ライフサイエンスコーパス: solar radiation

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

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

3 sensitive to changes in both temperature and solar radiation.

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

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

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

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

8 energy transduction, and protection against solar radiation.

9 and negatively correlated with the amount of solar radiation.

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

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

12 depth and the consequent impacts on incident solar radiation.

13 tratosphere by smoke, which strongly absorbs solar radiation.

14 preventing skin damage resulting from acute solar radiation.

15 cause scattering and absorption of incoming solar radiation.

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

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

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

19 erosols enhance scattering and absorption of solar radiation.

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

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

22 erogeneity modulated impacts of rainfall and solar radiation.

23 nditions with PAM fluorescence under natural solar radiation.

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

25 diurnal cycles of the OVOC measurements and solar radiation.

26 getically this accounts for much of incoming solar radiation.

27 , including changes in exposure to mutagenic solar radiation.

28 es them the preferred target for terrestrial solar radiation.

29 ental chemical interactions of canopies with solar radiation.

30 romoting hydrogen production under simulated solar radiation.

31 ction in the stratosphere, blocking incoming solar radiation.

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

33 aytime GEM flux was strongly correlated with solar radiation.

34 chemical reactions initiated by high-energy solar radiation.

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

36 Solar radiation absorbed by marine phytoplankton can fol

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

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

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

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

41 Solar radiation alone did not inactivate B. subtilis spo

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

67 Under weak solar radiation and stagnant moist meteorological condit

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

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

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

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

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

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

74 -400 m apart differ dramatically in aridity, solar radiation, and associated vegetation.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

101 Solar radiation causes immunosuppression that contribute

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

167 imate balance of gravitational attraction by solar radiation pressure.

168 craft, autonomously stabilized by modulating solar radiation pressure.

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

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

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

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

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

174 Solar radiation reaching this planet is distributed over

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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