ライフサイエンスコーパス: km

1 on foraminifera from a sediment core at 5.0 km in the northern subtropics show that there may have a

2 lly connected episodes with scales of >1,000 km and clearly coincide with large-scale meteorological

3 opomum), with an impact extending over 1,000 km from the rainforest city of Manaus (population 2.1 mi

4 ly-important nearshore habitats across 1,000 km of the California Current Large Marine Ecosystem.

5 -resolution (100 m x 100 m) regional (10,000 km(2)) CH4 flux map of the Mackenzie Delta, Canada, base

6 sland of Newfoundland (approximately 110,000 km(2)) and Labrador (approximately 295,000 km(2)) today

7 that spanned distances from 0.001 to 12,000 km.

8 es ("geoglyphs") occupy approximately 13,000 km(2) of Acre state, Brazil, representing a key discover

9 ariability observed over distances of 15,000 km.

10 , ice-free areas could expand by over 17,000 km(2) by the end of the century, close to a 25% increase

11 oil palm plantations ( approximately 188,000 km(2)) in Indonesia, the leading producer of palm oil, a

12 000 individuals and born 20 years and 20,000 km apart suggest that the association between childhood

13 osed subduction network approximately 22,000 km in circumference prior to 150 million years ago befor

14 0 km(2)) and Labrador (approximately 295,000 km(2)) today constitute a province characterized by abun

15 rn Europe during northward migration - 3,000 km from the nonbreeding grounds - but in males only.

16 Large marine protected areas (>30,000 km(2)) have a high profile in marine conservation, yet t

17 atial scales (up to [Formula: see text]4,000 km).

18 ples, whose ancestors had trekked some 5,000 km from the west coast, arrived approximately 10,000 cal

19 Coastal Louisiana has lost about 5,000 km(2) of wetlands over the past century and concern exis

20 is required to reduce hypoxic area to 5,000 km(2) The interim goal of a 20% load reduction is expect

21 the global positioning system as a 50,000 km aperture dark matter detector to search for such obje

22 nded its breeding range an exceptional 7,000 km when it began breeding 35 years ago in its regular wi

23 community data from 36 sites across a 75,000 km(2) region, and analyzed bee abundance, species richne

24 n 1869 to its current extent of over 900,000 km(2) in Eastern North America.

25 Focusing on a 100-km by 1,000-km transect spanning the State's fivefold east-west prec

26 density was objectively assessed within a 1 km street catchment of a participant's residence.

27 e core leads to an estimated approximately 1 km of ice thinning in northwest Greenland during the ear

28 nt nighttime illumination at approximately 1 km(2) scale for each residence during follow-up.

29 poor accuracy at all resolutions (e.g., at 1 km resolution, up to approximately 45% underestimates of

30 stence by regenerating a forest connection 1 km in width among the largest and closest fragments at 1

31 tion efforts underway, mule deer remained >1 km away from well pads.

32 tions vary sharply over short distances (<<1 km) owing to unevenly distributed emission sources, dilu

33 Here we use a novel, 1 km surface mass balance product, evaluated against in si

34 ap a contamination plume that extends over 1 km from the source of the contamination.

35 a global erosivity map at 30 arc-seconds( 1 km) based on a Gaussian Process Regression(GPR).

36 In this study, we combined two 1 km actual evapotranspiration datasets (ET), one obtained

37 the estimated amount of sulfur used within 1 km of child residence during the year prior to pulmonary

38 stimated agricultural pesticide use within 1 km of maternal residences during pregnancy using a geogr

39 entories from a large-scale network of 447 1-km(2) plots with remotely sensed indices of primary prod

40 Daily PM2.5 and ozone levels in a 1-km x 1-km grid were estimated using published and valida

41 e-bin and polarization entanglement over a 1-km-long FMF.

42 Daily PM2.5 and ozone levels in a 1-km x 1-km grid were estimated using published and validated air

43 ization knots at a rate of 28 GHz along a 10 km length of normally dispersive optical fibre.

44 and tilting over a breadth of only about 10 km.

45 tal respiratory disease cases residing at 10 km distance from a surveillance hospital.

46 ion distance sharply increased to 5.3 km (10 km when excluding infections linked to household and sch

47 f approach of a large commercial vessel, <10 km from the listening station, the communication space o

48 A horizontal displacement of 10 km developed at 50 km altitude before connecting to the

49 nature of the local plants in a radius of 10 km.

50 r beneath the center and deepens by up to 10 km beneath its southern and northern boundaries.

51 sal at spatial scales varying from 1 m to 10 km while maintaining a realistic spatial structure of sp

52 ree CsMPs (3.79-780 Bq) collected within 10 km from the FDNPP to determine the CsMPs' origin and mec

53 postcodes (average 12 households) within 10 km of MWIs in Great Britain (GB) in 2003-2010.

54 nutrient surveys in surface water along a 10-km stream reach over four visits spanning 18 y (1995-201

55 l wildfires ignited after the impact of a 10-km-diameter asteroid on the Yucatan Peninsula 66 million

56 p and show that it disappears beneath 60-100 km depth, marking the depth of dehydration metamorphism

57 About 100 km east of Rome, in the central Apennine Mountains, a cr

58 killer whales were present (within about 100 km), narwhal moved closer to shore, where they were pres

59 This was an area of approximately 100 km radius, including the location where resistance was f

60 adar (InSAR)] show broad ( approximately 100 km) aseismic uplift symmetrically spanning the fault zon

61 ute error (MAE, describing accuracy); at 100 km, up to 15% underestimates and nearly 20% MAE).

62 some were detected at large distances (>100 km) in snow and surface lake sediments, suggesting that

63 de mean of 5.6 L/100 km in 2014 to 3.0 L/100 km by 2030.

64 ovements from a fleet-wide mean of 5.6 L/100 km in 2014 to 3.0 L/100 km by 2030.

65 verlapping SAR tracks covering a region 100 km in extent.

66 this population is prevented by several 100 km of bear-free territories.

67 er maps at resolutions ranging from 1 to 100 km, and then calculated errors in several representative

68 Focusing on a 100-km by 1,000-km transect spanning the State's fivefold e

69 rule out the presence of a approximately 100-km-thick denser-than-average basal structure, our result

70 btained from 33 populations spanning a 1000 km gradient that encompassed the majority of the species

71 y among a network of MPAs spanning over 1000 km of coastline off the coast of eastern Australia.

72 s at relatively large distances of over 1000 km.

73 Maximum (LGM) and eventually retreated 1000 km to the current grounding-line position on the inner s

74 5 mum (PM2.5) and ozone at an approximate 11 km x 11 km resolution with satellite-based estimates, ch

75 M2.5) and ozone at an approximate 11 km x 11 km resolution with satellite-based estimates, chemical t

76 of temperature change (usually more than 110 km over 100 years) under a high-emissions scenario.

77 d spatial-segmentation along the entire 1100 km-long Cascades Arc.

78 lator (APSIM), driven by high-resolution (12 km) dynamically downscaled climate projections for 1995-

79 during the last deglaciation and spread 120 km apart along the south Texas shelf edge.

80 ases 10-100 times from 750 km to 1000-1250 km, with a smaller decrease at deeper depths, pointing t

81 At sites ranging from 0 to 134 km from the major AOSR upgrading facilities, we examined

82 st axis, stretching 230 km southwest and 140 km northeast of the DWH wellhead, and (2) in the eastern

83 tial autocorrelation was observed at 100-150 km and was stronger in urban ponds in both cases.

84 high electrical resistivity to at least 150 km depth, implying a cold stable state well into the upp

85 n oceanographic sampling line extending 1500 km westward of British Columbia (BC), Canada in June 201

86 , Swainson's Thrushes could survive the 1500 km flight between Alabama and Veracruz, Mexico.

87 m an Mw 9.2 earthquake that generated a 1600 km-long rupture along the Sumatran Megathrust and genera

88 nardo River, which was investigated for a 17 km stretch.

89 ve cloud close to the highest regions at 17 km altitude.

90 that evolutionary dispersal kernels were 17 km (95% confidence interval: 12-24 km) wide, while an ex

91 r (T eff 8000 K; log g = 4.0, v sin i 18 km s(-1)).

92 In this study, two CWT plants 10 and 19 km upstream of a reservoir left geochemical signatures i

93 sted kernel widths of 27 km (19-36 km) or 19 km (15-27 km) across two years.

94 who both injected drugs (</=7 miles (</=11.2 km)).

95 es) during the first wave: about 1.5 km (2.2 km if infections linked to household and school transmis

96 that the ocean was poorly ventilated at 4.2 km, with better ventilation above and below that depth.

97 wells stimulated during 2014 exist within 2 km of at least one recently constructed (2000-2014) dome

98 ed domestic groundwater wells exist within 2 km of one or more hydraulically fractured wells stimulat

99 ed domestic groundwater wells exist within 2 km of one or more recorded oil and gas wells producing d

100 Most of these eddies are 5-20 km in radius, less than the local first baroclinic defor

101 tential temperature level of 460 K (about 20 km or 60 hPa in tropics), the global circulation strengt

102 f new VO2 peak ) at a speed approximating 20 km race pace was reduced in HCHO and PCHO (90% CI: -7.04

103 the next century were far below (usually <20 km) that required to track the velocity of temperature c

104 DW mobility is remarkably enhanced up to 20 km s(-1) T(-1).

105 cting a common thermal niche despite a 2,200 km geographic distance and 13 degrees C difference in me

106 esoscale eddies with typical sizes of 30-200 km contain more than half of the kinetic energy of the o

107 e subsequent punctuated large-distance ( 200 km) grounding-line retreat may have been a highly non-li

108 uvenile (age 0 and 1) cod sampled along >200 km of the Norwegian Skagerrak coast.

109 rom the ground level could travel up to 2000 km from northern to southern China within two days.

110 verse populations of Scots pine along a 2000-km climatic gradient in Europe.

111 y 60 m and a horizontal extent exceeding 220 km.

112 heast to west-southwest axis, stretching 230 km southwest and 140 km northeast of the DWH wellhead, a

113 km(3) (all +/-17%; 1 MAF approximately 1.233 km(3)), while total annual water consumption has changed

114 s were 17 km (95% confidence interval: 12-24 km) wide, while an exhaustive set of direct larval dispe

115 er seasons that ranged between 5.51 and 6.24 km(2).

116 uxtaposed along a structure that excised 25 km of crust.

117 local scale (99% of transmission occurs <25 km), movement restrictions are predicted to be effective

118 Jay (Aphelocoma insularis), endemic to a 250 km(2) island.

119 arent secondary peak in agreement below 2500 km depth may reflect the degree-two lower mantle slow se

120 The shifted distance on average covers 259 km, 9% of range extent.

121 opped below 50% at distances greater than 26 km for severe neurological disease and at distances grea

122 l widths of 27 km (19-36 km) or 19 km (15-27 km) across two years.

123 l observations suggested kernel widths of 27 km (19-36 km) or 19 km (15-27 km) across two years.

124 simulation was conducted over East Asia (27-km) and over South Korea (9-km) to assess the impact of

125 age stack) for detecting peatlands in a 2715 km(2) area in the high elevation mountains of the Ecuado

126 scending melt has previously been imaged 28 km northwest of the volcano, while to the south, the vol

127 s to 2060 indicate loss of an additional 286 km of stream across the region, as well as continued rep

128 ng' effects on natural habitats located >1.3 km away.

129 n in forest primary productivity along a 3.3 km elevation gradient in the Amazon-Andes.

130 ansmission distance sharply increased to 5.3 km (10 km when excluding infections linked to household

131 that the maximum effective dispersal is 8.3 km.

132 e mid-latitude NAA transmitter is due to a 3 km reduction in the effective height of the nighttime io

133 A high resolution (3 km foot print) SM/ST dataset prepared from a land data a

134 biodiversity and aquatic habitat along ten 3-km sites within the Upper Neosho River subdrainage, KS,

135 rate megacorer deployments inside a 30 by 30 km seafloor area.

136 and repeatedly sampled every street in a 30-km(2) area of Oakland, CA, developing the largest urban

137 Intermediate-depth earthquakes (30-300 km) have been extensively documented within subducting o

138 h a tick bite in the province of Avila - 300 km away from the province of Caceres, where viral RNA fr

139 ions, with a minimum sea-travel range of 300 km per generation; (ii) leapfrog coastal dispersals yiel

140 e constellation at galactic velocities 300 km s(-1).

141 res within countries were similar within 300 km, suggesting an appropriate spatial scale for surveill

142 rmed long-distance flights of more than 3000 km, highlighting the key importance of a single stopover

143 al surveys of two ("East" or "West") 35 x 35 km grids, two aircraft-based mass balance methods measur

144 oximately 1.1M individuals who ran over 350M km in a global social network over 5 years.

145 flux after 2010, ranged from 12805 to 35425 km(2).

146 avel a median distance of 10.79 miles (17.36 km) to reach the nearest abortion clinic, although 20% o

147 ions suggested kernel widths of 27 km (19-36 km) or 19 km (15-27 km) across two years.

148 dramatically from approximately 0.97 to 5.37 km(3) (all +/-17%; 1 MAF approximately 1.233 km(3)), whi

149 miting agricultural pesticide use within 0.4 km of schools and childcare facilities.

150 across a sampling grid measuring 32.9 x 28.4 km in Memphis, Tennessee.

151 These swarms struck a high-attenuation 3-4 km deep reservoir of supercritical fluids under Pozzuoli

152 lip of approximately 1.7 m occurred around 4 km depth from the surface.

153 lluted environment, and to altitudes up to 4 km.

154 4.8 x 10(-13) mol cm(-2) s(-1)) and pH 3.4 (km = 3.2 x 10(-13) mol cm(-2) s(-1)).

155 However, the 0.4-km buffer may not be appropriate for all pesticides beca

156 g species' shifts by an average of 90 +/- 40 km.

157 the local environmental conditions, along 40 km of NW Mediterranean subtidal rocky shores (Corsica, F

158 ed 40-69 years who lived within 25 miles (40 km) of one of 22 assessment centers in England, Wales, a

159 Although situated approximately 400 km from the east coast of Africa, Madagascar exhibits cu

160 to historical data from sites spanning >400 km.

161 rn end of C. rubescens' range originated 400 km to the north, at the centre of the species' range, wh

162 soil layers (0-10 and 10-20 cm) along a 4000-km climate transect in two grassland biomes of China, th

163 The low-velocity layer (LVL) atop the 410-km discontinuity has been widely attributed to dehydrati

164 would have had to travel 42.54 miles (68.46 km) or more.

165 reshocks leading to the mainshock within 0.5 km distance, suggesting existence of precursory aseismic

166 rt measures of [Formula: see text] up to 0.5 km.

167 infectees) during the first wave: about 1.5 km (2.2 km if infections linked to household and school

168 istance travelled to and from games was 41.5 km.

169 tional variation in the species pool above 5 km.

170 ed is 6.86 x 10(17) m(3) (or approximately 5 km of global equivalent layer, GEL).

171 account 65% of the co- variability (below 5 km) in the outer tropical (10-25 degrees N) central Paci

172 e achieved assuming low spatial dispersal (5 km) and delayed stages up to two years (temporal dispers

173 In addition to reporting 5 x 5 km estimates, we also aggregated results obtained from t

174 neonatal mortality at a resolution of 5 x 5 km grid cells across 46 African countries for 2000, 2005

175 ity aircraft data and oversampled on a 5 x 5 km(2) grid, to map surface air HCHO concentrations acros

176 vertical displacement of an approximately 5-km(2) area that is consistent with the footprint of an e

177 ecorded for urban and nonurban ponds at 0-50 km (distance between pond study sites) and negative spat

178 d in the Severn River (UK), approximately 50 km upstream of the estuary (i.e. not "in the Severn Estu

179 geographical resolution of approximately 50 km x 50 km.

180 ntal displacement of 10 km developed at 50 km altitude before connecting to the lower ionosphere.

181 Long range flights (>50 km in 2 hours) occurred almost exclusively at night; at

182 At scales >50 km such connectivity is decreased, particularly across t

183 g that the impact of industry can extend >50 km.

184 er distances (99% of transmission occurs <50 km) they are not.

185 ll decrease from north to south along the 50 km length of the study area.

186 migrated through the landscape for up to 50 km, the pregnant woman from Isernia was probably local,

187 hical resolution of approximately 50 km x 50 km.

188 ars ago before migrating approximately 1,500 km westward at an average rate of 1 cm year(-1), indicat

189 ground track for distances of at least 1,500 km.

190 ithic indicate that it expanded across 2,500 km in about 300 y.

191 entire geotherm to depths of at least 2,500 km, thus demonstrating that self-oxidation-reduction rea

192 ppe, covering a territory of more than 3,500 km in breadth.

193 -resolution upper crustal structure on a 500 km-long profile that is perpendicular to the LMS.

194 1930s, community peak abundance would be 500 km further south in the contemporary era.

195 17) survival probability over the entire 500 km study area compared to 0.199 (0.012) for the surgical

196 gentina [6], subsequently expanding over 500 km from its starting point [7-11].

197 ly short distance (with median value of 2.51 km).

198 d constant in the North Qinling Belt ( 45-55 km) during the Triassic to Jurassic but fluctuates in th

199 anical vs. thermal sources of support, a 550 km-long transect of magnetotelluric geophysical sounding

200 creased depth to groundwater and loss of 558 km of stream, and transformation of fish assemblage stru

201 ring 2000-2015 with a net decrease of 251.58 km(2)/year.

202 xpansion during 1975-1990 at a rate of 96.58 km(2)/year, rapid expansion during 1990-2000 of 213.65 k

203 The average locational error was 6 km (600%).

204 ip extending seaward, at least, to within 6 km of the deformation front.

205 t were assessed via surveys, and 1-mile (1.6-km) densities of supermarkets, fruit-and-vegetable store

206 gible villages were paired by proximity (<60 km) and the time that a free male circumcision outreach

207 The profiles cover 100- and 60-km transects across the Yarlung-Zangbo suture of the Him

208 he Southeast Asian records, from sites 2,600 km apart, suggests that the records reflect regional cha

209 n GNP and four in mountain ranges up to 600 km southwest.

210 Here we use moss bank cores from a 600-km transect from Green Island (65.3 degrees S) to Elepha

211 displayed a high coverage of peatlands (614 km(2) ) containing an estimated 128.2 +/- 9.1 Tg of peat

212 , rapid expansion during 1990-2000 of 213.65 km(2)/year, and a reversion during 2000-2015 with a net

213 imum dispersal distance of approximately 650 km.

214 deep-earthquake zone but stagnant below 660 km, consistent with tomographic imaging.

215 yond mining lease boundaries, causing 11,670 km(2) of deforestation between 2005 and 2015.

216 in diamonds coming from depths exceeding 670 km are obvious evidence that carbonates exist in the Ear

217 erage velocities of range movement between 7 km per decade northwards for taxa exhibiting niche plast

218 t 80% of tagged whale positions was near (<7 km) the closest suitable habitat.

219 c simulations with a spatial resolution of 7 km we obtain for the first time a direct estimate of the

220 ical disease and at distances greater than 7 km for fatal respiratory disease.

221 the Tarim Basin, Northwest China, down to 7 km depth is constrained using the anelastic strain recov

222 evels in Fort McMurray ( approximately 10-70 km downwind of the OS) are controlled by OS emissions; >

223 he eastern portion of the study area on a 70 km northeast to southwest axis near the DeSoto Canyon.

224 cantly increased Amazon forest loss up to 70 km beyond mining lease boundaries, causing 11,670 km(2)

225 g began at 240 Ma and culminated with 60-70-km-thick crust at 215 Ma.

226 s the largest tropical wetland area (800,720 km(2) ).

227 iet-Sun field-of-view of 60" x 60" (1" = 725 km).

228 were 3941.16, 5389.92, 7526.38, and 3752.74 km(2) of ADL in the above 4 periods, accounting for 28.5

229 ation during the non-breeding season was 743 km, covering 10-20% of the maximum width of Africa/South

230 t viscosity increases 10-100 times from 750 km to 1000-1250 km, with a smaller decrease at deeper d

231 t consumption each year ( approximately 1.76 km(3) on average).

232 The excess red-shift first appeared with 0.8 km.s(-1) impacts.

233 d (19.0% vs 16.6%), and those who lived 12.8 km (8 miles) or more away from the index hospitals (23.7

234 Here, the authors have discovered a 4-8 km thick mushy zone at the inner core boundary beneath t

235 present seismic evidence for a localized 4-8 km thick zone across the inner core boundary beneath sou

236 ting in a mushy zone with a thickness of 4-8 km.The existence of a mushy zone in the Earth's inner co

237 ribution ranges of any European amphibian (8 km(2)) and is considered critically endangered by the In

238 hese massive eruptions has been found >2,800 km from Mount Takahe.

239 essions in Myanmar's Hukaung Valley ( 21,800 km(2)).

240 n crustal seismic velocity model for an 800 km section of the active South American Cordillera (Puna

241 will become favored in the current core 800 km eastward of their current location.

242 In total, the CV encompasses 15% of CA, 8415 km(2) of which was identified as potentially land-sparin

243 er seasons that ranged between 7.68 and 9.88 km(2), and for two summer seasons that ranged between 5.

244 = 1,247-4,214) over the approximately 25,880-km(2) fishery.

245 The average velocity of the centroid is 5.89 km.yr(-1) .

246 0-100 cm of soils across a total of 24 945.9 km(2) of tidal wetland area, twice as much carbon as the

247 were within 1 order of magnitude for pH 7.9 (km = 4.8 x 10(-13) mol cm(-2) s(-1)) and pH 3.4 (km = 3.

248 er East Asia (27-km) and over South Korea (9-km) to assess the impact of meteorology under constant a

249 rations on the ionospheric D-region at 60-90 km altitudes.

250 vant EOC and EEM data were obtained for a 90 km stretch of the Simeto River, the main river in Sicily

251 to 42.8 +/- 1.2 dB in a link comprised of 90 km of installed fiber with additional optical attenuatio

252 Differences in range shifts were up to 900 km in a recent warming period, with average velocities o

253 rom approximately 3.37 to approximately 3.98 km(3) (+/-20%).

254 for taxa exhibiting niche plasticity and 99 km per decade for taxa exhibiting niche conservatism.

255 that 5-CQA exerts a mixed type inhibition as km increased and Vmax decreased.

256 ensities range from 0.23 to 20.3 g CO2e/(bbl.km), exhibiting considerably greater variability than da

257 as much higher than the estimated whole-body km (0.03 d(-1)).

258 The reaction rate constants (km) for the dissolution of uranyl-vanadate (U-V) mineral

259 e calculate estimates of sea turtle density (km(-2)) in nearshore waters.

260 ock numbers and emission intensity (emission/km(2) ) by up to 47% and 32%, respectively, in developed

261 36% higher emission intensity (CH4 emissions/km(2) ) compared to that in nondrylands in 2014, due to

262 inite carbonation across scales ranging from km to sub-mm by combining aeromagnetic observations, out

263 1 kg km(-2) a(-1)) than icebergs (0.0-1.2 kg km(-2) a(-1)).

264 h suspended sediment than icebergs (0-241 kg km(-2) a(-1)).

265 xport more acid-soluble iron (27.0-18,500 kg km(-2) a(-1)) associated with suspended sediment than ic

266 ts more filterable (<0.45 mum) iron (6-81 kg km(-2) a(-1)) than icebergs (0.0-1.2 kg km(-2) a(-1)).

267 rease with depth constituting a 7.8 to 12 kg/km(2) reservoir of Cr(VI) in soil.

268 0 mg/kg, or two times per week at 4 and 6 mg/km on weeks 1 and 2 of 3-week repeated cycles.

269 nant (>80% of ignitions) in over 5.1 million km(2), the vast majority of the United States, whereas l

270 More than 3 million km(2) of forest, grassland and shrublands were converted

271 pical forest edges sums to nearly 50 million km.

272 ropical wetlands estimates reach 4.7 million km(2) (Mkm(2) ).

273 rted fires were dominant in only 0.7 million km(2), primarily in sparsely populated areas of the moun

274 mula: see text] eqa(-1), and 1.5-2.8 million km(2), while providing the health cobenefits of adopting

275 in the morning peak and from 2.8 to 5.3 min/km in the evening peak.

276 e from 2.1 to 3.1 minutes per kilometer (min/km) in the morning peak and from 2.8 to 5.3 min/km in th

277 For each 10-minute-km increase in upwind congestion within 150 m, the odds

278 igestion time (hrs), average daily movement (km h) and numbers of viable seagrass seeds excreted (per

279 marsh sediments remove an average of 3.6 t N km(-2) y(-1) compared to 0.9 t N km(-2) y(-1) in unveget

280 of 3.6 t N km(-2) y(-1) compared to 0.9 t N km(-2) y(-1) in unvegetated sediments.

281 of tens of GHz and velocities up to tens of km/s.

282 tensive (continuous for tens to thousands of km) layers comprise fish and zooplankton and are readily

283 cit and frost at a spatial resolution of one km.

284 The BC mass emissions per passenger-km were similar to gasoline vehicles, but the number-bas

285 ally from tens to hundreds of dead trees per km(2) , rising dramatically during the fourth year of dr

286 ts per km(2), an increment of 1000 units per km(2) was positively related with adiposity, being assoc

287 0 kg/m(2)) on residential density (units per km(2)), adjusting for activity-influencing built environ

288 elow a residential density of 1800 units per km(2), an increment of 1000 units per km(2) was positive

289 Beyond 1800 units per km(2), residential density had a protective effect on ad

290 ential density of 1800 residential units per km(2).

291 velocity of approximately 1.4 +/- 0.5 nm/ps (km/s), in close agreement with the expected speed of sou

292 at 540 river sites (representing 82954 river km) in 2008-2009, and analyzed samples for 50 persistent

293 of the national sampled population of river km, and in 70% of the urban sampled population.

294 of 21.3 (95% CI 17.8, 24.7) grey reef sharks/km(2), which is an order of magnitude lower than the est

295 tectable in melted snow, except at one site (km = 0.0007 d(-1)).

296 lation rate constants were low in snowpacks (km = 0.001-0.004 d(-1)) and nondetectable in melted snow

297 , a similar size city, impacts <1,000 stream km, leading to only seven local extinctions.

298 cross four major river basins, 12,500 stream km, and contribute to 100 local extinctions of aquatic s

299 s produced at a rate of 0.3 to 4.8 kg Cr(VI)/km(2)/yr and subsequently flushed from soil during water

300 nfiltration, exporting 0.01 to 3.9 kg Cr(VI)/km(2)/yr at concentrations ranging from 25 to 172 mug/L.