ライフサイエンスコーパス: solar radiation

1 (i.e., temperature, water availability, and solar radiation).

2 getically this accounts for much of incoming solar radiation.

3 , including changes in exposure to mutagenic solar radiation.

4 es them the preferred target for terrestrial solar radiation.

5 ental chemical interactions of canopies with solar radiation.

6 romoting hydrogen production under simulated solar radiation.

7 ction in the stratosphere, blocking incoming solar radiation.

8 to a flow of energetic charged particles or solar radiation.

9 aytime GEM flux was strongly correlated with solar radiation.

10 chemical reactions initiated by high-energy solar radiation.

11 sensitive to changes in both temperature and solar radiation.

12 ias of 0.23 V versus Ag|AgCl under simulated solar radiation.

13 urce, environmental pH, iron speciation, and solar radiation.

14 rface or in volcanic vents in the absence of solar radiation.

15 ps under forest canopies that expose them to solar radiation.

16 energy transduction, and protection against solar radiation.

17 and negatively correlated with the amount of solar radiation.

18 inely subjected to DNA damage induced by UVB solar radiation.

19 s and a consequent decrease in reflection of solar radiation.

20 depth and the consequent impacts on incident solar radiation.

21 tratosphere by smoke, which strongly absorbs solar radiation.

22 preventing skin damage resulting from acute solar radiation.

23 cause scattering and absorption of incoming solar radiation.

24 e against some of the deleterious effects of solar radiation.

25 ed cloud cover and the resulting increase in solar radiation.

26 al models to predict seasonal wind speed and solar radiation.

27 sphere in the solar system not controlled by solar radiation.

28 erosols enhance scattering and absorption of solar radiation.

29 e epidermal damage seen in response to acute solar radiation.

30 n, followed by mean annual precipitation and solar radiation.

31 rturbations such as scattering and absorbing solar radiation.

32 es are stabilized or over-cooled by blocking solar radiation.

33 NO(2) near the light source compared to the solar radiation.

34 re rapidly than lighter ones when exposed to solar radiation.

35 or clouds to increase scattering of incoming solar radiation.

36 y driven by seasonality in water deficit and solar radiation.

37 s in response to soil water availability and solar radiation.

38 fects the extent to which they interact with solar radiation.

39 g winter are mitigated by the seasonality of solar radiation.

40 longwave radiation, wind speed, and incoming solar radiation.

41 erogeneity modulated impacts of rainfall and solar radiation.

42 nditions with PAM fluorescence under natural solar radiation.

43 ct against harmful effects of exposure to UV solar radiation.

44 diurnal cycles of the OVOC measurements and solar radiation.

45 ment distinguished by hypersalinity and high solar radiation: (1) The proteome is highly acidic, with

46 by mean annual maximum temperature (21.1%), solar radiation (13.6%), annual precipitation (11%), liv

47 precipitation together with higher incoming solar radiation (~7% decade(-1) cloud-cover reduction) i

48 operties and extent of cooling by reflecting solar radiation-a key uncertainty in anthropogenic clima

49 Solar radiation absorbed by marine phytoplankton can fol

50 rates the rate of snowmelt by increasing the solar radiation absorbed by the snowpack.

51 bove 96.1%, and over 95%, respectively under solar radiation according to the Air Mass Index 1.5 (AM1

52 The relation between solar radiation, air humidity and temperature, and pesti

53 normalized difference vegetation index, and solar radiation all significantly predicted likelihood o

54 ere relaxing with increasing temperature and solar radiation, allowing an upward trend in NPP from 19

55 ainst both elevated metal concentrations and solar radiation, allowing them to persist under the hars

56 Solar radiation alone did not inactivate B. subtilis spo

57 describing the dust absorption efficiency of solar radiation, although it is highly variable.

58 Deserts, with a combination of high solar radiation and availability of large areas unusable

59 unstressed growth conditions, total incident solar radiation and average growing season temperature m

60 ns due to relevant climatic parameters, e.g. solar radiation and average temperature, characterising

61 requires particle-phase humic acid to absorb solar radiation and become photoexcited, then directly o

62 the Earth's radiation balance by scattering solar radiation and by acting as cloud condensation nucl

63 ffectively degrade common organic dyes under solar radiation and can perform very well in photo-assis

64 l Irradiance Monitor (SIM) instrument on the Solar Radiation and Climate Experiment (SORCE) satellite

65 With a solar forcing derived from the Solar Radiation and Climate Experiment data, modeled OH

66 shed solar spectral irradiance data from the Solar Radiation and Climate Experiment suggest a solar U

67 In high altitude Andean streams an intense solar radiation and coinciding metal pollution allow the

68 in which state b is coupled to a via, e.g., solar radiation and coupled to the valence band reservoi

69 c microhabitat gives protection from intense solar radiation and desiccation, and it provides mineral

70 ir distribution, to different intensities of solar radiation and different air temperatures.

71 on, incorporating a distribution of incoming solar radiation and diffusion of heat consistent with a

72 ibers in our engineered material backscatter solar radiation and emit strongly in mid-infrared wavele

73 per canopy leaves are exposed to the highest solar radiation and evaporative demand, which can elevat

74 strongly correlated with exposure to higher solar radiation and evaporative demand.

75 ation nuclei, oxidative stressors--including solar radiation and Fe limitation--may be involved in co

76 ion-a mating-related trait that also absorbs solar radiation and heats individuals above ambient temp

77 me mesic regions (10 degrees -15 degrees S), solar radiation and increased temperature caused increas

78 se modified tetrapyrroles for the capture of solar radiation and its conversion to chemical energy.

79 , the periodicity, the incident angle of the solar radiation and its wavelength are varied in the wid

80 flower activity were associated with greater solar radiation and lower rainfall during El Nino years.

81 ompounds in atmospheric aerosols that absorb solar radiation and may play an important role in planet

82 ensile bars and MP particles using simulated solar radiation and mechanical stress.

83 anin counteracts both the adverse effects of solar radiation and of metals.

84 p of the atmosphere between the net incoming solar radiation and outgoing longwave radiation from Ear

85 in forest productivity with elevation, with solar radiation and plant functional traits (leaf dry ma

86 arine clouds to increase their reflection of solar radiation and reduce the amount of energy absorbed

87 Ms) incorporating land cover, precipitation, solar radiation and selected aqueous chemical measuremen

88 fect Earth's radiative balance by scattering solar radiation and serving as cloud condensation nuclei

89 The ability of sulfate aerosols to reflect solar radiation and simultaneously act as cloud condensa

90 ated by a sulfuric acid proxy that considers solar radiation and SO(2) levels.

91 The combination of intense solar radiation and soil desiccation creates a short cir

92 Under weak solar radiation and stagnant moist meteorological condit

93 Nevertheless, variation in solar radiation and temperature at the timescale of hour

94 ormation in the spring and fall when reduced solar radiation and temperatures reduce emissions from l

95 known about the degradation of oil spills by solar radiation and the impact of nutrient limitation on

96 s, despite similar natural forcings, such as solar radiation and the North Atlantic Oscillation, duri

97 he Earth's climate system because it absorbs solar radiation and therefore potentially warms the clim

98 Clouds' efficiency at reflecting solar radiation and trapping the terrestrial radiation i

99 -hemisphere heating of haze by absorption of solar radiation and winter-hemisphere cooling due to inf

100 High-albedo materials reflect more solar radiation and, thereby, alter the earth's radiativ

101 ts including, among others, climate warming, solar radiation, and alterations of atmospheric componen

102 -400 m apart differ dramatically in aridity, solar radiation, and associated vegetation.

103 Vitamin D is made in the skin on exposure to solar radiation, and it is necessary to optimal skeletal

104 ifically, high vapour pressure deficit, high solar radiation, and low precipitation during the wet se

105 linked to projected cloud trends, reflected solar radiation, and model sensitivity.

106 d further analyses suggest that xeric areas, solar radiation, and non-forest plant productivity are a

107 y reference evapotranspiration, temperature, solar radiation, and precipitation together, but nonline

108 (reference evapotranspiration, temperature, solar radiation, and precipitation) in China simultaneou

109 cover with a resulting increase in received solar radiation, and secondarily by a decrease in the st

110 t important predictors include LAI, downward solar radiation, and soil moisture.

111 , or fivefold stronger effect than rainfall, solar radiation, and the Multivariate ENSO Index, respec

112 compounds, the scattering and absorption of solar radiation, and the reactive uptake of gas species

113 Decomposition of plant litter exposed to solar radiation appears to be a significant contributor

114 Elevation, dry season length, and solar radiation are the most important drivers in determ

115 tures (greater than 50 degrees C), driven by solar radiation, are the primary cause of nitrogen loss

116 Our findings emphasize solar radiation as a significant driver of mass balance

117 Living in a region of residence with high solar radiation as an adult was also associated with an

118 l microbial agents and simulated and natural solar radiation as light sources.

119 rmine reliable criteria weights, identifying solar radiation as the most important criterion (weight:

120 ssful synthesis employing neat substrate and solar radiation as the sole energy source to drive this

121 g-but through an enhancement of net absorbed solar radiation (ASR).

122 Long-term variations in solar radiation at Earth's surface (S) can affect our cl

123 a reduction of 22.8 W m(-2) of net incoming solar radiation at surface.

124 rrelation to ensuing seasonal wind speed and solar radiation at the Baoshan weather observing station

125 of longwave radiation and that of reflected solar radiation at the top of the atmosphere, this study

126 e and some organic aerosol particles scatter solar radiation back into space and can cool Earth's sur

127 bstantial daytime temperature, humidity, and solar radiation barriers.

128 cts of interannual variation in rainfall and solar radiation between 2007 and 2016 on seedling surviv

129 aerosols in the satellite-observed clear-sky solar radiation budget over the world's oceans.

130 ied with temperature, rather than cumulative solar radiation, but no inherent absorptivity difference

131 Absorption of incoming solar radiation by aerosols, however, can reduce the clo

132 e gases is offset by increased reflection of solar radiation by clouds with smaller droplets that for

133 Absorption of solar radiation by colored dissolved organic matter (CDO

134 ic antenna complexes capture and concentrate solar radiation by transferring the excitation to the re

135 Thus, solar radiation, by diminishing infectivity of the paras

136 mosphere contains many compounds that absorb solar radiation, called brown carbon (BrC).

137 Daily skin exposure to solar radiation causes cells to produce reactive oxygen

138 Solar radiation causes immunosuppression that contribute

139 The simulated decreases in surface solar radiation, changes in surface and atmospheric temp

140 For particles reflecting solar radiation, clouds of CO2-ice or H2O-ice particles

141 Solar radiation comprises <10% of UV, and thus the purpo

142 Solar radiation contains ultraviolet B (280-315 nm) and

143 particularly the ultraviolet wavelengths in solar radiation, contributes to the etiology of cutaneou

144 ts for a quarter of the total opacity at the solar radiation/convection zone boundary.

145 Incoming and outgoing solar radiation couple with heat exchange at Earth's sur

146 it affects the absorption and scattering of solar radiation, creates cloud condensation nuclei and p

147 d near-infrared range of the spectrum, where solar radiation culminates, but also the emissivity of t

148 and the CRU temperature, precipitation, and solar radiation datasets.

149 ly achievable with a moderately concentrated solar radiation, demonstrating their potential as an eff

150 causes: variation in environmental drivers (solar radiation, diffuse light fraction, and vapor press

151 The solar radiation dose in the oceanic upper mixed layer (S

152 l mechanism that contributes to regulate the solar radiation doses reaching the earth's biosphere.

153 s strongly with temperature, reflecting that solar radiation drives emissions.

154 et by not only scattering but also absorbing solar radiation due to the presence of the so-called "br

155 ge amount of fresh-DOC and exposed to strong solar radiation during the polynya opening in austral su

156 ly-September season to predict wind speed or solar radiation during the subsequent November-January s

157 ive skill is highest for both wind speed and solar radiation during winter, and lowest during summer.

158 diation experiments and known 1 day incident solar radiation enabled the estimation of a possible REE

159 he upper canopy loss, alongside increases in solar radiation, even during periods of drier soil and a

160 time, the presence of RGM was increased when solar radiation exceeded 200 W m(-2), suggesting a photo

161 One factor that may influence incident solar radiation exposure on litter is surface albedo.

162 t high incidence of exposure to HPV, and the solar radiation exposure that people in this region of t

163 suggest the association of this disease with solar radiation exposure, HIV, and human papilloma virus

164 e predominant causative agent is ultraviolet solar radiation exposure, with the majority of cases occ

165 nd mirrors the concurrent global increase in solar radiation fluxes at Earth's surface and may have c

166 to the usage of a broader spectrum range of solar radiation for water splitting catalytic reactions

167 stations in the NOAA database combined with solar radiation from the NASA-POWER database were in muc

168 The temporary absence of solar radiation gives particular insight into different

169 which could convert water to H(2) driven by solar radiation (H(2)O + hnu --> 1/2O(2) + H(2)).

170 cularly those with nests exposed to incident solar radiation, have darker eggs.

171 Major adaptations on the AS are because of solar radiation, heat, and drought, whereas those on the

172 The DeltaT 0-50 was related to solar radiation, horizontal heat flux, relative humidity

173 easonal cycle is timed to the seasonality of solar radiation in a manner that is suggestive of antici

174 tubular photocatalytic reactor that may use solar radiation in combination with artificial radiation

175 s more sensitive to the fluctuations of mean solar radiation in hot arid regions.

176 tones/aldehydes in crude oil when exposed to solar radiation in laboratory experiments, whereas biode

177 itivity of plants under the broad spectra of solar radiation in nature.

178 ment in response to different wavelengths of solar radiation in nature.

179 6 h, corresponding to 3 to 6 days of natural solar radiation in summer at the sampling locations.

180 Due to the attenuation of solar radiation in the indoor environment, the possibili

181 ure regimes, absolute and relative inputs of solar radiation in ultraviolet and photosynthetically ac

182 enetration, which is primarily a function of solar radiation incidence and water clarity.

183 ate climate change by intentionally reducing solar radiation incident on Earth's surface.

184 tal productivity is the product of the total solar radiation incident per unit land area and the effi

185 ed uniform photoprotective responses to high solar radiation, including increased de-epoxidation of p

186 aches based on satellite indices of absorbed solar radiation indicate marked heterogeneity in NPP for

187 candidates that consent a noteworthy dynamic solar radiation Infrared (NIR-IR) regulation and hence a

188 , we demonstrate that UV-B levels present in solar radiation inhibit maize (Zea mays) leaf growth wit

189 d fuzzy_DS methods at 20 points with various solar radiation intensities and the number of dusty days

190 Y182H is significantly correlated with lower solar radiation intensity in East Asia and infer that MF

191 a and climate model outputs, we characterize solar radiation intermittency to assess future photovolt

192 The optical conversion of incoherent solar radiation into a bright, coherent laser beam enabl

193 Using photovoltaics (PV) to directly convert solar radiation into electricity for battery electric ve

194 erns in a lake survey: higher penetration of solar radiation into lakes correlated with smaller epide

195 the aerosol effect on the shallow clouds and solar radiation is -11 +/- 3 W/m2 for the 3 months studi

196 Solar radiation is a versatile source of energy, convert

197 energy contained with the UV wavelengths of solar radiation is absorbed within the epidermis and upp

198 UVB from solar radiation is both an initiating and promoting agen

199 ops and increasing the efficiency with which solar radiation is converted into biomass has recently b

200 Thus the spectral composition of solar radiation is crucial in determining atmospheric st

201 chromatic where there are fewer pollinators, solar radiation is high, precipitation and net primary p

202 forests increases with climate change and as solar radiation is higher during droughts, the trade-off

203 easonal variations of [Formula: see text] If solar radiation is in phase with water availability, sum

204 model of Triton's atmosphere, in which only solar radiation is present, predicts a large column of c

205 loroplasts, where a fraction of the absorbed solar radiation is reemitted at longer wavelengths by ph

206 spectral range of 290-320 nm of terrestrial solar radiation is responsible for formation of cyclobut

207 ction, even in rainforests where much of the solar radiation is shielded by the forest canopy.

208 ucture, as a broader part of the spectrum of solar radiation is used and the thermalization loss of p

209 Latitude, a proxy for solar radiation, is a dominant driver of snow-free date,

210 Black carbon (BC) absorbs solar radiation, leading to a strong but uncertain warmi

211 osses more than changes in precipitation and solar radiation, leading to strongest impacts in tempera

212 research has been devoted to trends in mean solar radiation, less attention has been paid to its int

213 oling of the climate may provide a basis for solar radiation management (SRM) geoengineering.

214 "upstream" climate interventions, including solar radiation management techniques and carbon dioxide

215 , the changes are related to obliquity-paced solar radiation, manifest as variations in total summer

216 The parasite's sensitivity to solar radiation may underlie patterns in a lake survey:

217 model simulation and the other inferred from solar radiation measurements made over a 12-year period

218 ty, then the injection of some materials for solar radiation modification might significantly increas

219 all (positive at the C. panamensis site) and solar radiation (negative at the C. panamensis and Cyper

220 compensated by their reflection of incoming solar radiation (negative radiative forcing).

221 (0.2 mum) samples were exposed to artificial solar radiation of 350 W m(-2) for 48 to 96 h, correspon

222 the wavelength dependence of the effects of solar radiation on biological and ecological processes;

223 V radiation obscured facilitative effects of solar radiation on biotic decomposition.

224 The effects of pH and solar radiation on Fe dissolution have also been explore

225 fects of pH, simulated cloud processing, and solar radiation on iron solubility have been explored.

226 f daily minimum and maximum temperatures and solar radiation on rice yields in tropical/subtropical A

227 d (IR) and visible light (Vis) components of solar radiation on skin and their interaction with UV is

228 studies have examined the effects of non-UV solar radiation on skin physiology.

229 We evaluated the effect of cultivar and solar radiation on the melatonin content of Capsicum ann

230 has amplified the effects on temperature of solar radiation on west-facing slopes.

231 nces the climate by scattering and absorbing solar radiation or acting as nuclei for cloud formation.

232 exert a systematic modulating effect on the solar radiation penetrating into the subsurface layers,

233 d ground-based data (soil moisture, downward solar radiation, precipitation and mean air temperature)

234 meters of 0.2 to 0.4 micrometer experience a solar radiation pressure force as much as twice the forc

235 of the 2- to 4-astronomical unit region, the solar radiation pressure must be 1.4 to 1.8 times the fo

236 avitational effects of the sun and moon, and solar radiation pressure) to reduce their propellant and

237 is also investigated in this work, like the solar radiation pressure, gravity of the Moon and oblate

238 ch 2009, evolving slowly under the action of solar radiation pressure, in agreement with independent

239 imate balance of gravitational attraction by solar radiation pressure.

240 craft, autonomously stabilized by modulating solar radiation pressure.

241 ion of the ejecta with the binary system and solar radiation pressure.

242 UVB is a component of solar radiation primarily responsible for causing damage

243 ers (i.e., TiO2 and ZnO nanoparticles) under solar radiation produces significant amounts of hydrogen

244 Renewable natural resources, such as solar radiation, rainfall, wind, and geothermal heat, to

245 t wavelengths as long as 355 nm pertinent to solar radiation reaching a large portion of Titan's atmo

246 severe aerosol pollution over China reduces solar radiation reaching the surface.

247 Solar radiation reaching this planet is distributed over

248 of the Southern Westerly Winds that enhanced solar radiation receipt (and ablation) at the ice sheet

249 Modeling showed that high solar radiation, reduced water depth and wind speed, and

250 they influence climate by absorbing incoming solar radiation resulting in a highly uncertain warming

251 At low latitudes the solar radiation should result in a weak planet-wide glow

252 ved from delta(13) C, growth temperature and solar radiation, showed meaningful agreement with inferr

253 Mean annual precipitation and solar radiation (SR) modified the trade-off.

254 Accurate solar radiation (SR) prediction can substantially lower

255 and minimum temperature (T(max) and T(min)), solar radiation (SR), wind speed (WS), vapor pressure de

256 It was found that surface solar radiation (SSR) decreased considerably with wind s

257 Most proposals involve managing incoming solar radiation such that future greenhouse gas forcing

258 rge sample exposed to high levels of ambient solar radiation, sun protection and skin examination pra

259 witnessed strong negative trends of surface solar radiation, surface evaporation, and summer monsoon

260 ment probably due to varying factors such as solar radiation, temperature, brine volume, and atmosphe

261 ssessed considering environmental variables (solar radiation, temperature, chlorophyll a concentratio

262 The AS receives 200-800% higher solar radiation than the ES.

263 e the spectral components of the ultraviolet solar radiation that cause significant oxidative damage

264 rth's albedo, i.e., the fraction of incident solar radiation that is reflected back to space.

265 rations have a large impact on the amount of solar radiation that reaches Earth's surface.

266 nditions, such as atmospheric turbulence and solar radiation, that affect CO(2) exchange between leav

267 direct and indirect reduction of short-wave solar radiation, the increased cloudiness and cloud liqu

268 Apart from broadband absorption of solar radiation, the performance of photovoltaic devices

269 ere used to explore the associations between solar radiation, then ultraviolet B, and learning disabi

270 efficiently in skin by the UVA component of solar radiation through photosensitization reactions.

271 truments that measure spectral extinction of solar radiation throughout the entire atmosphere.

272 By causing more solar radiation to be reflected, cleaner snow/ice could

273 efficiency with which plant canopies convert solar radiation to biomass, we provide an upper-envelope

274 analysis we added location-specific modelled solar radiation to datasets of a previous observational

275 n memory of recent trends in temperature and solar radiation to decide whether to feed on a particula

276 ar to solar cells, but instead of converting solar radiation to electricity, they are designed to uti

277 h, which uses the large per-photon energy of solar radiation to excite electrons, as in photovoltaic

278 re optically thin enough to allow sufficient solar radiation to penetrate through them and raise surf

279 Enhancement of the diffuse solar radiation to which lettuce plants were exposed cle

280 iour that will enable the dynamic control of solar radiation transmittance through windows.

281 ime series, an anomalous diffusion model for solar radiation transport in the cloudy atmosphere, and

282 n the future power supply and long-term mean solar radiation trends is spatially heterogeneous, showi

283 However, solar radiation turns into heat reducing the photovoltai

284 rms of strong decreases in measured incident solar radiation up to the mid-1980s, has monotonically i

285 gy input via leaf litter, increased incident solar radiation (UV and PAR) and increased algal product

286 oxidative environment, including ultraviolet solar radiation (UVR).

287 y changes in air temperature, precipitation, solar radiation, vapor pressure deficit and frost at a s

288 ), relative humidity (%), soil moisture (%), solar radiation (W/m(2)), specific humidity (kg/kg), and

289 FA, PFPrA, and PFBA with downward short-wave solar radiation was observed.

290 st electron transport in leaves under canopy solar radiation was shown to be a major contributor to t

291 Solar radiation was used as the surrogate variable to de

292 categories such as responses to temperature, solar radiation, water deficit, photosynthesis and cell

293 Significant variables (p < 0.05) included solar radiation, water temperature and water conductivit

294 In contrast, community-wide responses to solar radiation were predominantly positive.

295 ce and amount are primarily driven by summer solar radiation, which is controlled by the Earth's prec

296 Black carbon (BC) aerosol strongly absorbs solar radiation, which warms climate.

297 ely linked to elevated temperatures and high solar radiation, while the sensory profiles displayed ma

298 Increasing sea levels and altered rainfall, solar radiation, wind speed, waves, and oceanic currents

299 surface air also showed more net heating by solar radiation, with operative temperatures up to 4 deg

300 cal melanoma risk factor is ultraviolet (UV) solar radiation, with the highest risk associated with i