ba

272 volutionary diversity, areas of intermediate precipitation that are found in the South American 'arc

273 sequestration of halide ions through simple precipitation that results in catalyst loadings as low a

274 mposition of local precipitation (delta(18)O(precipitation)) that depends on the source of water vapo

275 y a means for biorecovery of REE via oxalate precipitation the bioleaching and bioprecipitation poten

276 alaria transmission is more sensitive to the precipitation threshold than the thermal response curve

277 oved from solution, regardless of ettringite precipitation time or the presence of TcO(4)(-) or CrO(4

278 ignificantly improved with longer ettringite precipitation times, and decreased to zero in the presen

279 Variations in long-term precipitation trends due to climate forcings have been o

280 procedures of purification including alcohol precipitation, ultrafiltration (UFDF) and microfiltratio

281 Areas of precipitation unambiguously attributed to cloud seeding

282 determine whether daily maximum temperature, precipitation, UV index, and the incidence 5 days later

283 ed mass from common gardens, and bioclimatic precipitation variables.

284 Increases in projected seasonal precipitation variation in already highly variable preci

285 Overall, antisolvent precipitation was able to improve the functionality of z

286 n 154 observations from experiments in which precipitation was manipulated in the field and root biom

287 pitation at weekly and monthly scales, while precipitation was more important at seasonal scales.

288 Precipitation was not associated with a greater rate of

289 ratio of calcium ion to phosphate, periodic precipitation was obtained accompanied by pH oscillation

290 tundra fires, our results reveal that summer precipitation was the most important climatic driver (r

291 e simulations of mean annual temperature and precipitation, we project socio-economic outcomes under

292 The median, the estimated average, and the precipitation-weighted average TFA concentration of all

293 the stomatal pores, small amounts of silver precipitation were observed in some epidermal cells, ind

294 climatic variability (variability of summer precipitation) were among the best predictors of global

295 tocol for AAV production based on chloroform-precipitation, which allows for fast in-house production

296 ium target material was recovered via alkali precipitation with ammonia solution.

297 cting Escherichia coli cultures, followed by precipitation with polyethylene glycol (PEG).

298 s years using Climate Hazards Group InfraRed Precipitation with Station data, with recent drought cla

299 Greenhouse gas (GHG) emissions affect precipitation worldwide.

300 During low precipitation years, RUE is lowest when rainfall event s