ライフサイエンスコーパス: km

1 ide continental rifts, which can reach 1,000 km across, have been extensively studied in the North Am

2 journey: In Spring, they migrate over 1,000 km from their breeding grounds to the alpine regions of

3 mation radius, a length scale of order 1,000 km in the atmosphere and 100 km in the ocean, smaller th

4 t no work extended beyond 10 years and 1,000 km(2) [4, 5].

5 ng sites after extended (up to almost 10,000 km) migration to and from distant breeding sites as well

6 s from 66 large rivers (basin area > 100,000 km(2)) worldwide, we identify 34 GIWs, mostly distribute

7 re Shark Bay World Heritage Area (ca. 13,000 km(2) ) before (2002 and 2010) and after the MHW (2014 a

8 dest total CAMP volumes of 85,000 to 169,000 km(3) beneath the South Georgia Rift, consistent with mo

9 ty rates of up to 100% have destroyed 24,000 km(2) boreal forest since the 1960s, coincident with dra

10 polating to the whole Atlantic, over 260,000 km(2) of rock habitats potentially occur along Atlantic

11 to the total CRB province constitutes 31,000 km(3) of low-delta(18)O rocks.

12 natures across an area that covers ca 36,000 km(2) The results show that the area presents many more

13 acoustic array covering approximately 4,000 km(2) in MB.

14 ensor system with three satellites at 51,000 km altitude illustrates the feasibility of using radio-f

15 es (Orcinus orca; n = 3), in a large (63,000 km(2)), partially ice-covered gulf in the Canadian Arcti

16 ion Greenland ice-core record that is >7,000 km from Ilopango; and calculated that between 37 and 82

17 a humid to arid gradient covering >1,800,000 km(2) of continental eastern and central Australia.

18 n models, we found these fires burnt ~97,000 km(2) of vegetation across southern and eastern Australi

19 km(2) per year and a median value of $91,000/km(2) Wetlands confer relatively more protection against

20 Mean over-ground distance travelled was 2.03 km (+/- 0.71 km SD) with an over-ground average swim spe

21 ce, ~ 11 x 8 x 1 km; ~ 6.5 km depth; ~ 0.037 km(3)/year volume-change rate) and warming (0.3-0.4 degr

22 f disease spread is reduced from 5.18 to 1.1 km per year.

23 e above three variables were computed at a 1 km radius buffer zone around these locations; these valu

24 e ground-level PM(2.5) concentrations at a 1 km resolution during the October 2017 California wildfir

25 e cover, and cropland extent, as well as a 1 km resolution map of global pasture land, to estimate th

26 g experiment with plots distributed across 1 km(2) of treeline birch (Betula pubescens) forest and wi

27 nts into a random forest model to generate 1 km daily PM(2.5) estimates.

28 ude of CO(2) variability near the ground (~1 km altitude) at an airport was correlated with the inten

29 d the scale of short-distance dispersal (> 1 km), offering evidence contrary to the inverse isolation

30 parameters in fluids sampled from depths >1 km will present a challenge.

31 ddy deltaic protrusion at Camau; it was < +1 km(2)/year before 1400 years ago but increased drastical

32 differentiation among plots separated by < 1 km, with selection acting on growth and phenological tra

33 wo-month period as a focal coastal event (<1 km radius).

34 -estuarine ecosystems have a surface area <1 km(2) and are abundant in Mediterranean regions.

35 npredictable direction, covering a mean of 1 km horizontal distance from their last vocal position.

36 ed in areas protected by mangrove belts of 1 km or more.

37 tions feature a fine spatial resolution of 1 km to preserve spatial details.

38 With its large area of ~1 km(2) and perennial motions at ~10-20 mm per day, the Sl

39 ived, for the first time, high-resolution (1 km x 1 km) maps of the current and future forest biomass

40 ter data sets at high spatial resolution (~1 km) and for larger geographic units including uncertaint

41 f the two motorways included in the 17 1 x 1 km squares of the study area.

42 or the first time, high-resolution (1 km x 1 km) maps of the current and future forest biomass C dens

43 n InSAR-derived tabular source, ~ 11 x 8 x 1 km; ~ 6.5 km depth; ~ 0.037 km(3)/year volume-change rat

44 riability over the past four decades at a ~1-km resolution.

45 rminous United States from 1971 to 2015 at 1-km resolution using an enhanced dynamic global vegetatio

46 High-resolution (1-km) chemical transport model simulations predict stronge

47 6C4, with the ground resolution of about 10 km and a precision of about 10 milliGals.

48 were geographically separated by at least 10 km to minimise contamination.

49 ls of sequence divergence at both small (<10 km) and large (>600 km) spatial scales for four of the s

50 ion in 2012 at a high spatial resolution (10 km x 10 km) using a detailed, firm-level emission invent

51 2,918,089 births to mothers living within 10 km of at least one production well between January 1, 20

52 012 at a high spatial resolution (10 km x 10 km) using a detailed, firm-level emission inventory.

53 Storm deposits extended up to 10-km inland from the Gulf of Mexico.

54 ancy and abundance across 274 sites (10 x 10-km squares) over a 20-y time frame, we show a clear rela

55 ast one established population within 10-100 km of the boundaries of 89%-99% of protected areas, whil

56 redominant sulfur loss takes place at 70-100 km with a net delta(34)S composition of -2.5 +/- 3 per m

57 SD southern boundaries advance 100 km southward, and ArcTG boundaries are displaced about 5

58 operational ranges of 30 km, 65 km, and 100 km (UAS30, UAS65, and UAS100) and lifespans of 1000 to 1

59 of order 1,000 km in the atmosphere and 100 km in the ocean, smaller than the planetary scale and th

60 (SDLP; a measure of lane weaving) during 100 km, on-road driving tests that commenced at 40 minutes a

61 At smaller spatial scales (<100 km), sites showed heterogeneous patterns of low-level bu

62 system ranges between 4 and 22 leaks per 100 km of roadway in downtown Toronto, which is comparable t

63 ., daily), but rather can travel several 100 km off the direct routes to their goal before reorientin

64 radients of AGB density at scales below 1000 km.

65 Here we show that throughout a ~1000-km transect in Scots pine (Pinus sylvestris L.) forests

66 lithosphere with the constant thickness (11 km), requiring the presence of a mantle thermal anomaly

67 At least 60 km(3) +/- 12 km(3) or between 41 and 62% of the LIA total ice volume

68 cal energy and flash length of 16 fJ, and 12 km, respectively.

69 We performed high-resolution (12 km x 12 km) atmospheric chemical transport modeling (WRF

70 We performed high-resolution (12 km x 12 km) atmospheric chemical transport modeling (WRF-Chem) f

71 eptomyces biogeography in soils along a 1200 km latitudinal transect across New Zealand (NZ).

72 urchin barrens at nine islands spanning 1230 km of the Aleutian Archipelago where the loss of predato

73 astwards ('short-stopping') at a rate of ~13 km/year, thereby shortening individual migration distanc

74 closely located caves (ranging from 3 to 13 km apart) in the cave-rich southern Cumberland Plateau o

75 so reflect the presence of a buried ~17 x 13-km crater.

76 entified an entire trade chain, covering 137 km.

77 We sampled the fences along the 14 km of the two motorways included in the 17 1 x 1 km squa

78 m(2)), and Daxiangling, with few dogs (~0.14/km(2)).

79 rmined the NLCB of a lowland catchment (~140 km(2) ) in tropical Australia over 2 years by evaluating

80 mid- to lower-crustal portions (here, ~5-15 km and >15 km respectively) of these magmatic systems wh

81 ted regularly between 1904 and 2016 along 15 km of Belgian coastline, along with records of key envir

82 wer-crustal portions (here, ~5-15 km and >15 km respectively) of these magmatic systems where interme

83 ite forms a high velocity, high density, >15 km thick east-dipping body that during emplacement flexe

84 ducted sequentially at separate locations 15 km apart in the Florida Keys (USA).

85 de continental rift and highly extended (<15 km) continental margin.

86 rth from 2008 to 2016 while living within 15 km of LAX were included in this analysis (N = 174,186; i

87 al address, using weather stations within 15 km of the residence and 100 m in elevation.

88 nce and habitat was sampled across a 30 x 15 km area by remotely-operated vehicle, and included locat

89 India-Eurasia convergent zone to 1,350-2,150 km and limit the north-south extent of northwestern Grea

90 eedlots separated by distances exceeding 150 km, suggesting that European starlings could be involved

91 At depths shallower than 150 km, poloidal-mode flow is perpendicular to the trajector

92 o other major complexes of passage tombs 150 km to the west of Newgrange, as well as dietary differen

93 measured densities of 10(-2) cm(-3) at ~1500 km.

94 ch range from several hundred meters to 1540 km and their elevations vary from near sea level to near

95 rred in both Mongolia and North China (>1600 km apart), whereas in eastern Russia the switch occurred

96 arctic expeditions (IM: N = 6, 61 days, 1700 km; SP-17: N = 5, 67 days, 1750 km).

97 lew for >5 h without flapping, covering ~172 km.

98 1 days, 1700 km; SP-17: N = 5, 67 days, 1750 km).

99 t the convective anvil cloud, reaching 16-18 km above sea level, was ice-rich and ash-poor.

100 relation in the UFP concentrations up to 180 km and clear differences between the north and the more

101 jecta couplet within a distance of up to 180 km from the crater.

102 5-2050, and $0.27 to $0.31/mile ($0.17-$0.19/km) in 2050.

103 Specifically, velocities of 2.7 +/- 0.2 km/s correspond with growth of porosity from dissolution

104 0.9 km m(-2) y(-1) increased linearly by 1.2 km m(-2) y(-1) (130%) for every degree increase in soil

105 leiitic basalts of oceanic plateaus, the 1.2 km vertical submarine stratigraphic profile reveals two

106 faults penetrating to the depth of 13 +/- 2 km below the seafloor were identified based on the micro

107 e of particles is analyzed from a locality 2 km from the north-western perimeter of the site - north

108 ence for shallow waters (5-15 m) less than 2 km from the coast.

109 propagated at a relatively slow velocity (2 km/s) along a segment that was unloaded by the M(w) 6.5

110 ouldery sandstone and mudstone breccia 10-20 km from the center of the impact and fractured quartz gr

111 es forests for flood risk reduction every 20 km worldwide.

112 (130 fJ) and longer median flash lengths (20 km).

113 n additional 100 upwind UOGD wells within 20 km is associated with an increase of 0.024 mBq/m(3) (95%

114 Many (>45) 20-km coastal stretches particularly those near cities rece

115 rguments in favour of impact origin of a 200 km suspected impact crater Kotuykanskaya near Popigai, S

116 on the downstream side of dry patches >=200 km across.

117 ations but not the shorter-wavelength (<~200 km) rotations observed in the western USA.

118 urvey were located in a stretch along a 2000 km of the Amazon river in the northern region.

119 m) in 2020, $0.30 to $0.33/mile ($0.19-$0.21/km) in 2035-2050, and $0.27 to $0.31/mile ($0.17-$0.19/k

120 n-driven seagrass loss in Cockburn Sound (23 km(2) between 1960s and 1990s) and identifies the main d

121 subducted sulfur is released between 30-230 km depth, and the predominant sulfur loss takes place at

122 Sampling sites are 230 km apart from west to east, but are at varying elevation

123 ce of thick young oceanic lithosphere (20-25 km), and extremely heterogeneous upper mantle.

124 ess flammable than older forests, up to a 25-km radius around communities compared to that in the sur

125 The predicted shaking for a 25-km-long fault matches the intensity distribution, with a

126 breeding populations (in this case, 140-250 km apart) can identify dramatically different vulnerabil

127 ly suitable cultivation areas by 7%, the 250 km(2) (3%) expansion under low-emission scenarios will s

128 One sample site, 28 km north of the plant, had PFOA at 143 ng/L and HFPO-DA

129 ranged from $0.38 to $0.45/mile ($0.24-$0.28/km) in 2020, $0.30 to $0.33/mile ($0.19-$0.21/km) in 203

130 climate velocity increased on average by 0.3 km/year and cumulative climatic resistance increased for

131 rlier Hasanabad advances during 1892/93 (9.3 km) and 1903 (9.7 km).

132 two 4-minute treadmill exercises (at 2 and 3 km/h), and ADLs: ADL1 (getting dressed), ADL2 (folding 8

133 Shield: one near a highway and the other >3 km from roads where salt is applied in the winter.

134 m the largest individuals propagating over 3 km.

135 species living across the Messina strait (3 km wide) separating Sicily from the Italian Peninsula, w

136 The area of lakes is 1,095 x 10(3) km(2) and total CH(4) emission is 13.8-17.7 Tg CH(4) yea

137 dispersal (48.9%) was LDD (classified as >30 km), and the likelihood of LDD was positively associated

138 lled three UAS with operational ranges of 30 km, 65 km, and 100 km (UAS30, UAS65, and UAS100) and lif

139 the mean shell thickness is around 10 to 30 km.

140 This burial site was ~30 km from his reported jump location which gave no apparen

141 n sediment resuspension, primarily within 30 km of the southeastern shore.

142 8.1 +/- 5.6 degrees N, placing it 600-2,300 km south of the contemporaneous Eurasian margin.

143 Silica at depths greater than 300 km may be present in the form of the rutile-type, high p

144 l years of landscape use visible on a 35,300-km(2) mosaic of aerial photographs covering much of cont

145 ed from a re-sampling campaign along a ~3000 km transect and simulations obtained from a process-base

146 unctioning of the soil food web along a 3000-km north-south transect across European Russia, spanning

147 oss in dense seagrass extent globally (1,310 km(2) ) following an acute disturbance.

148 re kilometers (km(2)), compared with 308,311 km(2) that were deforested.

149 We refine the boundaries of an area of ~0.35 km(2) below the crest of the prehistoric landslide.

150 t the top of the profile implies that the 35 km-wide Hirondelle Basin opened after this time along no

151 nd expanding the highly suitable land by 352 km(2) in 2050, the overall cultivation potential for Per

152 dual migration distance on an average by 353 km.

153 In 2017, the 129,361 km(2) of secondary forest in the Brazilian Amazon stored

154 idence of recent deformation propagating >37 km south of the MFT.

155 We estimated that 27.4 km(2) of deforestation was averted in the national park

156 sity and community compositions across a 3.4 km elevational gradient (consists of five elevations) on

157 (>100 ng/L) found in surface water up to 6.4 km north of the plant.

158 ed managed areas (with a median width of 9.4 km) would need to be enforced as strict no-take MPAs and

159 accreted consistently at a rate of +2 to +4 km(2)/year.

160 The European XFEL (EuXFEL) is a 3.4-km long X-ray source, which produces femtosecond, ultrab

161 ofiles penetrating down to an altitude of 40 km.

162 brated using field measured traits, over 400 km(2) of northeastern Borneo, including a landscape-leve

163 remote sensing emission data with over 4000 km of 1 Hz real driving data.

164 associated with the phase transitions at 410 km and 660 km.

165 mangrove systems were deltaic, 27.5% (37,411 km(2)) were estuarine and 21.0% (28,493 km(2)) were open

166 s , a low-stability layer extends down to 42 km, which has been unreported in analyses of previous me

167 ed) for three land types ranged from 351-428 km (cultivated cropland), 80-492 km (perennial forage cr

168 ironments and coating survived even after 44 km of linear sliding.

169 populations: Liziping, with many dogs (~0.44/km(2)), and Daxiangling, with few dogs (~0.14/km(2)).

170 birth coordinates with a median error of 45 km.

171 ruption coignimbrite column that rose to ~45 km by modeling the deposit thickness using state-of-the-

172 From 300 to 450 km depth, return flows surround the edges of the Rivera

173 tress pattern related to bending down to 450 km, followed by unbending as the slab is laid flat upon

174 Kites migrated for 3300-4800 km along a narrow corridor, crossing the Himalayas at ex

175 rom 351-428 km (cultivated cropland), 80-492 km (perennial forage cropland), and 117-799 km (grazing

176 ,411 km(2)) were estuarine and 21.0% (28,493 km(2)) were open coast, with lagoonal mangroves the leas

177 enario, 374-1,144 grid cells of 1.5 km x 1.5 km each, comprising 0.5%-1.5% of Great Britain's land ar

178 of seropositive children in communities <1.5 km from the lake.

179 Two sandy tsunami deposits extend over 1.5 km inland of the coast.

180 on the scenario, 374-1,144 grid cells of 1.5 km x 1.5 km each, comprising 0.5%-1.5% of Great Britain'

181 sub-horizontal reflections at ~11 and ~14.5 km below the seafloor over the 0.51-2.67 Ma old Juan de

182 along an Amazon-Andes transect spanning 3.5 km in elevation and 16 degrees C in mean annual temperat

183 ently launched satellite sensor TROPOMI (3.5 km x 7 km at nadir), averaged to 0.01 degrees x 0.01 deg

184 rived tabular source, ~ 11 x 8 x 1 km; ~ 6.5 km depth; ~ 0.037 km(3)/year volume-change rate) and war

185 geographic information systems (GIS) on a 5 km pixel size for best-possible inference.

186 are typically most sensitive to shallow (<5 km) storage and/or have insufficient resolution at these

187 five adjacent modern reefs extending over 5 km.

188 rient inputs, with 60% of blooms less than 5 km from a penguin colony.

189 twice as many nightly flare events within 5 km as those with <20% Hispanics.

190 ourth quartile, >= 27) vs. no wells within 5 km had a higher odds of preterm birth [OR = 1.31 (95% CI

191 Nearly 400000 people live within 5 km of an unconventional oil or gas well in this largely

192 f flaring activity during pregnancy within 5 km of maternal residence.

193 ith the number of oil and gas wells within 5 km using data from DrillingInfo (now Enverus).

194 adjustment for the number of wells within 5 km.

195 and ArcTG boundaries are displaced about 50 km poleward in 1950-2015.

196 y stratified layers above 58 km and below 50 km, respectively.

197 Some dolphins can exceed speeds of 50 km/h, a feat accomplished by thrusting the flukes while

198 s anthropogenic imprint at distances over 50 km from the coastline and >500 m depth, beyond the conti

199 gion, including in Switzerland, less than 50 km from the Alpine ice sheet margin.

200 year survivors with pain who lived within 50 km from the study hospital.

201 category 2 hurricanes per century within 50 km of TPBH since 1850 CE.

202 s, and can migrate distances exceeding 1,500 km in North America.

203 northern Gulf of Mexico - located about 500 km from the Chicxulub crater - offer a unique opportunit

204 nami that poured over the coast flooding 500 km alongshore the Mexican Pacific coast and up to 6 km i

205 s (<5 mm) and far from coastal sources (>500 km).

206 ies (<10(2) cm(-3)) at high altitudes (~5300 km) by the MESSENGER spacecraft.

207 hrub warming response rate increased to 2.54 km m(-2) degrees C(-1) Soil moisture was negatively corr

208 used a 19 year moose location dataset, a 568 km transect of field shrub sampling, and forecasted warm

209 ted substantial illegal logging activity-579 km of logging canals were located beneath the canopy.

210 a low-stability layer at altitudes of 50-58 km and highly and moderately stratified layers above 58

211 ly and moderately stratified layers above 58 km and below 50 km, respectively.

212 jing reduces cumulative GW depletion by ~3.6 km(3), accounting for 40% of total GW storage recovery d

213 hese hydrothermal fluids could circulate ~ 6 km deeper than the Moho boundary and to much greater dep

214 gshore the Mexican Pacific coast and up to 6 km inland.

215 ina are projected to accelerate from ~2 to 6 km/yr by 2050.

216 e imagery over a region spanning 4.7 x 10(6) km(2) in Alaska and northwestern Canada to characterize

217 tern gorillas in Republic of Congo across 60 km(2).

218 At least 60 km(3) +/- 12 km(3) or between 41 and 62% of the LIA tota

219 The main body extends up to 60 km from the coast and a seawater depth of 110 m.

220 e velocities from 1992-2019 across a ~10,600 km(2) land-terminating area of southwest Greenland.

221 pletion of rocks around dikes covers 500-600 km(3), which, when scaled to the total CRB province cons

222 gence at both small (<10 km) and large (>600 km) spatial scales for four of the six Collembola specie

223 ous slab dipping at ~30 degrees down to ~600 km, and earthquake mechanisms point to down-dip compress

224 c to the Andaman Archipelago, located ~ 6000 km away from Madagascar where the genus Phelsuma likely

225 ng ratios, covering a distance of about 6400 km, and sampled emission plumes from sources such as clo

226 low suitability for Perigord truffles (6418 km(2)).

227 ree UAS with operational ranges of 30 km, 65 km, and 100 km (UAS30, UAS65, and UAS100) and lifespans

228 with the phase transitions at 410 km and 660 km.

229 ending as the slab is laid flat upon the 660 km boundary.

230 Further, the slab is lying at the 660-km discontinuity, and this zone is aseismic.

231 milar volumes to GW storage recovery of ~2.7 km(3) (30%) along with policies on reduced irrigation (~

232 vances during 1892/93 (9.3 km) and 1903 (9.7 km).

233 aunched satellite sensor TROPOMI (3.5 km x 7 km at nadir), averaged to 0.01 degrees x 0.01 degrees us

234 > graphene was estimated to be 2.71 x 10(-7) km(2)/W and 2.65 x 10(-7) km(2)/W, respectively, implyin

235 o be 2.71 x 10(-7) km(2)/W and 2.65 x 10(-7) km(2)/W, respectively, implying the absence of the therm

236 necessary GHG accounting parameters in the 7-km(2) Zostera marina (eelgrass) meadow in Virginia, U.S.

237 t] (95 per cent confidence; h(70) = H(0)/(70 km s(-1) Mpc(-1)) and H(0) is Hubble's constant).

238 erical impact simulations indicate that a 70 km-diameter crater into a continental glacier could rele

239 The ~70 km-diameter Yarrabubba impact structure in Western Austr

240 ervations span a distance of more than 1,700 km, suggesting that occasional tool use may be widesprea

241 Furthermore, at 700 km depth, the study region is dominated by the Farallon

242 o typical exospheric densities found at ~700 km altitudes.

243 e southeast coast of the United States (>700 km away) where the oceanographic environment is dominate

244 (2) of habitat at the local-scale and 45,703 km(2) at the state-scale.

245 und distance travelled was 2.03 km (+/- 0.71 km SD) with an over-ground average swim speed of 0.41 m/

246 nd cousins, close relatives buried around 75 km apart in Hispaniola and low genetic differentiation a

247 d most non-breeders made long-distance (5-77 km) movements during the breeding season while conspecif

248 <0.5 Ma, over a minimum slipped area of ~780 km(2) These observations demonstrate that Himalayan rupt

249 We identified 23,798 km(2) of habitat at the local-scale and 45,703 km(2) at

250 km (perennial forage cropland), and 117-799 km (grazing land).

251 Citizen responders located 1.8 km (1.1 miles) from the OHCA were dispatched to start CP

252 r reference sites that were located from 2-8 km from the outlet.

253 ng with policies on reduced irrigation (~2.8 km(3), 30%).

254 ing 1000 ng/L at 13 sample sites within an 8 km radius of the plant.

255 7-8% of the total pore fluid pressure at ~ 8 km depth.

256 he modern splay fault at shallow depths (~ 8 km) in the Nankai Trough.

257 ng to show that deep serpentinization (40-80 km) generates significant amounts of H(2) and abiotic CH

258 a, and rendered all areas within at least 80 km of the volcano uninhabitable for years to decades aft

259 aster in Iwanuma, a Japanese city located 80 km from the epicenter.

260 tope dataset from Schrader Pond, located ~80 km from the Arctic Ocean, which we interpret alongside s

261 between sites, from 0.58 for sites within 80 km of each other to 0.47 for sites farther away.

262 ntly, an estimated 17% (1,036,800 +/- 24,800 km(2) , 95% confidence interval) of the original forest

263 n to be extensive, with thickness of 300-800 km.

264 pango; and calculated that between 37 and 82 km(3) of magma was dispersed from an eruption coignimbri

265 gricultural land in the Czech Republic (8486 km(2)), whereas only ~ 8% of the warmest part of souther

266 n and fate of 216 P. unifilis nests along 88 km of rivers.

267 (+0 degrees C) shrub fine-root growth of 0.9 km m(-2) y(-1) increased linearly by 1.2 km m(-2) y(-1)

268 he foray distance of free-roaming dogs (10.9 km path-distance).

269 ving in a restricted geographical area (<900 km(2) ) that shows marked changes in diet through ontoge

270 extent of northwestern Greater India to <900 km.

271 es buried beneath lavas of a long-lived, 910-km(3) volcanic field in Southern Laos: 1) Tektite geoche

272 red to map forest biomass dynamics across 96 km(2) of PSF in Kalimantan, Indonesia.

273 t, based on their 2016 extent, 40.5% (54,972 km(2)) of mangrove systems were deltaic, 27.5% (37,411 k

274 mangroves the least abundant (11.0%, 14,993 km(2)).

275 Annually, fire emissions (-56 Mg C km(-2) year(-1) ) and SigmaF(aq) (-28 Mg C km(-2) year(-

276 C km(-2) year(-1) ) and SigmaF(aq) (-28 Mg C km(-2) year(-1) ) reduced NEP by 13% and 7%, respectivel

277 catchment was a large C sink (NLCB 334 Mg C km(-2) year(-1) ), and that savanna and wetland areas co

278 metre of walking range between 0.05 kgCO(2)e/km in the least economically developed countries to 0.26

279 mically developed countries to 0.26 kgCO(2)e/km in the most economically developed countries.

280 graded forest was 337,427 square kilometers (km(2)), compared with 308,311 km(2) that were deforested

281 aily PM(2.5) levels were estimated at 1-kmx1-km grid cells from a previously validated prediction mod

282 size over a land area that spans 1.3 million km(2) in the West African Sahara, Sahel and sub-humid zo

283 Globally, only 17.4 million km(2) of forest (40.5%) has high landscape-level integri

284 mate change has degraded 12.6% (5.43 million km(2)) of drylands, contributing to desertification and

285 lf, juvenile material forming some 5 million km(2) new continental crust.

286 Mining potentially influences 50 million km(2) of Earth's land surface, with 8% coinciding with P

287 st and wetland conservation and ~1.7 million km(2) for restoration or altered management opportunitie

288 We identified ~4.8 million km(2) for possible forest and wetland conservation and ~

289 with an average value of about $1.8 million/km(2) per year and a median value of $91,000/km(2) Wetla

290 two nest densities (moderate = 12.5-25 nests/km(2), high = 25-50 nests/km(2)) in south-central Texas,

291 te = 12.5-25 nests/km(2), high = 25-50 nests/km(2)) in south-central Texas, USA during March-June 201

292 d the number of HIV-infected individuals per km(2), and an impedance map.

293 , and 1-4 kg of DON to the coastal ocean per km of shoreline per day during late summer.

294 nal line-transect estimates (0.33 whales per km(2), CV = 0.09).

295 lity and weather conditions (0.13 whales per km(2), CV = 0.38), they fall within an order of magnitud

296 t mean monthly temperature for 465,775 river km in the western U.S., and then applied simple yet plau

297 rust while the eastern limit extends several km offshore, where it is defined seismically by a ~40-45

298 tating substrate binding at the active site (km) and the other, for example, E542K and E545K, reduces

299 ted the thermal suitability of 31,699 stream km which are currently blocked by dams to explore reintr

300 lar mass neutron star is [Formula: see text] km at 90% confidence and the Hubble constant is [Formula