ライフサイエンスコーパス: air temperature

1 g water stress (precipitation, humidity, and air temperature).

2 combination of elevated [CO2 ] and increased air temperature.

3 o shifting precipitation patterns and rising air temperature.

4 cts of decreased precipitation and increased air temperature.

5 mates of daily averages of PM2.5 and maximum air temperature.

6 ology) weaker in the year with lower average air temperature.

7 s or imprecise surrogates like elevation and air temperature.

8 modification of the associations by ambient air temperature.

9 ring in annual-mean global-mean near-surface air temperature.

10 1- degrees C increase in global mean surface air temperature.

11 ntration (Ca ) will increase with increasing air temperature.

12 py structure and increases in dormant season air temperature.

13 ent upon the estimated PFO size and inspired air temperature.

14 both lakes in the absence of any changes in air temperature.

15 er of 40.1 watts per square metre at ambient air temperature.

16 es which deviate significantly from the cave air temperature.

17 s increase immediately after periods of high air temperature.

18 parable data are not currently available for air temperature.

19 ar-sky UV indices, ozone levels, and outdoor air temperature.

20 on flux density, vapor pressure deficit, and air temperature.

21 ffer thoracic temperature against changes in air temperature.

22 s were observed to be correlated with indoor air temperature.

23 he need to import energy, and thereby reduce air temperatures.

24 nism for globe readings to incorrectly track air temperatures.

25 intensities of solar radiation and different air temperatures.

26 eastern United States as a result of warming air temperatures.

27 equilibrium between drip water and host rock/air temperatures.

28 nsmission parameters that strongly depend on air temperatures.

29 albedo change on monthly and annual surface air temperatures.

30 ossover analyses, adjusted for dew point and air temperatures.

31 The increase in autumn air temperature (0.22 degrees C yr(-1)) during the 9 yea

32 ence was decreased with the highest-quartile air temperature (0.80 (0.70-0.92), P=0.002) but increase

33 rrigation cooling effect is also observed on air temperature (-0.38 to -0.53 degrees C) from paired f

34 as a result of the combination of increased air temperature (+1.8 ~ +5.2 degrees C) and precipitatio

35 OLE/SA ratio 1:1.6 and inlet air temperature 135 degrees C were the optimal condition

36 g factors: microwave power (100, 200, 300W), air temperature (20, 30, 40 degrees C) and pre-treatment

37 attle began to seek thermal refugia at lower air temperatures (24 degrees C) by selecting areas close

38 eticornis trees exposed to ambient or warmed air temperatures (+3 degrees C).

39 sought refugia within wooded areas at higher air temperatures (36 degrees C), which occurred much les

40 ere investigated using a convective dryer at air temperatures 50, 60 and 70 degrees C and air velocit

41 grain drying was carried out at three drying air temperatures: 60 degrees C, 60/80 degrees C and 80 d

42 ect of rising atmospheric carbon dioxide and air temperature(7-9).

43 temperatures and six at a 3 degrees C warmer air temperature; a late-summer drought was also imposed.

44 vironmental conditions (that is, accumulated air temperatures above 0 degrees C per year, freshwater

45 tion to obtain a high resolution estimate of air temperature across Africa.

46 ses in atmospheric carbon dioxide (CO2 ) and air temperature affect silicon accumulation in grasses,

47 ality with atmospheric CO2 concentration and air temperature after the start of the Industrial Revolu

48 Increases in air temperatures aloft and lesser increases at the surfa

49 s California and Texas, projections based on air temperature alone underestimates cooling demand by a

50 the existing projections are based on rising air temperatures alone, ignoring that rising temperature

51 tic projections showed a drastic increase in air temperature and a mild decrease in precipitation at

52 rehydration ratio increased with increasing air temperature and air velocity.

53 elated to changing precipitation, increasing air temperature and anthropogenic activities in the vici

54 We studied the effects of increasing air temperature and aridity on a Burrowing Owl (Athene c

55 In fall, simulated air temperature and atmospheric moisture between the two

56 the potential forest loss impact on regional air temperature and atmospheric moisture.

57 he long-term links between multiple climate (air temperature and cryospheric dynamics) and vegetation

58 gical stations, and corresponding daily mean air temperature and daily precipitation data from 19 cli

59 ibrated reconstructions of separate Pliocene air temperature and East Asian summer monsoon precipitat

60 ion) was positively correlated with the mean air temperature and global radiation (r(s) 0.44 and 0.42

61 to account feedbacks between climate change, air temperature and humidity, and consequent power plant

62 mpacts when modeling NEELAND using projected air temperature and incoming shortwave radiation.

63 birds will be affected by rapid increases in air temperature and increased drought frequency and seve

64 ormula: see text] is close to growing-season air temperature and is projected to fall below it under

65 the AMO appear to produce anomalous surface-air temperature and low-level wind fields in the two pol

66 ut the burn site, which recorded the maximum air temperature and made comparisons to the degree of th

67 in all three subwatersheds under the minimum air temperature and maximum precipitation scenario due t

68 In contrast, the maximum air temperature and minimum precipitation scenario led t

69 a record of late autumn through early winter air temperature and moisture source changes in East-Cent

70 ften use heat index, which incorporates both air temperature and moisture.

71 ces, stratospheric ozone levels, and outdoor air temperature and National Allergy Bureau total pollen

72 ey measures of heat stress, considering both air temperature and near-surface humidity, in characteri

73 ward shortwave radiation at surface, surface air temperature and planetary boundary layer (PBL) heigh

74 Here, we investigated effects of seasonal air temperature and precipitation (fall, winter, and spr

75 c, and significant anomalies of land surface air temperature and precipitation over all the continent

76 Air temperature and precipitation were found to be the m

77 c parameters with different sensitivities to air temperature and precipitation.

78 Lower air temperature and prolonged exposure to oxygen resulte

79 ase in pore-water salinity mainly depends on air temperature and relative humidity, and tide and wave

80 particle metrics and MI cases, adjusted for air temperature and relative humidity.

81 istent with a rapid and coherent response to air temperature and sea-ice trends, linked through the d

82 may be attributed to the coupling effects of air temperature and snow depth associated with the under

83 Air temperature and snowpack trends projected from obser

84 ased turbulent heat flux is used to increase air temperature and specific humidity in the lower tropo

85 he malaria transmission parameters driven by air temperature and their seasonal variation.

86 rnal sap flow, was strongly affected by PAR, air temperature and vapor-pressure deficit.

87 g conditions, such as infrared power, drying air temperature and velocity, on quality of strawberry w

88 ime decreased with increased infrared power, air temperature and velocity.

89 nd the drying time decreased with increasing air temperature and velocity.

90 initions using maximum, minimum, and average air temperatures and apparent temperatures.

91 % more of the summer daytime hours had lower air temperatures and evaporation rates, higher soil mois

92 r flood-rich periods in terms of its extent, air temperatures and flood seasonality.

93 Our models reveal that increasing air temperatures and heat wave occurrence will potential

94 These trends are attributed to increasing air temperatures and reduced snow cover duration in spri

95 esponding to a rapid rise in regional summer air temperatures and related permafrost temperatures.

96 ated variables for PB-PAH, PNC, and NOx, and air temperatures and relative humidity for PM2.5.

97 the ecological impacts of recent record warm air temperatures and simultaneous peak drought condition

98 heet, either indirectly, by its influence on air temperatures and winds, or directly, mostly through

99 Outdoor PM2.5, ambient air temperature, and asthma symptoms in the past 14 days

100 e account for the variability in wind speed, air temperature, and equilibrium partitioning over the c

101 r cools to 4.9 degrees Celsius below ambient air temperature, and has a cooling power of 40.1 watts p

102 was in turn dependent on wetness rather than air temperature, and higher FCH4 in flooded years was th

103 ct to influence daytime and nighttime summer air temperature, and how effects vary with the spatial s

104 hile E. coli was associated with population, air temperature, and N and C concentrations (p < 0.05).

105 hat the time lags between radiation forcing, air temperature, and rainfall generate a rate-dependent

106 nd environmental parameters (level of ozone, air temperature, and relative humidity) on particle emis

107 n in the watershed), and climatic variables (air temperature, and river discharge) with Escherichia c

108 ainage area, population density, mean annual air temperature, and watershed slope.

109 tterflies responded to fine-scale changes in air temperature, and whether species-specific responses

110 interactions between increased thaw, warmer air temperatures, and higher levels of soil moisture.

111 of the millennium, significant increases in air temperature are expected later this century, with pr

112 winter, Bewick's swans frequent areas where air temperatures are c.

113 orthern circumpolar permafrost region, where air temperatures are increasing two times faster than th

114 anomalies from the London average of modeled air temperature at a 1-km grid resolution.

115 IP5 climate projections are for a warming of air temperature at all sites throughout the 21(st) centu

116 of the relationship between land-surface and air temperature at lower resolution to obtain a high res

117 d Chl trends were found in regions with high air temperature at the beginning of the study period.

118 sures correlated significantly to reciprocal air temperature at the coastal station Rao and over the

119 ing event after an extraordinary increase in air temperature at the end of 2015.

120 sition of the alpine treeline in relation to air temperature at two sides in the Changbai Mountains i

121 leads changes in Northern Hemisphere surface air temperatures at multi-decadal timescales, indicating

122 atures (breeding season or winter) and local air temperatures at the nesting colony.

123 ed their laying dates in relation to October air temperatures at the same rate, preserving allochrony

124 Variation in nighttime air temperature averaged 2.1 degrees C (range, 1.2-3.0 d

125 icant inter-model correlation between SM and air temperature biases (R = -0.65), (ii) a wet/cold bias

126 patterns of summertime SM, precipitation and air temperature biases over CONUS in 20 different CMIP5

127 edback of plant respiration to rising global air temperature, but a lack of evidence on long-term (we

128 buted to rapid increases in regional surface air temperature, but it is now clear that this cannot be

129 s: sea-level rise is often assumed to follow air temperature, but this assumption holds only for TSLR

130 temperatures have warmed rapidly relative to air temperatures, but changes in deepwater temperatures

131 verage of 1.1 degrees C and summer nighttime air temperature by 1.5 degrees C.

132 d feedback increases the continental surface air temperature by roughly two degrees for each degree i

133 warming treatment increased winter nighttime air temperatures by an average of 1.1 degrees C and summ

134 However, air temperatures can be very different from the equilibr

135 nterannual variations in seasonally averaged air temperature, canopy biomass, and precipitation can p

136 s predict that droughts and hotter water and air temperatures caused by climate warming will reduce t

137 osphere (TOA) radiative responses to surface air-temperature changes over the Arctic by using TOA ene

138 Snow depth variation combined with air temperature contributed to the variability in the SG

139 The global mean surface air temperature data indicate a global warming hiatus be

140 ared maximum daily 8-hour average ozone with air temperature data taken from the National Oceanic and

141 The fitted air temperature datasets are made publicly available alo

142 Increasing mean air temperatures, declining precipitation, and changes i

143 On the day of the eclipse, air temperature decreased by 6.4 degrees C, coupled with

144 Mean air temperature decreased slightly with distance from th

145 influences larval development rates whereas air temperature determines adult longevity as well as th

146 log-linear models controlling for continuous air temperature, dew-point temperature, day of week, hol

147 9%) moderate the wintertime land-sea surface air temperature difference and further decrease winds by

148 , we show that daytime and nighttime leaf-to-air temperature differences are key to geographic gradie

149 However, air temperature differences were smaller (2 degrees C vs

150 he CO2 growth rate and tropical land-surface air temperature during 1959 to 2011, with a 1 degrees C

151 ) from four mountain chains as a function of air temperatures during mid-gestation.

152 ng's large effect was due to not only warmer air temperatures during the growing season, but also to

153 ree increase of the initial maritime surface air temperature, effectively suppressing Arctic air form

154 In years with anomalously high spring air temperatures, elderberry fruited several weeks earli

155 nal risks of ED visits beyond those of daily air temperature, even in a region with high air-conditio

156 ounted measurement system was used to sample air temperature every 5 m along 10 transects (~7 km leng

157 n the Arctic and Boreal biomes, we show that air temperature explains c.

158 1960s, including seasonality of stream flow, air temperature, floodplain shrub habitat, and snowshoe

159 of days with high precipitation amounts and air temperatures fluctuating around 0 degrees C) during

160 primarily driven by the increase in surface air temperature, followed by declining snowfall.

161 The global distribution of the optimum air temperature for ecosystem-level gross primary produc

162 disentangling the contribution of water and air temperature for the buildup of thermal stress.

163 ns of the year-to-year variations of surface air temperature for today's climate, with areas of large

164 e comparison of observed global mean surface air temperature (GMT) change to the mean change simulate

165 evel of leaf thermoregulation across a broad air temperature gradient.

166 ict environmental regulation on stem growth (air temperature > 2 degrees C and soil water potential >

167 eased the filtration efficiency; and (3) the air temperature had very limited effect on the filtratio

168 variance CO(2) flux measurements showed that air temperature has a primary influence on net CO(2) exc

169 At night, passive cooling below ambient air temperature has been demonstrated using a technique

170 A long-term local cooling trend in surface air temperature has been monitored at the largest concen

171 motivated by our previous observations that air temperature has increased over the last 30 years in

172 ted to improved forage resources, as warming air temperatures have been shown to improve survival rat

173 Local mean annual and mean summer air temperatures have increased at a rate of 0.2-1.2 deg

174 ese two options buffer individuals from free-air temperature, however, is not well known.

175 sources that are directly exposed to ambient air temperature (i.e., outdoor sources).

176 of terrestrial ectotherms often exceed local air temperatures, implying a high degree of thermal safe

177 ct of: (a) different drying methods, (b) hot air temperature in a convection oven, and (c) the moistu

178 bations due to rapid changes of sunlight and air temperature in big sagebrush (Artemisia tridentata s

179 The increase in surface air temperature in China has been faster than the global

180 crease of 2 degrees C in seasonally averaged air temperature in combination with a 10% reduction in c

181 ation in wood-NPP could be explained by mean air temperature in May, precipitation from April to May

182 Air temperature in the chamber changes only at ~.2 mK/mi

183 hese findings indicate that further rises in air temperature in the maritime Antarctic may enhance te

184 ome of the largest increases in near-surface air temperature in the Southern Hemisphere.

185 imary limiting factors to GPP beginning with air temperature in winter and proceeding to moisture and

186 Air temperatures in the arid western United States are p

187 r, we found that the light signals with warm air temperatures in the fall might induce the accumulati

188 The fact that air temperatures in the UK in 2007 were marginally lower

189 Our results show that air temperatures in this region are now at their warmest

190 fect, as manifested by elevated near-surface air temperatures in urban areas, exposes urban dwellers

191 ward solar radiation, precipitation and mean air temperature) in a complex landscape of the Reynolds

192 ed trend follows the Arctic amplification of air temperature increase in the Northern Hemisphere.

193 ury if midrange projections of a 2 degrees C air temperature increase occur.

194 ring this 19-year period, CO(2) rose 40 ppm, air temperature increased by 1 degrees C and annual rain

195 Daytime air temperature increased linearly with increasing imper

196 s became more attracted to riparian areas as air temperature increased, with preferences increasing t

197 m in many streams during the 20th Century as air temperatures increased by 0.6 degrees C and would sh

198 As air temperature increases, evaporative demand also incre

199 of how seasonal and interannual variation in air temperatures influence phenology is poorly understoo

200 redominantly during October when the average air temperature is 10 degrees C-15 degrees C.

201 Our results establish that air temperature is a necessary but not sufficient variab

202 n the current observation network of surface air temperature is maintained.

203 models, our results confirm that global mean air temperature is nonlinearly related to heat stress, m

204 ed to elevated water temperature, while high air temperature is only stressful if water temperature i

205 contraction are large body mass, increase in air temperature, loss of natural land, and high human po

206 Similarly, exposure to air temperature maxima associated with delayed fledging,

207 Increasing air temperatures may result in stronger lake stratificat

208 these microclimatic conditions than to free-air temperatures, microclimatic ground and near-surface

209 itime Antarctic, we determine whether rising air temperatures might similarly influence the diversity

210 erefore, contrary to previous findings using air temperatures, most ectotherms do not have a physiolo

211 Mean summer air temperature (MSAT) was the principal factor driving

212 August 2010 average air temperature near the exposure site was 25 degrees C,

213 ature is comparable with previously reported air temperature observations used in predicting Rs and i

214 on was carried out in a spray-drier at inlet air temperature of 160 degrees C.

215 onding to an average decrease in mean annual air temperature of ~4-6 degrees C from the Late Eocene t

216 g free convection when calculating t(r) from air temperatures of 2 K above t(r) could introduce a mec

217 roximately 10 d for initial maritime surface air temperatures of 20 degrees C.

218 .1mm) containing 10% (w/v) WPI were dried at air temperatures of 45, 65 and 80 degrees C for 600s at

219 ce a near-surface cooling effect on regional air temperatures of up to 3-4 degrees C in late winter a

220 In particular, the effect of air temperature on GEP was fully mediated through phenol

221 e GPP response to VPD, (b) direct effects of air temperature on GPP dynamics, (c) hysteresis in the d

222 fects of a climate or land-use driver (e.g., air temperature) on lake environment could be relatively

223 tes, and meteorological data (precipitation, air temperature) on leachate PFAS concentrations was als

224 speed, and between urbanization and surface air temperature, on flight altitudes.

225 mpact of climate change-in particular higher air temperatures-on a nuclear power station that recircu

226 ing three climate datasets of precipitation, air temperature or drought severity, combined with sever

227 temperature) was greatly overestimated when air temperature or intact leaf temperature was erroneous

228 nce of ISMR extremes on both the 2 m surface air temperature over India and on the sea surface temper

229 t 65 million years, with mean annual surface air temperature over ten degrees Celsius warmer than dur

230 ccounting for actual changes in moisture and air temperature over that period, showed a 7.1-7.9% incr

231 The surface air temperatures over the tropical Pacific were construc

232 al climate projections of monthly changes in air temperature, precipitation, solar radiation, vapor p

233 ed that tropospheric ozone concentration and air temperature predicted from the model are sensitive t

234 similarly to expected increases in Antarctic air temperature (presently occurring along the Antarctic

235 An increase of 1 degrees C in air temperature produced an increase of 8% in the averag

236 ive correlations were observed with the mean air temperature (r between 0.32 and 0.66), the global ra

237 d a significant correlation with average low air temperature (r=0.359, p<0.01) as well as precipitati

238 city had a positive correlation with average air temperature (r=0.705, p<0.01), while hydroxyl radica

239 dent data for diverse taxa spanning a global air temperature range of approximately 60 degrees C.

240 e present a revised and extended high Arctic air temperature reconstruction from a single proxy that

241 t this large thinning is consistent with our air temperature reconstruction.

242 Here, we make use of air temperature records and observations of spring leaf

243 High air temperature reduced hatchling output only at the are

244 increase due to changes in precipitation and air temperature regime for the period 2050-2069.

245 curred due to increased snow thickness while air temperature remained statistically unchanged.

246 hile our model simulations support a surface air temperature response to the eruption of the order of

247 habitat, and food chain length increases, as air temperatures rise.

248 Atmospheric water vapor increases as air temperature rises, which causes further warming.

249 of its major tributaries over 1949-2006 when air temperatures rose by 1.4 degrees C while annual prec

250 e slowing of the trend of increasing surface air temperature (SAT) in the late 1990 s, intense intere

251 e temperatures (SSTs) and land-based surface air temperatures (SATs) display multidecadal variations

252 ril 2016, southeast Asia experienced surface air temperatures (SATs) that surpassed national records,

253 tic warming compared to local summer surface air temperatures (SATs).

254 ditions (e.g., declining snow depths, rising air temperatures, shortening winters), spatially explici

255 cipitation intensity with daily mean surface air temperature shows a negative scaling of -9.6%/K, in

256 towards winter, a large-scale decline in the air temperature, significantly shallower atmospheric bou

257 ogy; a decoupling of tree growth from rising air temperatures since the 1970s.

258 Mean air temperature, soil pH and ruminant animal species (sh

259 at warm sampling sites with increased summer air temperature, soil temperature, and soil moisture, wh

260 mounts and their seasonal distribution, mean air temperature, specific humidity, and atmospheric CO2

261 Spring air temperature strongly regulated the SGS of both decid

262 y to heat and drought stress as indicated by air temperature (T(a) ) and evaporative fraction (EF).

263 perature (T(L-AW) ) across 265 d, varying in air temperature (T(air) ) from -1 to 45 degrees C.

264 nnual precipitation (-2 mm) and no effect on air temperature (Table 1)" the word 'precipitation' was

265 -m tall whole-tree chambers tracking ambient air temperature (Tair ) or ambient Tair + 3 degrees C (i

266 Antecedent air temperature (Tairant ) and vapor pressure deficit (V

267 This led to a substantial local forcing on air temperature that contributed to the intensity of the

268 y, wind speed, soil moisture differences and air temperature; the relative importance of these factor

269 e reduction of 37 degrees C from the ambient air temperature through a 24-h day-night cycle, with a m

270 The time it takes for the surface air temperature to drop below freezing increases nonline

271 ghted climate networks based on near-surface air temperature to investigate the global impacts of El

272 gional climate models that predict increased air temperature, together with hydrologic models that pr

273 t, and litter and negatively correlated with air temperature, total soil N (TN) and microbial biomass

274 linearly with projected increases in surface air temperature towards the end of this century.

275 < 0.05) abrupt change in the autumn Eurasian air temperature trend occurred in 2003.

276 little correlation with global mean surface air temperature trends, but are strongly anti-correlated

277 of 2069 (+/-18 years s.d.) for near-surface air temperature under an emissions stabilization scenari

278 o nearly 5 degrees Celsius below the ambient air temperature under direct sunlight.

279 We explored variation by air temperature using similar models, stratified into qu

280 e efficiency (Q) as functions of soil water, air temperature, vapor pressure deficit, vegetation gree

281 Abiotic variables (air temperature, vapour pressure deficit and UV-B radiat

282 theory predicts optimal chi as a function of air temperature, vapour pressure deficit, c(a) and atmos

283 ostics of PC1 indicate previous year's local Air Temperature variability being the primary influence

284 ases evaluated for sensitivity to historical air-temperature variability and computationally interpol

285 Five intervals reflect ice sheet minima and air temperatures warm enough for substantial ice mass lo

286 cade; median velocity = 1.07 km/decade) when air temperatures warmed at 0.21 degrees C/decade.

287 piration (RE) were associated primarily with air temperature: warmer conditions enhanced GPP and RE.

288 thin the vernal window were sequential, with air temperatures warming prior to snow melt, which prece

289 The daily range of the surface air temperature was also reduced by up to 1.1 K due to t

290 Air temperature was consistently the best predictor of p

291 2 environmental factors, mean annual surface air temperature was the strongest and most consistent pr

292 ariables that drive vegetation productivity (air temperature, water availability and cloud cover).

293 ental dissipation data with reported average air temperatures, we estimated a reaction activation ene

294 Vapor pressure deficit (VPD) and air temperature were manipulated to determine effects of

295 a severe drought event, when fuel loads and air temperatures were substantially higher and relative

296 Particularly, we predict that Norwegian air temperature will decrease over the coming years, alt

297 Climate simulations indicate air temperatures will warm by 1 degrees C to >3 degrees

298 efficiency is influenced by the insolation, air temperature, wind speed and relative humidity.

299 Variability in daytime air temperature within the urban landscape averaged 3.5

300 d that Takanari clearly decreased canopy and air temperatures within the planetary boundary layer com