ライフサイエンスコーパス: air temperature

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

2 modification of the associations by ambient air temperature.

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

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

5 py structure and increases in dormant season air temperature.

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

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

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

9 es which deviate significantly from the cave air temperature.

10 s increase immediately after periods of high air temperature.

11 parable data are not currently available for air temperature.

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

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

14 ated with milder winters and warmer seasonal air temperature.

15 ow a direct linear relationship with surface air temperature.

16 ffective as CO(2) in altering global surface air temperature.

17 Atlantic Oscillation and global mean surface air temperature.

18 o shifting precipitation patterns and rising air temperature.

19 t endogenously, were exposed to decreases in air temperature.

20 g link between atmospheric CO2 and Antarctic air temperature.

21 cts of decreased precipitation and increased air temperature.

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

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

24 s or imprecise surrogates like elevation and air temperature.

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

26 intensities of solar radiation and different air temperatures.

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

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

29 nsmission parameters that strongly depend on air temperatures.

30 albedo change on monthly and annual surface air temperatures.

31 farms can significantly affect near-surface air temperatures.

32 ifying North Atlantic Oscillation and rising air temperatures.

33 hanges in land use have an impact on surface-air temperatures.

34 ago, apparently in response to warmer spring air temperatures.

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

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

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

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

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

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

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

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

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

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

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

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

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

52 cial-interglacial linkages between Antarctic air temperature and atmospheric CO2 variations.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

69 es in SST coincide with changes in Antarctic air temperature and precede changes in continental ice v

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

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

72 Lower air temperature and prolonged exposure to oxygen resulte

73 n climate change with projected increases in air temperature and reduced summer rainfall are also con

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

75 ear relationship between global mean surface air temperature and sea-ice habitat substantiated the hy

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

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

78 Air temperature and snowpack trends projected from obser

79 nic twitching is sensitive to the prevailing air temperature and the activation of BAT thermogenesis.

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

81 sea surface temperature, lower-tropospheric air temperature and total column water-vapour content ov

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

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

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

85 for the operation of a "bipolar see-saw" in air temperatures and an oceanic teleconnection between t

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

87 with 5-6 degrees C increases in mean winter air temperatures and associated decreases in winter sea-

88 more quickly than can be explained by warmer air temperatures and decreased precipitation, and their

89 % more of the summer daytime hours had lower air temperatures and evaporation rates, higher soil mois

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

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

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

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

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

95 r period, atmospheric carbon dioxide, Vostok air temperature, and deep-water temperature are in phase

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

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

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

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

100 th tropical sea-surface temperature, mean SH air temperature, and North Pacific sea-level pressure, u

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

102 climate-related trends of river flow, winter air temperature, and snow pack between 1950 and 1999 are

103 tropospheric humidity, cloud amount, surface air temperature, and vertical velocity confirm that thes

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

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

106 MR) imaging, an MR-compatible incubator with air, temperature, and humidity regulators and integrated

107 We find that the air temperature anomaly (the deviation from the 1961-199

108 Because air temperatures are statistically increasing along the

109 litter layer is also higher than the shaded air temperature at 0.4 m, both temperatures being higher

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

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

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

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

114 The average air temperature at the Earth's surface has increased by

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

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

117 addition, predicted increases in summertime air temperatures at high southern latitudes would contri

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

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

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

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

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

123 sive warming treatment increased plant-level air temperature by 1-3 degrees C, which is in the range

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

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

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

127 edict a net annual global warming of surface air temperatures by approximately 0.65 K, enhancing dust

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

129 , with the meteorological archive of surface air temperatures can provide a 19th-century baseline tem

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

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

132 today in the Turkana Basin and reflect high air temperatures combined with solar heating of the soil

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

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

135 The fitted air temperature datasets are made publicly available alo

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

137 Mean air temperature decreased slightly with distance from th

138 rming: a pattern in parallel with increasing air temperatures, decreasing relative humidity, and wide

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

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

141 9%) moderate the wintertime land-sea surface air temperature difference and further decrease winds by

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

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

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

145 ical conditions (wave forces, surge flow, or air temperature during low tide).

146 d that, among the climatic factors, the mean air temperature during seed development greatly influenc

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

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

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

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

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

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

153 et-sampled SST and night-time marine surface air temperature features a reduced zonal gradient in the

154 1960s, including seasonality of stream flow, air temperature, floodplain shrub habitat, and snowshoe

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

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

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

158 Here it is shown that a rise in air temperature from 20 degrees to 40 degrees C causes l

159 has become possible with the availability of air temperatures from the Microwave Sounding Unit (MSU)

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

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

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

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

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

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

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

167 olocene, peak (summer) insolation drove July air temperatures higher than present, and resulted in in

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

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

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

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

172 mosphere has been linked to decreased global air temperature in past ice core studies of glacial to i

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

174 Atelopus spp. extinctions and mean tropical air temperature in the previous year is indeed robust, b

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

176 Air temperatures in the arid western United States are p

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

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

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

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

181 As air temperature increases, evaporative demand also incre

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

183 approximately decadal periodicity in surface air temperature is discernable in global observations fr

184 Average global surface-air temperature is increasing.

185 Here we show that surface air temperature is lower in open land than in nearby for

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

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

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

189 annual precipitation and mean annual surface air temperature is said to be uniform +/-10% over East A

190 g extreme cold exposure (21 degrees C < or = air temperature < or = 25 degrees C), pups at both ages

191 moderate cold exposure (30 degrees C < or = air temperature < or = 32.5 degrees C), pups at both age

192 Increasing air temperatures may result in stronger lake stratificat

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

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

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

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

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

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

199 .1mm) containing 10% (w/v) WPI were dried at air temperatures of 45, 65 and 80 degrees C for 600s at

200 years earlier; these translate to increasing air temperatures of about 1.2 degrees C per 100 years.

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

202 Here, the influence of air temperature on sleep in 8-day-old rats was examined

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

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

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

206 effects of CO(2) on land plants alone causes air temperature over land to increase by 0.42 +/- 0.02 K

207 adiative effect of CO(2) causes mean surface air temperature over land to increase by 2.86 +/- 0.02 K

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

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

210 The surface air temperatures over the tropical Pacific were construc

211 declines with decreasing photoperiod, before air temperatures peak.

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

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

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

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

216 ears, with the Greenland Ice Sheet Project 2 air temperature proxy record and atmospheric methane rec

217 and 2008, implying a global R(S) response to air temperature (Q(10)) of 1.5.

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

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

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

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

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

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

224 High air temperature reduced hatchling output only at the are

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

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

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

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

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

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

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

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

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

234 Air temperature strongly affects the flight metabolic ra

235 Spring air temperature strongly regulated the SGS of both decid

236 The rise in air temperature suggested by the temperature sensitiviti

237 We also measured air temperature (T(a)) and beetle body temperature (T(b)

238 primary climatic drivers humidity (e(a)) and air temperature (T(air)) have on cellulose delta(18)O va

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

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

241 emperature at an 8.6 degrees C lower average air temperature than did tropical species.

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

243 to the present, LGM ELAs were maintained by air temperatures that were 3.5 degrees to 6.6 degrees C

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

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

246 anches serve to raise leaf temperature above air temperature to a much greater extent in more norther

247 when cultures are shifted from cool, ambient air temperature to a warmer, blood temperature.

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

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

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

251 their potential for improving a 50-y surface air temperature trend prediction with data from earlier

252 ove the component of the cold-season surface air temperature trends (over land areas poleward of 40 d

253 Surface air temperature trends are disaggregated by boreal cold

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

255 rban warming on reported large-scale surface-air temperature trends.

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

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

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

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

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

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

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

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

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

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

266 Air temperature was consistently the best predictor of p

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

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

269 Allele frequencies and air temperatures were intermediate in the middle drainag

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

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

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

273 unts for effects of short-term variations in air temperature, wind speed, stomatal opening, and leaf

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