ライフサイエンスコーパス: winter

1 period of lowest resource availability (i.e. winter).

2 he Central and Eastern Pacific during boreal winter.

3 summer, and 107 mug/m(3) and 24 h PM(2.5) in winter.

4 evels of EOPEs than samples collected in the winter.

5 ty allocation to storage in order to survive winter.

6 n summer and different forage composition in winter.

7 ation photosynthetic activity throughout the winter.

8 ine, proline and a variety of sugars rose in winter.

9 odel-observation bias (+19% to -53%) through winter.

10 m the F&M of other farms, both in summer and winter.

11 e cooling in autumn is stronger than that in winter.

12 e target rock also contributed to the impact winter.

13 he U.S, with most outbreaks occurring during winter.

14 ead enhancement across the IGP region during winter.

15 plants to enhance freezing tolerance (FT) in winter.

16 ned the planet-a scenario known as an impact winter.

17 ements in the PM(2.5) concentrations towards winter.

18 apacity lowers to 0-5 L/m(2)/day in fall and winter.

19 r sites and during colder periods throughout winter.

20 dant species, accompanied by benzanthrone in winter.

21 imited to the algal species available during winter.

22 ingly non-owners had higher survival in cold winters.

23 afted detritus contents indicate less severe winters.

24 ars of high predator abundance and in colder winters.

25 viability, offsetting the impacts of harsher winters.

26 during summer and high values during spring/winter (0 to - 3 per mille), while 70% of the annual rai

27 roduces ripe metallic blue fruits throughout winter [1].

28 TEP (summer 13-160 and winter 18-46, ng/L) and TCPP (summer 242-4282 and winter

29 mples (277) were collected during summer and winter (2012-2014).

30 rine impacts in the Northeast Pacific during winter 2013/2014.

31 nths with ARI from 50-60 US clinics during 5 winters (2013-2018) and tested for influenza with RT-PCR

32 Three consecutive dry winters (2015-2017) in southwestern South Africa (SSA) r

33 lity benefits of the coal-to-gas strategy in winter 2017 and reflects structural challenges and poten

34 rrounding areas (the "2+26" pilot cities) in winter 2017 compared to the same period of 2016, where t

35 gside medical staff and biobank samples from winter 2018/2019.

36 r 18-46, ng/L) and TCPP (summer 242-4282 and winter 215-854, ng/L) were the main OPEs.

37 AFM1 Levels were the highest in winter (48.70 ng/Kg).

38 Whereas, in contrast, towards winter, a large-scale decline in the air temperature, si

39 e two linked phenomena play crucial roles in winter acclimation and protection.

40 otherms have increased opportunities for mid-winter activity but need to move deep to digest captured

41 g spring, while patterns of selection during winter aligned best with ease-of-travel for the less-ind

42 Sigma(10)OPAHs were 10.0 +/- 9.2 ng/m(3) in winter and 3.5 +/- 1.6 ng/m(3) in summer.

43 ason" of elevated up-call detections in late winter and early spring corresponding to the season when

44 old (freezing) temperatures during long dark winter and fully recover during summer.

45 lfate aerosols and dust, initiated an impact winter and global darkening that curtailed photosynthesi

46 roughout the water system were higher in the winter and lower in the summer months.

47 ors to GPP beginning with air temperature in winter and proceeding to moisture and leaf area during t

48 erall, due to increased snow exposure in the winter and spring months.

49 Surveys in winter and spring produced the best datasets, and, as po

50 attack timing was negatively correlated with winter and spring temperatures and spring and summer pre

51 These trends were strongly attributable to winter and spring warming.

52 a primary influence on net CO(2) exchange in winter and spring, while soil moisture has a primary con

53 rban air in Brno in two campaigns during the winter and summer of 2018.

54 er locations, and GPP was responsive to both winter and summer precipitation such that two distinct G

55 95 +/- 0.77 and 1.15 +/- 0.36 ng/m(3) during winter and summer, respectively.

56 10 conventional) in the Netherlands, during winter and summer.

57 abolically-driven energy conservation during winter and sustaining foetal growth, which may also appl

58 n long-distance migrants that weather at the wintering and stopover grounds almost entirely (~80%) ex

59 ergo antigenic mutations in both summers and winters and thus monitoring the virus in both seasons ma

60 hat the UK will experience warmer and wetter winters and warmer and dryer summers.

61 Greenland (breeding), Ireland and Scotland (wintering) and Iceland (spring and autumn staging).

62 r both wind speed and solar radiation during winter, and lowest during summer.

63 ries for Brassica napus spring, winter, semi-winter, and Siberian kale crop types.

64 mediated floral bud break, early blooming in winter, and strong cold tolerance.

65 fe history-physiology axis from slow-growing winter annuals to fast-growing spring/summer annuals.

66 negative effects of albedo management during winter are mitigated by the seasonality of solar radiati

67 In this period the wintering area of the Bewick's swans shifted eastwards (

68 rlings defy long distances but may end up in winter areas with poor fitness prospects.

69 ve population of migratory Black-eared kites wintering around the megacity of Delhi-India, which host

70 the shift to a more anti-Bd microbiome over winter as a preparatory response for subsequent infectio

71 tes and seasons with the single exception of winter at the cool-temperate rainforest site where irrad

72 n, whereby plants remain dormant through the winter before flowering in spring.

73 temperature data showed that, throughout the winter, Bewick's swans frequent areas where air temperat

74 g BMAL2 and the EYA3/TSH pathway, triggering winter biology.

75 Populations of wintering birds were more dynamic, having higher rates o

76 of winter weather on population dynamics of wintering birds, and (b) what role species' physiology m

77 G, and HILPDA had increased expression among winter births (Bonferroni P < .05).

78 scripts, 583 displayed DE between summer and winter births (False Discovery Rate [FDR] q < .05); amon

79 seasonally variant genes between summer and winter births indicated overrepresentation of transcript

80 as recently replaced diatoms as the dominant winter, bloom forming organism.

81 d data range) was estimated to increase late winter body mass by 10%.

82 Because average late winter body mass explains 90% of the variation in popula

83 ales exhibited a temporary decrease in their winter body temperature.

84 Marmot survival declined during winter but generally increased during summer.

85 l samples with highest concentrations during winter, but also all organoarsenicals were detected thro

86 erritory owners had lower survival in colder winters, but surprisingly non-owners had higher survival

87 kely had hydrological controls influenced in winter by compromised subglacial flow and low meltwater

88 Winter CARVs were dominant during the early SARS-CoV-2 p

89 D) and a fungicide (tebuconazole) applied to winter cereal crops during the breeding season of most f

90 ezing treatment (DF) that emulates summer-to-winter change.

91 P. deltoides seed release, because decreased winter chilling combined with increased spring forcing l

92 sized relationships with autumn temperature, winter chilling, and the timing of spring onset, we accu

93 ing success were also strongly influenced by winter chlorophyll-a concentrations and sea-surface heig

94 ow that decadal variations in North Atlantic winter climate are highly predictable, despite a lack of

95 Winter climate change is expected to lead to the tropica

96 oach greatly improves decadal predictions of winter climate for Europe and eastern North America.

97 ith harsh environmental conditions such as a winter climate or food scarcity, leading to highly varia

98 Winter climate warming is rapidly leading to changes in

99 zation accelerates flowering after prolonged winter cold.

100 understanding relationships among antecedent winter conditions and carbon exchange across land-cover

101 quired was still remarkably low, and even in winter conditions with weak thermals, condors are only p

102 To survive harsh winter conditions, conifers have evolved a unique but po

103 idence of reproductive dormancy in simulated winter conditions, while flies overexpressing tim show a

104 that are exposed to limited food and adverse winter conditions.

105 TIM isoforms facilitate EYA accumulation in winter conditions.

106 fs between forage, predation risk and severe winter conditions.

107 These findings suggest that, as winters continue to warm, increases in ecosystem respira

108 ty could be observed concomitant with a weak winter convection.

109 licated four times, consisting of six single winter cover crop species, a three-species mixture, a si

110 Therefore, the use of winter cover crops and chicken grazing in a winter fallo

111 rotation of corn-soybean-wheat planted with winter cover crops.

112 oric agriculture previously based mainly on (winter) cropping of wheat and barley.

113 forests with freezing temperatures on bright winter days puts the photosynthetic machinery in great r

114 ble, by producing positive covariation among winter demographic rates, depicts a measure of environme

115 ties remain active during much of the Arctic winter, despite deeply frozen soils.

116 sanderling Calidris alba using six and eight winter destinations between 55 degrees N and 25 degrees

117 Cascades mountain ranges migrated to farther wintering destinations, with birds from the Lassen regio

118 al combustion and vehicle exhaust under poor winter dispersion conditions.

119 were correlated with the range shift of the wintering distribution.

120 Conversely, winter dormancy was transient at warmer locations, and G

121 We demonstrate that at winter-dormant sites, seasonal changes in canopy color c

122 lated sunlight levels representative of late winter/early fall and summer were 0.121 +/- 0.017 min-1

123 might contribute to 'sustained quenching' of winter/early spring pine needles, time-resolved fluoresc

124 m became a sustained carbon sink well before winter ended, taking up roughly 90 g/m(2) more carbon du

125 Chilling requirements for overcoming winter endodormancy were strongest in Salix exigua, mode

126 icit effects of future climate change on the wintering energetics of a freeze-tolerant amphibian, the

127 nter survival and spring breeding, increased winter energy requirements have the potential to impact

128 er length have opposing effects on Wood Frog winter energy requirements, leading to geographically he

129 Scaling up the winter estimate to annual indicated an anthropogenic emi

130 Work by de Winter et al. in this issue of the JCI provides evidence

131 Winter Eurasian cooling after the mid-1990s has been ver

132 is the major atmospheric mode that controls winter European climate variability because its strength

133 Willets from Nova Scotia to Georgia winter exclusively on the Atlantic coast of northern Sou

134 winter cover crops and chicken grazing in a winter fallow field was effective at reducing CH(4) emis

135 [cover crops and chicken grazing (+ C)] in a winter fallow field, we found that the soil organic matt

136 is underlying floral scent biosynthesis; and winter flowering, and highlight the utility of multi-omi

137 plant, has evolved unique fragrant aroma and winter-flowering properties, which are critical for its

138 ld disturb CA and increase the potential for winter freeze-injury.

139 es, responded to a period of highly variable winters from 2014 through 2017 that included the warmest

140 ver, also depends on whether the last day of winter frost is advancing more rapidly, or less rapidly,

141 g site in Iceland 5-15 days later than birds wintering further north or south.

142 ld experiment with 65 spring genotypes and 9 winter genotypes of camelina was conducted in Poland fro

143 By attaching radio tags on the wintering grounds and relocating the same individuals on

144 Concurrently, the time spent at the wintering grounds has reduced ('short-staying') by ~38 d

145 seasonal migrations between the breeding and wintering grounds have been observed across biological t

146 onsider the role of rainfall on the species' wintering grounds in North Africa.

147 metry arrays to track individuals from their wintering grounds in the Andes of South America along th

148 een upper and lower latitudinal breeding and wintering grounds rely on a limited network of endorheic

149 n the distribution of the species within its wintering grounds towards the east and north.

150 n when making the first return trip from the wintering grounds.

151 ng southbound migration, peaking on southern wintering grounds.

152 btypes, as waterfowl migrate toward southern wintering grounds.

153 tions allowing birds to delay departure from wintering grounds.

154 ever, how migratory strategies are shaped by winter habitat choice is largely unknown due to the gene

155 s that birds made facultative adjustments to winter habitat quality and environmental conditions.

156 spatial predictions of migrant and resident winter habitat.

157 importance of the Azores as a migratory and wintering habitat for three species of baleen whales and

158 haracteristics of wild migratory waterfowl's wintering habitat in the Republic of Korea (ROK) and to

159 neral inability to track birds from specific wintering habitats to stopovers or breeding destinations

160 Isolates recovered during winter had the highest proportion of mixed and rare HA/N

161 lerance to freezing and the development of a winter-hardy plant structure.

162 In recent decades, the final frost dates of winter have advanced throughout North America, and many

163 Fog and cloud readily form under winter haze conditions, leading to high liquid water con

164 explanation for sulfate formation under some winter haze conditions.

165 ertime particulate air pollution in Beijing (winter haze) are associated with high relative humidity

166 We quantified spatial overlap between the winter home ranges of GPS-collared elk and three measure

167 vention trial conducted during late fall and winter in 2 areas of Sweden (latitude 63 degrees N and 5

168 to low pH and algal resource identity during winter in a subpolar, marine ecosystem.

169 ith peaks in late spring and late fall/early winter in California.

170 of predation by wolves (Canis lupus) during winter in northern Yellowstone, USA.

171 140 m of each other for 2 h in total during winter in Seattle, Washington.

172 s in natural variants and mutants throughout winter in three field sites, we find that autumnal FLC e

173 tory strategies between habitats, with birds wintering in native forest departing later than birds in

174 vival was considerably lower for adult birds wintering in tropical West Africa (Mauritania: 0.74 and

175 ransmission, is typically characterized by a winter incidence peak in most countries.

176 are consistent in their migratory timing in winter, indicating that the frequency of individuals wit

177 Crucial in temperate climates, adaptation to winter is characterized by cold acclimation and vernaliz

178 es have been conducted in regions with harsh winters; it remains unclear whether snowfall is associat

179 spring release of CH(4) stored in bubbles in winter lake ice.

180 hat warming soil temperatures and decreasing winter length have opposing effects on Wood Frog winter

181 ised under control Equinox (LD 12:12), Short winter-like (LD 8:16), or Long summer-like (LD 16:8) pho

182 The slow, winter-long upregulation of VERNALIZATION INSENSITIVE 3

183 In late winter, low SWE and a relatively large elk population in

184 Wolves may follow the winter migration of their staple prey, moose (Alces alce

185 seasonal upwelling in the tropical ocean and winter mixing in the Southern Ocean.

186 iratory viruses within households during the winter months during the emergence of the SARS-CoV-2 pan

187 sCoVs were prevalent in winter months in most temperate sites except for China,

188 With the gradual cooling occurrence in winter, more accumulation of anthocyanin, chlorophyll de

189 generated from glaciogenic cloud seeding of winter mountain cloud systems and its spatial and tempor

190 Microwave thermal emission from the winter night side is consistent with a mean brightness t

191 Annual trends in wintering numbers differed throughout the range.

192 assland, record-breaking temperatures in the winter of 2015/2016 led to a February onset of plant gro

193 ent adaptation to humans sometime during the winter of 2019 in Wuhan Province, China.

194 with peak outbreaks likely occurring in the winter of 2021-2022.

195 female AUFS (970 foraging trips) during the winters of 1998-2019.

196 2014 through 2017 that included the warmest winter on record to date.

197 in population growth rates, such a delay in winter-onset would enable a population growth of r = 0.2

198 ycle indices of spring ENSO, summer NAO, and winter or spring PDO accounted for 40-54% of the variati

199 minantly driven by wind conditions at likely wintering or spring stopover areas during the migration

200 atory syncytial virus (RSV) typically causes winter outbreaks in temperate climates.

201 ey feature of the Arctic ice pack during the winter owing to their substantial contribution to the su

202 Wolves selected for lower altitudes in winter, particularly in the area where bears and wolves

203 RFRP-3 in the camel's brain with, during the winter period lower RFRP-3 expression and higher Kp expr

204 roductivity, snow water equivalent (SWE) and winter period.

205 We find that exposure to projected future winter pH conditions decreases metabolism and growth, an

206 In early winter, poor plant growth in either year t or t - 1, or

207 Due to counteracting winter (positive) and summer (negative) GPP responses to

208 rovirus were detected year-round with a fall/winter predominance.

209 tal population in the San Francisco Bay area wintered predominantly in western Mexico (n = 18), where

210 alization, is central to plants interpreting winter progression(5,6,8-11).

211 rd allowed the exploration of their spatial (wintering quarters/breeding grounds) and seasonal (nonbr

212 oduction chemistry and titration of ozone in winter, reduced nitrogen oxides resulted in ozone enhanc

213 forest loss was greater in the breeding and wintering regions of the two Cascade-Sierra populations

214 ak pollutant formation periods in summer and winter, respectively.

215 ration during the preceding anomalously warm winter, resulting in nearly neutral effects on the annua

216 Winter sampling revealed the highest proportion of mixed

217 During northward migration, tropical-wintering sanderlings occurred at their final staging si

218 hward but not southward migration by Namibia-wintering sanderlings, all suggest they face issues duri

219 eland during northward migration of tropical-wintering sanderlings, in addition to the skipping of th

220 The increasing concentration of wintering Scaup in coastal Poland and Germany (where lac

221 as fitted to the data, which showed that the winter season has the greatest influence on decreases in

222 t the human population like clockwork in the winter season in temperate regions.

223 bserved increased cases during the following winter season, when the new lineage was the predominant

224 ptome time series for Brassica napus spring, winter, semi-winter, and Siberian kale crop types.

225 The timing of wintering site departure, breeding site arrival, nesting

226 ive to the direct route between breeding and wintering sites, respectively, and contrasted it to the

227 that soil moisture increased under deepened winter snow in early growing season, particularly in dee

228 rns, and there is a trend towards increasing winter snow in semi-arid regions in China.

229 Here, we conducted a 5-year winter snow manipulation experiment in a temperate grass

230 Winter snowfall is an important source of water during e

231 Hence, our study demonstrates that increased winter snowfall may stabilize arid grassland systems by

232 Global warming has greatly altered winter snowfall patterns, and there is a trend towards i

233 However, we know little about how changes in winter snowfall will affect ecosystem productivity and p

234 Warmer winter soils are thought to yield greater microbial resp

235 ments, we demonstrate that persistently warm winter soils can lead to labile C starvation and reduced

236 If winter soils continue to warm, microbial C limitation wi

237 summer temperatures, coupled with cold early winter soils, are related to high herbivory by lepidopte

238 ges in snowpack are leading to warmer Arctic winter soils.

239 depths, rising air temperatures, shortening winters), spatially explicit assessments of species ener

240 , the latitudinal distributions of temperate-wintering species have increased while the latitudinal d

241 llected in four periods of the year (autumn, winter, spring and summer).

242 and to protect overwintering tissues against winter stresses.

243 ecies occurred throughout all regions in the winter, suggesting that baleen whales are widely distrib

244 tus- (resident/migrant) and season-specific (winter/summer) differences in resource selection by eigh

245 mperature, the major seasonal cues heralding winter, suppress branching by simultaneous activation of

246 viours appear to be specializations for cold winter survival and may have evolved in response to late

247 Simultaneously, negative responses of winter survival and reproductive-status change to declin

248 rely on body stores acquired in fall to fuel winter survival and spring breeding, increased winter en

249 gression, higher group cohesion and improved winter survival in both tit species.

250 However, winter survival of birds in egalitarian groups was impai

251 ming of territory acquisition influenced the winter survival of juvenile North American red squirrels

252 Winter survival was largely driven by conditions during

253 Evergreen conifers are champions of winter survival, based on their remarkable ability to ac

254 a decrease in the intensity and duration of winter temperature extremes (i.e., freeze events).

255 Warming winter temperatures are a main driver of expansion of th

256 systems with a perennial leaf habit, warming winter temperatures are more likely to increase ecosyste

257 Cold winter temperatures can influence insects' survival in t

258 e change and uncover a key mechanism, warmer winter temperatures delaying insect phenology, by which

259 alyses indicate that, in response to warming winter temperatures, Brazilian pepper is expected to exp

260 where they are seasonally absent due to low winter temperatures.

261 when particles were most acidic, whereas in winter the relative importance of WS-Fe from combustion

262 rns (maximum, average and minimum) from late winter to early spring affected the timing of cambial re

263 ern of accumulation of temperature from late winter to early spring is a critical factor in determini

264 atures started to increase earlier from late winter to early spring, cambial reactivation occurred ea

265 thwestern Canada during the anomalously warm winter to spring conditions of 2015 and 2016 (relative t

266 up roughly 90 g/m(2) more carbon during the winter to spring transition than in other recorded years

267 o tens of thousands of kilometers from their wintering to their breeding grounds.

268 e controlling processes from post-monsoon to winter transition profoundly affect the composition of t

269 modeling (WRF-Chem) for the post-monsoon to winter transition to unravel the underlying dynamics and

270 ms are experiencing warmer and more variable winters, trends that are expected to continue into the f

271 in in the absence of intense deep convective winters until 2018.

272 he warming trend of the Florida peninsula in winter was closely related to enhancement of the North A

273 on its body reserves to overcome the arctic winter, we investigated the direct and indirect impacts

274 Nino events may be responsible for the late winter weakening of the Aleutian Low Circulation in rece

275 stratospheric warmings can influence surface winter weather conditions, but their timing is difficult

276 t extent land cover moderates the impacts of winter weather on population dynamics of wintering birds

277 eased local colonization during the harshest winter weather.

278 ed landscapes are most vulnerable to extreme winter weather.

279 show that biomass starts increasing in early winter, well before sea ice begins to retreat.

280 The snow accumulation decreased and dry winters were reestablished in Dasuopu after 1880 AD when

281 linked to the meridional displacement of the winter westerlies from 1810 until 1880 AD.

282 Winter wheat (Triticum aestivum L.) is essential to main

283 Winter wheat (Triticum aestivum L.), a dual-purpose crop

284 3) epitopes, in a set of 60 German hexaploid winter wheat cultivars from 1891 to 2010 and grown in th

285 Slugs were collected in a commercial winter wheat field in which a 5x6 trapping grid had been

286 Here we analyze US winter wheat production from 1970 to 2017 and find that

287 wing for simultaneous phenotyping of popular winter wheat varieties from US Midwest and advanced bree

288 that can significantly reduce grain yield in winter wheat worldwide.

289 methods and fertilizer rate under a dryland winter wheat-fallow rotation.

290 ties of four different varieties of hard red winter wheat.

291 imitation of these two critical nutrients in winter wheat.

292 itrogen (N) and phosphorus (P) metabolism in winter wheat.

293 ough this may be common for consumers during winter when primary producers are limited by light.

294 e the onset of future waves, or the start of winter when risks of infection are higher.

295 d no differences between the groups after co-wintering when graded for commercial almond pollination.

296 dendron 'Elsie Lee', ABA and JA decreased in winter, which may be due to the strong requirement of ze

297 the prolonged intervals of immobility during winter, which suggests that they have adaptive mechanism

298 s maintained stable body temperatures during winter, while non-pregnant females exhibited a temporary

299 abalone caused by ocean acidification during winter will be exacerbated by seasonal shifts in their r

300 The cause was unusual winter wind patterns driving major changes in ocean circ