ライフサイエンスコーパス: relative humidity

1 /w (11% relative humidity) to 18.8% w/w (75% relative humidity).

2 mA h g(-1) in humid air ( approximately 10% relative humidity).

3 ame conditions in regards to temperature and Relative Humidity).

4 conditions (25 degrees C, approximately 100% relative humidity).

5 herically relevant conditions (1 atm and 30% relative humidity).

6 640 water activity (approximately 70.0-64.0% relative humidity).

7 y exposure to a dehydrating environment (42% relative humidity).

8 w (23% relative humidity) to 19.52% w/w (75% relative humidity).

9 o be stable in humid air ( approximately 40% relative humidity).

10 tent of the ionomer membrane by lowering the relative humidity.

11 amined with varying aerosol compositions and relative humidity.

12 llent stability even in ambient air with 40% relative humidity.

13 or 20 adsorption-desorption cycles up to 70% relative humidity.

14 n tropical cyclone size and mid-tropospheric relative humidity.

15 kness increases reproducibly with increasing relative humidity.

16 3.30) compared with moderate temperature and relative humidity.

17 used for the selective capture of CO2 in 65% relative humidity.

18 rown galls under normal, but not under high, relative humidity.

19 e vapors, dependent on the particle size and relative humidity.

20 hybrid to the A-DNA conformation, at 84-79% relative humidity.

21 frequency upon hybridization and at varying relative humidity.

22 cients on the initial HONO concentration and relative humidity.

23 high-intensity light, low [CO(2)], and high relative humidity.

24 ns above 10(-3) S/cm at 60 degrees C and 98% relative humidity.

25 high-intensity light, low [CO(2)], and high relative humidity.

26 room temperature (20 degrees C) gas with 0% relative humidity.

27 ditional upon high light intensities and low relative humidity.

28 es between green and yellow depending on the relative humidity.

29 are exposed to nitrogen dioxide at different relative humidity.

30 week, temperature, barometric pressure, and relative humidity.

31 at below 100 degrees C, depending on the air relative humidity.

32 on mica at room temperature as a function of relative humidity.

33 glycerol, and squalane at approximately 75% relative humidity.

34 water adsorbed increases with an increase in relative humidity.

35 2.3x10(-3) S cm(-1) at 90 degrees C and 95 % relative humidity.

36 s also observed to be more humid with higher relative humidity.

37 stharvest dehydrated at 20 degrees C and 41% relative humidity.

38 d storage in ambient with approximately 70% relative humidity.

39 luted urban areas under conditions of modest relative humidity.

40 egrees and 78 degrees C) and close to 90% of relative humidity.

41 th increasing drying temperature for a given relative humidity.

42 was performed at 18 degrees C and different relative humidities.

43 ater water adsorption when exposed to higher relative humidities.

44 Studies of temperature (5-32 degrees C) and relative humidity (0 and 80% RH) dependence revealed tha

45 p to 18 months) and a control condition (47% relative humidity, -20 degrees C).

46 denuders declined by 4-60% during spikes of relative humidity (25 to 75%).

47 A comparison of CO2 release properties (75% relative humidity, 25 degrees C) from complexed powders

48 having been pre-equilibrated under different relative humidities (3, 10, 20, 40%) of water vapor.

49 In the growth chamber at low relative humidity (30%), culturable amounts of the nonto

50 y relevant temperature (10-30 degrees C) and relative humidity (30-100%) conditions, such that 943 Ks

51 ures (20 degrees C and 30 degrees C) and two relative humidities (33% and 52%) under strictly control

52 with acidic aerosol (pH = 1) and low ambient relative humidity (40%).

53 ture control within the recommended range of relative humidity (45%-65% RH) set by the American Socie

54 kept in nine different equilibrium levels of relative humidity (8.2-97.3%) at 20, 30 and 40 degrees C

55 high oxygen partial pressure, high moisture (relative humidity = 90% at 85 degrees C), corrosive agen

56 major hypothesis driving this work was that relative humidity affects collection of GOM on KCl-coate

57 were characterized in terms of temperature, relative humidity, air pressure, and wind speed.

58 The second adlayers, observed at higher relative humidity, also appear icelike, and thicker laye

59 contracting of the hydrogels in response to relative humidity alters the polarity of the environment

60 osed in the APXPS chamber up to 5 Torr ( 28% relative humidity), an increase in the amount of ionic b

61 environmentally relevant O3 concentrations, relative humidities and protein phase states (amorphous

62 controlled desiccating environment (15%-25% relative humidity and 2-5 L/min airflow) for 90 minutes.

63 roton conductivity (4.5 x 10(-4) S/cm at 98% relative humidity and 25 degrees C) of MFM-500(Ni) is me

64 ditions were adopted: accelerated aging (84% relative humidity and 30 degrees C, up to 9 months) and

65 nt material, to 2.1 x 10(-2) S cm(-1) at 90% relative humidity and 85 degrees C, while maintaining th

66 der hydroperoxyl-dominant conditions for <5% relative humidity and at 20 degrees C in the presence of

67 mass sensitivity at the zeptogram scale for relative humidity and CO(2) detection.

68 n binary and ternary mixtures, Dw depends on relative humidity and follows a simple compositional Vig

69 The increases in relative humidity and intensity of T(2) maps were also c

70 el results and omit optical focusing at high relative humidity and of involatile components.

71 e models may double-count plant feedbacks on relative humidity and other surface variables, leading t

72 density of human, coverage of built-up land, relative humidity and precipitation were significant pre

73 sses in organic aerosols will depend on both relative humidity and temperature and thus altitude.

74 e the potential magnitudes of the effects of relative humidity and temperature on M(o) levels must be

75 a 2009 pandemic strain shows a dependence on relative humidity and temperature very similar to that o

76 most likely to show sensitivity to changing relative humidity and temperature.

77 ls may potentially be affected by changes in relative humidity and temperature.

78 uce sensitivity in M(o) levels to changes in relative humidity and temperature.

79 ility was evaluated at different equilibrium relative humidity and temperatures.

80 a reverse J-shaped relationship between mean relative humidity and the risk of gout attacks (P = 0.03

81 1.3 nm, the H2 production increases with the relative humidity and thus with the water amount.

82 nt of cooling is dependent on the drip rate, relative humidity and ventilation.

83 ning 400-530 ppm CO2 at 30 degrees C and 60% relative humidity and with CO2 desorption at 90 degrees

84 h) increased with increasing temperature and relative humidity and with decreasing soil organic carbo

85 Bulgur must be stored below 70% relative humidity and with less than 10 g water per 100

86 in climate (temperature, precipitation, and relative humidity) and agricultural characteristics (whe

87 , [OH], UV light lambda = 185 and/or 254 nm, relative humidity) and PF film surface density (0.38-3.8

88 nds on the water content (as measured by the relative humidity) and temperature of the environment, w

89 es g(s) as a function of Anatomical g(smax), relative humidity, and [CO(2)] at the leaf.

90 to a controlled normal condition (23 C, 45% relative humidity, and air flow 0.10 m/s) and a controll

91 that simulates desiccating stress (23 C, 5% relative humidity, and air flow 0.10 m/s).

92 s for geriatric pneumonia, mean temperature, relative humidity, and air pollution concentrations betw

93 rse droplet equilibration experiments at 75% relative humidity, and condensed-phase mass was measured

94 , CO(2) uptake remained similar whatever the relative humidity, and correlations were difficult for m

95 tional length, season of birth, temperature, relative humidity, and maternal characteristics.

96 At high relative humidity, and once the size of the confining su

97 The effect of air velocity, temperature, relative humidity, and particle concentration were furth

98 ge monthly minimum and maximum temperatures, relative humidity, and precipitation were calculated usi

99 r) combinations under different temperature, relative humidity, and soil organic carbon conditions.

100 nium nitrate and amines after an increase of relative humidity, and sulfate dominated when the air ma

101 nal lattice (T-phase) over a narrow range of relative humidity, and then to a phase of rhombohedral l

102 linity mainly depends on air temperature and relative humidity, and tide and wave actions dilute a fr

103 influence is not as strong as that of CAPE, relative humidity, and VWS, which increase MCSs' lifetim

104 particle morphology is present even at high relative humidity ( approximately 70%).

105 led temperature (from 5 to 35 degrees C) and relative humidity (approximately 40 and 80%) as well as

106 ught to undergo two phase transitions as the relative humidity around the particles is varied: efflor

107 ith pH values (controlled largely by ambient relative humidity) as low as -0.8 and strong acidity (co

108 details of water vapor (0.0-19.0 Torr; 0-96% relative humidity at 25 degrees C) adsorption at surface

109 fter exposure to harsh humid conditions (90% relative humidity at 353 K).

110 ted under accelerated conditions (75 and 90% relative humidity, at 35, 45, and 55 degrees C for 35day

111 d delta(13) C, is primarily to variations in relative humidity, but by different processes.

112 e nature of the exchangeable cation, and the relative humidity by following the H2 production under e

113 water vapour (c. - 200 per thousand) at high relative humidity (c. 93%) for 5 h, simulating a fog eve

114 eceived warm (37 degrees C), humidified (98% relative humidity) CO(2) gas insufflation, whereas contr

115 esponse to environmental conditions, such as relative humidity, CO(2) concentration, and light intens

116 n certain weather conditions (e.g., very low relative humidity, cold weather).

117 results, omitted optical focusing under high relative humidity conditions and by involatile component

118 inoculation without additives under moderate relative humidity conditions permitted (1) a detailed an

119 osporium genera in different temperature and relative humidity conditions, and the square root model

120 rsity is resolved, we find Eabs=1-1.5 at low relative humidity, consistent with ambient observations.

121 ochemical cell, in air at 60 degrees C, with relative humidity controlled between 70% and 98%.

122 At constant relative humidity, CRE does not decrease with increasing

123 As the relative humidity cycles in the atmosphere and the water

124 Increasing relative humidity dampens the impact of the perturbation

125 e show that satellite-based near surface air relative humidity data can further improve drought onset

126 ned for drought monitoring, we show that its relative humidity data offers a new and unique avenue fo

127 n films with the extent of nitrate formation relative humidity dependent.

128 were exposed to controlled low humidity (5% relative humidity, desiccating environment) for 2 hours

129 tio of the particle diameter at a particular relative humidity divided by the dry particle diameter (

130 ibution, chemical composition, deliquescence relative humidity (DRH), acidity) and meteorological par

131 ers reaches levels of about 4% above ambient relative humidity due to additive evapotranspirational w

132 ater to hydrophobic surfaces exposed to high relative humidity due to its hygroscopic properties.

133 h are essential for stability within the low relative humidity environment of the Martian atmosphere.

134 el about half of the adsorbed water when the relative humidity exceeds a 50-80% threshold.

135 .5 mul/l of ethylene at 21 degrees C and 80% relative humidity for 72 h, while non-degreened fruits w

136 -PAH, PNC, and NOx, and air temperatures and relative humidity for PM2.5.

137 uthpiece with optimized performance reducing relative humidity from 95% (27,000 ppmV) to 29% (8000 pp

138 the latter requiring only delta(18)O(a) and relative humidity (h) as inputs.

139 tinue to be affected by flooding, even after relative humidity has returned to baseline levels and re

140 Elevated relative humidity has the potential to affect significan

141 The MOF becomes amorphous in >60% relative humidity; however, impedance analysis of pellet

142 s and elastic constants that is invariant to relative humidity, implying a critical strain of approxi

143 f TAA cations (C2-C8) were calculated at 14% relative humidity in air to be 1.36, 1.18, 1.03, 0.90, 0

144 weaker turbulence, may contribute to higher relative humidity in the surface layer during polluted c

145 moisture divergence and reduces tropospheric relative humidity in the tropics and subtropics, in conj

146 the 20-80% RH range studied, the increase in relative humidity increased CO2 capacity of NFC/PEI foam

147 As the relative humidity increases, adjacent rods (confining su

148 This paper introduces the Standardized Relative Humidity Index (SRHI) based on the NASA Atmosph

149 lly nonlinear when struvite was dried at low relative humidity, indicating bacterial persistence.

150 tion upon deliquescence/liquefaction at high relative humidity, indicating that the observed concentr

151 a Center and Weather Service measurements of relative humidity (%), indoor heating degree days (HDD),

152 a Center and Weather Service measurements of relative humidity (%), indoor heating degree days, preci

153 examined how different liquid sweeteners and relative humidity influenced greening of sunflower butte

154 , such as chamber volumetric residence time, relative humidity, initial concentration of oxides of ni

155 Survival to low relative humidity is a complex adaptation, and many repe

156 ns, their NO conversion drops to 0% when 50% relative humidity is added.

157 ngredients undergo dissolution at a critical relative humidity known as the deliquescence point (RH0)

158 The xis = 0.70-0.91, with lower relative humidity leading to both higher mass and number

159 liters of water per kilogram of MOF daily at relative humidity levels as low as 20% and requires no a

160 lest Criegee intermediate, CH2OO, at various relative humidity levels up to 85% at 298 kelvin.

161 ydrosphere via temperature driven changes in relative humidity levels.

162 lower with the highest-quartile mean annual relative humidity (logistic regression, adjusted odds ra

163 r with second and third quartile mean annual relative humidity (logistic regression, P </= .01 for bo

164 e glassy state (25+/-2 degrees C and 65+/-2% relative humidity) lost glycerol and water over time, as

165 tions studied is maximum at low pH and lower relative humidities (<60% RH), i.e., when the aerosol is

166 as a function of controlled temperatures and relative humidities may provide additional information r

167 Further, composition analysis combined with relative humidity measurements suggests that heterogeneo

168 In a desiccating environment (<20% relative humidity), mosquitoes with reduced AgAQP1 prote

169 e wild type when samples are maintained at a relative humidity of </=85%.

170 yzed reactions promote NOx formation up to a relative humidity of 50%.

171 overlaps with the most hygroscopic mode at a relative humidity of 90% (0.10-0.32 mum).

172 fter the film had been exposed to air with a relative humidity of 95 % for over four hours, whereas C

173 Model calculations at a relative humidity of 99.5% reveal significant respirator

174 adapted to automatically control the desired relative humidity of an enclosed space.

175 since Rosalind Franklin recognized that the relative humidity of the sample had to be maintained to

176 cts of seed aerosol composition, acidity and relative humidity on OS formation were examined.

177 The promoting effect of the relative humidity on the CO(2) capture capacity and on t

178 tudies on the impact of both PEI content and relative humidity on the CO2 capture capacity of the ami

179 re, which can be actuated by either changing relative humidity or contact with water.

180 activity of just 0.585 ( identical with58.5% relative humidity), outside the currently understood the

181 response to CO(2)-radiative forcing, whereas relative humidity over land decreases in response to CO(

182 ains within aerosols at 22 degrees C and 80% relative humidity over time.

183 d (2) mixture properties (e.g., temperature, relative humidity, particle size distributions of both r

184 , orienting to gradients as shallow as 0.03% relative humidity per millimeter.

185 lely regulated by a simple adjustment of the relative humidity, positioning this hydrolytically stabl

186 ccordingly, maintaining these animals at 90% relative humidity prevented lethality.

187 elationship between the diurnal cycle of the relative humidity profile and E.

188 elation is that the vertical variance of the relative humidity profile is less than would occur for i

189 with variability in terms of temperature and relative humidity (R.H.).

190 When the sensors are exposed to relative humidity ranging from 10-80%, we observe signif

191 tion-exchange membranes, was investigated at relative humidity ranging from 25 to 75%.

192 tion of oxygen, carbon dioxide, ammonia, and relative humidity readable by a smartphone.

193 nd effloresce transitions, albeit at a lower relative humidity relative to pure sodium chloride.

194 ns of airborne biological spores at elevated relative humidity remain poorly understood and their cli

195 Relative humidity remains roughly constant in response t

196 further exposure of coated soot to elevated relative humidity results in a more spherical particle.

197 (>10(-4) S cm(-1) ) under both ambient (with relative humidity RH < 75%) and hot (T > 90 degrees C, R

198 4(2-),dark) under dark conditions at various relative humidities (RH) ranging from 20% to 80%.

199 0 = (0.6 - 15.0) x 10(12) molecules cm(-3)), relative humidity (RH = 3 x 10(-4) - 84.1%) and temperat

200 ) ammonium sulfate seeds at exactly the same relative humidity (RH = 70%) and state of wall condition

201 x and placed at 10, 20, or 30 degrees C, 45% relative humidity (RH) and 1.5m/s of air flow to dehydra

202 conductivity (5.0 x 10(-2) S cm(-1)) at 98% relative humidity (RH) and 25 degrees C.

203 nano-Wilhelmy methodologies as a function of relative humidity (RH) and ambient temperature condition

204 d on quantifying the effects of temperature, relative humidity (RH) and ascospore density in multiple

205 on of isoprene in a flow tube reactor at 70% relative humidity (RH) and room temperature in the prese

206 ity, based on variations in mid-tropospheric relative humidity (RH) and their impact on clouds, is pr

207 stored for 6 months at 25 degrees C and 60% relative humidity (RH) and under accelerated stability c

208 n limit of 32 ppbv with ca. 21 000 ppmv (90% relative humidity (RH) at 20 degrees C) water present in

209 gates composed of inorganic salts exposed to relative humidity (RH) between 0 and 80% after formation

210 iquescing and then drying the particles to a relative humidity (RH) between the phase separation RH a

211 lution of known concentration, the gas-phase relative humidity (RH) can be accurately measured with a

212 tion as multiple influencing factors such as relative humidity (RH) can distort the observed relation

213 hydrophilic films are carried out under one relative humidity (RH) condition.

214 ecules within their pores under low (30-35%) relative humidity (RH) conditions.

215 ingredients were generated using controlled relative humidity (RH) desiccators at temperatures from

216 eric lifetime or only (re)crystallize at low relative humidity (RH) due to the kinetic limitations of

217 ient storage at 25+/-3 degrees C and 70+/-5% relative humidity (RH) for up to 14days.

218 d samples stored at 1-2 degrees C and 85-90% relative humidity (RH) in air (Control samples), under c

219 ctroscopic ellipsometry over a wide range of relative humidity (RH) levels.

220 ection limit while sampling ambient air at a relative humidity (RH) of 40% is 0.6 ppt (1 min average,

221 (aw) of 0.5 were stored at 30 degrees C and relative humidity (RH) of 40-50%.

222 The ability to account for the role of the relative humidity (RH) of the aerosol prior to, and duri

223 Specific Surface Area of the soil (SSA) and Relative Humidity (RH) of the air-filled pore space.

224 PcTs for better understanding the effects of relative humidity (RH) on hydrophilic phthalocyanines, a

225 ase microextraction (HS-SPME) conditions and relative humidity (RH) on the release of volatile lipid

226 Temperature (T) and relative humidity (RH) strongly affect the partitioning

227 trary to previously held assumptions, at low relative humidity (RH) these particles are semisolid and

228 ucturally diverse set of OS salts at varying relative humidity (RH) using a Hygroscopicity-Tandem Dif

229 In contrast, the relative humidity (RH) was found to have a strong impact

230 py is 0.11 S cm(-1) at 90 degrees C and 100% relative humidity (RH) with a low activation energy of a

231 polymerizing already below 60 degrees C (65% relative humidity (RH)), whereas gliadin only is incorpo

232 running time, real-time sample mass, target relative humidity (RH), actual RH, and isotherm temperat

233 nvestigate how the ozone (O3) concentration, relative humidity (RH), and particle size control reacti

234 acidic or basic solids changes under higher relative humidity (RH), as determined by using Kelvin fo

235 ready under mild dehydration conditions (97% relative humidity (RH), corresponding to freezing at -3

236 Results show that adsorbed water at 30% relative humidity (RH), not light, increases the concent

237 cosity is comparable to that of honey at 90% relative humidity (RH), similar to that of peanut butter

238 etics of squalene and O3 were independent of relative humidity (RH), the RH significantly affected th

239 (WSOCp,dry) maintained at approximately 35% relative humidity (RH).

240 e demonstrated using H2O(g) as a function of relative humidity (RH).

241 ) while responding to changes in the ambient relative humidity (RH).

242 s as a function of composition, acidity, and relative humidity (RH).

243 ph upon standing at room temperature and 90% relative humidity (RH).

244 pendent on the environmental temperature and relative humidity (RH).

245 of sulfur dioxide (SO2), ammonia (NH3), and relative humidity (RH).

246 egative water vapor adsorption at ca. 40-50% relative humidity (RH).

247 lowing changes in the particle diameter with relative humidity (RH).

248 y the shallow PBL, leading to an increase in relative humidity (RH); (2) the high RH induces an incre

249 oot did not exhibit increased M.A.C. at high relative humidity (RH); however, lab-generated soot coat

250 g methods hot air (HA), 50 degrees C, 58-63% relative humidity (RH); low humidity air (LHA), 50 degre

251 he solid particles, ammonia exposure at high relative humidity (RH; > 94%) induced a first-order deli

252 s to 5 ppm sulfur dioxide at arid (23 +/- 1% relative humidity, RH) and marine (98 +/- 1% RH) conditi

253 ormed from the ozonolysis of alpha-pinene at relative humidities (RHs) up to 87% at 297 +/- 2 K (whic

254 linked Na-caseinate were stored at different relative humidities (RHs; approximately 0%, 11%, 33%, 54

255 ials pre-equilibrated at three levels of air relative humidity (RHs 52, 73, and 92%).

256 te factors, especially temperature (TEM) and relative humidity (RHU), while H5N1 infections correlate

257 y liquid in tropical and polar air with high relative humidity, semi-solid in the mid-latitudes and s

258 The resistive relative humidity sensor was developed using a filter pa

259 ormed at room temperature and four different relative humidity settings (20, 50, 65, and 80% RH).

260 .8x10(-2) S cm(-1) at 22.5 degrees C and 98% relative humidity, single crystal).

261 icide Ksoil-air values based on temperature, relative humidity, soil organic carbon content, and pest

262 s as a significant predictor more often than relative humidity, solar irradiation, or temperature.

263 rate that greening can be promoted with high relative humidity storage, and use of high moisture and

264 controlled conditions (25 degrees C and 57% relative humidity), such as those found in health care s

265 ionship between f(part) of pinonaldehyde and relative humidity suggests that the aerosol water plays

266 d (40 +/- 6) %, respectively, independent of relative humidity, temperature, concentration of HONO an

267 ments have higher temperatures and different relative humidities than surrounding suburban and rural

268 IRMOF-3 is found to degrade at a lower relative humidity than MOF-5, a likely consequence of th

269 being their storage stability better at low relative humidity than that of the non-encapsulated cont

270 onductivities (up to 10(-3) S cm(-1) at high relative humidity) that compete with extended metal-orga

271 At atmospherically relevant relative humidities, the particulate chloride in the bio

272 At high relative humidity, there was no protection and low stora

273 nature with a growth factor up to 2.3 at 96% relative humidity, thus they may potentially influence c

274 the lowest water contents, we employed fixed relative humidities to control water films at nm thickne

275 ting for time, day of week, temperature, and relative humidity to investigate the association between

276 ange of moisture contents from 3.7% w/w (11% relative humidity) to 18.8% w/w (75% relative humidity).

277 nge of moisture contents from 7.34% w/w (23% relative humidity) to 19.52% w/w (75% relative humidity)

278 suppressed rainfall and reduced tropospheric relative humidity) under CO2 warming from Coupled Model

279 stability of this transparent conductor to a relative humidity up to 100% at room temperature for 25

280 articles decreased slightly upon increase of relative humidity up to 80%.

281 from ambient to supercooled temperatures at relative humidity up to 95%.

282 ) and natural aging (ambient temperature and relative humidity, up to 18 months) and a control condit

283 ts from 3.6% to 18.8%, which corresponded to relative humidity values of 11% and 75%.

284 he interactions between high temperature and relative humidity (vapor pressure deficit--VPD).

285 This stability is disrupted if relative humidity varies.

286 ures varying between 10 and 30 degrees C and relative humidities varying between 20 and 80%.

287 olatile pesticides and that the way in which relative humidity was accounted for was the most critica

288 A strong dependence upon relative humidity was also observed for uptake onto humi

289 r temperatures were substantially higher and relative humidity was lower than long-term averages.

290 d deviation) working ambient temperature and relative humidity were 29.6 degrees C (2.0 degrees C) an

291 to the mineral surfaces, K(min/air), at 60% relative humidity were fitted to experimental data and e

292 rom halites exposed to coastal fogs and high relative humidity were more diverse; their archaeal and

293 0.35 cm(3) mum day(-1) m(-2) kPa(-1) at 50% relative humidity, were produced from aqueous solutions

294 These results, in conjunction with the relative humidity, were used to obtain the equilibrium c

295 rs distinguish between subtle differences in relative humidity when other floral cues are held consta

296 of 6.45 x 10(-3) S cm(-1) (at 313 K and 100% relative humidity) which is among the highest values so

297 ed to solar radiation, horizontal heat flux, relative humidity, wind speed, soil moisture differences

298 onse of 12% for 0.5 ppm of TMA vapour in 54% relative humidity, with response and recovery times of 3

299 Near-infrared mapping reveals the relative humidity within prominent downwelling regions.

300 (up to 6months), temperature during storage, relative humidity within storage facilities, type of pac