ライフサイエンスコーパス: hydrology

1 ith significant consequences for terrestrial hydrology.

2 at is relevant for climate change impacts on hydrology.

3 rief in these systems, and largely driven by hydrology.

4 iability associated with climatic effects on hydrology.

5 overturning circulation and tropical Pacific hydrology.

6 portant effects on the biosphere and surface hydrology.

7 applications in the medical sciences and in hydrology.

8 rests are structured and maintained by their hydrology.

9 ed case of the effects of rainfed farming on hydrology.

10 al transitions in vegetation composition and hydrology.

11 altering the ice sheet's present and future hydrology.

12 owpack and climatic shifts in altering basin hydrology.

13 ough atmospheric circulation and continental hydrology.

14 re, has positive impacts on microclimate and hydrology.

15 erm aridity and short-term changes in stream hydrology.

16 stem properties including carbon balance and hydrology.

17 ical processes such as seasonality and tidal hydrology.

18 PSFs which are dependent on their unimpacted hydrology.

19 ld by a factor of 3.7 relative to historical hydrology.

20 respond to changes in stream temperature and hydrology.

21 that link peat accumulation and groundwater hydrology.

22 volutionary time scales of geomorphology and hydrology.

23 s to capture the topography critical to soil hydrology.

24 obial community occurs at sites with varying hydrology.

25 cluded in the conceptual model of subglacial hydrology.

26 ctors, including temperature, irradiance and hydrology.

27 ntext of landscape evolution, weathering and hydrology.

28 nteractions between subsurface chemistry and hydrology.

29 such as soil texture, pedogenesis, and soil hydrology.

30 ets are shrinking rapidly, altering regional hydrology(1), raising global sea level(2) and elevating

31 important to ecosystem carbon storage(7) and hydrology(8), exhibit greater sensitivity to drought tha

32 al grid to characterize forest phenology and hydrology across a forested catchment in central Pennsyl

33 versity on coupled dynamics of phenology and hydrology across a landscape is largely untested.

34 fluences interannual variability in regional hydrology across the world through long-range dependence

35 engineered landscapes and subsequent altered hydrology affect the fate and transport of reactive nitr

36 Local hydrology, agriculture, and socio-economic data are used

37 s in packed-bed columns results in effective hydrology alteration and homogenization of heterogeneous

38 d regionally by snowmelt- and monsoon-driven hydrologies and combined with climate and human water-us

39 ch has fundamental implications for tropical hydrology and atmospheric circulation.

40 ncludes key variables and processes of basin hydrology and atmospheric forcing in a data-driven model

41 ed to uniformly applied models of subglacial hydrology and basal sliding, and a new subglacial topogr

42 er time, correlating with seasonal shifts in hydrology and biogeochemistry and clustering into three

43 avers and magnify their impacts on watershed hydrology and biogeochemistry, illustrating that ecosyst

44 m fish assemblages and relationships between hydrology and biology are likely to be influenced by flo

45 s and were used to infer changes in peatland hydrology and carbon dynamics.

46 quantitative inference about the morphology, hydrology and carbon storage of bogs through Earth's his

47 alysis to account for changes in climate and hydrology and changes in water demand.

48 The prevailing concepts of Yellowstone hydrology and chemistry are that fluids reside in reserv

49 soil environment, considering soil physics, hydrology and chemistry.

50 rthwestern BS shelf and deeply affecting the hydrology and circulation of the BS and, probably, of th

51 Forests impact regional hydrology and climate directly by regulating water and h

52 l role of elevated [CO2 ] in altering future hydrology and climate of the region that is extensively

53 pact that city design has on the local-scale hydrology and climate.

54 The complex hydrology and competing demands necessitate improved for

55 frost may thaw, altering soil topography and hydrology and creating a mosaic of wet and dry soil surf

56 We conclude that a framework combining hydrology and crop models to assess climate change impac

57 Better information about changing hydrology and disturbance regimes is needed to complemen

58 ion patterns produced an abrupt shift in the hydrology and dust deposition in the Everglades over the

59 skills of models in many geosciences (e.g., hydrology and ecosystem sciences) strongly depend on spa

60 We coupled a detailed mechanistic hydrology and entomology model with climate projections

61 a revealed abrupt and synchronous changes in hydrology and fish assemblage structure of a floodplain

62 Fractures are integral to the hydrology and geochemistry of watersheds, but our unders

63 five fourth-order stream reaches with varied hydrology and geomorphology.

64 ary flows as well as changes to pH and river hydrology and hydrogeomorphology.

65 variation, such as differences in sewershed hydrology and laboratory protocols, have a substantial i

66 use river flow simulations from nine global hydrology and land surface models to explore uncertainti

67 through effects on environmental stability, hydrology and life-history filtering.

68 xamine the roles of storm-related changes in hydrology and long-term precipitation regime on the resp

69 Our findings show that hydrology and long-term precipitation regime predictably

70 mate impacts of mineral dust aerosols to the hydrology and mechanics of unsaturated soils and sedimen

71 Our findings suggest that hydrology and metacommunity dynamics, both changing pred

72 Changes in river hydrology and morphology caused by climate-induced glaci

73 , using high-resolution measurements of pond hydrology and numerical modelling, that episodic inundat

74 of extreme hydrological events on catchment hydrology and nutrient losses.

75 modifications to the underlying vegetation, hydrology and overall ecosystem.

76 By integrating insights from geology, hydrology and remote sensing technologies, the study nav

77 tivity to ecosystem properties such as local hydrology and residence time.

78 redox conditions that arise due to changing hydrology and resulting biogeochemistry.

79 ctively, are consistent with modern isotopic hydrology and reveal that dramatic fluctuations in water

80 fluorescence spectroscopy, here we show that hydrology and river geomorphology interactively shape mo

81 Since soil hydrology and soil pores are likely to be affected by fu

82 range of soil physical processes, including hydrology and soil strength regimes.

83 nt of possible climate change impacts on the hydrology and temperature of Arctic rivers at the region

84 d are thought to be controlled by subglacial hydrology and till deformation.

85 ure scenario for each district with restored hydrology and tree cover at 30%.

86 ed spatio-temporal dynamics of phenology and hydrology and understanding underlying processes is a fu

87 complex feedbacks between peat accumulation, hydrology and vegetation.

88 n long-term (21 years) field measurements of hydrology and water quality, we investigated the tempora

89 redicting how climate variability influences hydrology and water resources in water-limited landscape

90 ate techniques to delineate rainfall, stream hydrology, and antecedent moisture controls on sediment

91 ich capture the coupling between permafrost, hydrology, and atmosphere, we find that projected rapid

92 and function such as altered fire behavior, hydrology, and carbon storage.

93 e, mobilization of previously frozen carbon, hydrology, and changes in organic matter chemistry assoc

94 al pattern explained by geology, topography, hydrology, and climate.

95 he urban-water cycle modifies natural stream hydrology, and domestic and commercial activities increa

96 in order to simulate future global climate, hydrology, and ecosystem dynamics.

97 res on factors such as vegetation structure, hydrology, and fire regimes, it follows that the vast ma

98 Here, we linked climate, hydrology, and habitat models within a coho salmon (Onco

99 nergy fluxes that drive regional climate and hydrology, and have a negative impact on productivity an

100 for many applications, such as agriculture, hydrology, and natural hazard risk assessment.

101 he interactive effects of water temperature, hydrology, and other anthropogenic changes.

102 We combined field observations with climate, hydrology, and phenology models to simulate future chang

103 tanding of the hydrological cycle, catchment hydrology, and polar climate.

104 eates microhabitats, turns over soil, alters hydrology, and removes carbon from the above-ground carb

105 ies of linked models of climate, land cover, hydrology, and salmon population dynamics, we investigat

106 trongly influenced by urban runoff and tidal hydrology, and sediments therein exhibited SigmaPBDE con

107 ation bridges the gap between seismology and hydrology, and shows the promise of leveraging seismomet

108 ultimately driving changes in plant growth, hydrology, and the global carbon balance.

109 olled, at one level, by watershed landscape, hydrology, and their connections.

110 tify predictors describing proximity to UOG, hydrology, and topography that are important for metamod

111 es, including daily measurements of weather, hydrology, and water quality parameters, to generate a n

112 f the Ca amendment was a change in watershed hydrology; annual evapotranspiration increased by 25%, 1

113 d model for many applications in groundwater hydrology, applied geophysics, CO(2) subsurface storage,

114 Regional effects of farming on hydrology are associated mostly with irrigation.

115 racteristics including plant communities and hydrology are key for understanding Cl cycling in the en

116 geodesy, with applications in geophysics and hydrology as well as in space-based tests of fundamental

117 low soils is expected to decouple from plant hydrology, as soils dry out as a result of rapid evapora

118 results indicate that changes in short-term hydrology associated with precipitation can impact hot s

119 ses, suggesting significant changes in basal hydrology beneath the lakes driven by seasonal meltwater

120 eneath the East Antarctic ice sheet, but the hydrology beneath this ice mass is poorly understood.

121 l mechanism that maintains a tightly coupled hydrology between shallow rocky soils and trees, as well

122 ut also vital environmental services such as hydrology, biodiversity, and carbon cycles; livestock co

123 s are common boreal ecosystems with distinct hydrology, biogeochemistry and ecology that influence th

124 ineering, social science, soil science, law, hydrology, botany, geology, pollination biology, financi

125 on the magnitude of temperature increase and hydrology but also organic matter quality, permafrost hi

126 ns indicate a dramatic shift in the region's hydrology but the timing and triggers of this shift rema

127 nt regime shift with major ramifications for hydrology, carbon and nutrient cycling, water and habita

128 The post-fire ecosystem and hydrology changes also had strong ecological effects, wi

129 mussels preserve valuable information about hydrology, climate, and population dynamics, but develop

130 Leveraging global information on the hydrology, climate, geology and surrounding land cover o

131 Integrating knowledge across hydrology, climatology, agriculture, political science,

132 at this region experienced abrupt changes in hydrology coeval with orbital and millennial-scale event

133 imental permafrost warming introduced a soil hydrology component that interacted with temperature to

134 In hydrology, conceptual models are preferred for their sim

135 helf melt, our results imply that subglacial hydrology could trigger higher rates of mass loss than p

136 d due to a lack of in situ water quality and hydrology data and the irregular monitoring of these wat

137 urrent conceptual models for Greenland basal hydrology, derived primarily from the study of mountain

138 Hydrology drives the carbon balance of wetlands by contr

139 The latter is a measure of changes in local hydrology (e.g., precipitation/evaporation, freshwater i

140 will damage infrastructure, but also impact hydrology, ecology and biogeochemistry.

141 l theories (such as CBFT) can be melded with hydrology, engineering design, and ecology to improve th

142 ity models, describing the interplay between hydrology, epidemiology, and social behavior sustaining

143 an provide valuable information on catchment hydrology, flow paths, and subsurface storage.

144 fluences of copper ore composition and local hydrology for dynamically estimating leached metals of t

145 A precise streamflow forecast is crucial in hydrology for flood alerts, water quantity and quality m

146 Nevertheless, climate change and changes in hydrology, for example, due to construction of dams, can

147 ual contributions (ice sheets, glaciers, and hydrology) found in literature.

148 tem processes such as surface and subsurface hydrology from a single compact instrument, where co-loc

149 s used to better understand the interplay of hydrology, geochemistry, and biology controlling the cyc

150 tors including anthropogenic nutrient loads, hydrology, geology, elevation, climate, and lake and cat

151 on peatlands is affecting their morphology, hydrology, ground-level climate conditions, carbon funct

152 found that spatial and temporal variation in hydrology had a strong influence on fish assemblage dyna

153 While seasonal and interannual variations in hydrology have a direct impact on the amounts of C trans

154 Restoration has had a dramatic effect on hydrology, however, consequent changes in other ecosyste

155 analysis alone is inconclusive if an unknown hydrology impedes a distinction between degradation and

156 arvested than infiltrated to maintain stream hydrology in a preurban state.

157 eet inception and will have influenced basal hydrology in Greenland over past glacial cycles.

158 However, although ENSO is known to influence hydrology in many regions of the world, little is known

159 Our results highlight the importance of land hydrology in understanding/predicting forest-savanna tra

160 tic-derived n-alkanes that record changes in hydrology, including surface water salinity and precipit

161 18)O of sea water-a sea surface salinity and hydrology indicator-indicates a tight coupling with the

162 nderlying orbital-scale variability and drip hydrology influence the delta(18)O response.

163 We used a model for permafrost hydrology informed by detailed measurements of soil ice

164 We show that subglacial hydrology is crucial for controlling methane fluxes from

165 Our results demonstrate that sub-tropical hydrology is forced by both orbital cyclicity and North

166 ance, a global synthesis of their effects on hydrology is lacking.

167 ecipitation (PCP), a process driven by local hydrology, is a widely ignored control of speleothem del

168 en assessing the impact of climate change on hydrology, it is therefore critical to consider a divers

169 We highlight the importance of a muted hydrology mechanism that acts to weaken the PWC.

170 nopterus albus/javanensis) has disrupted the hydrology-mediated production of crayfish and some small

171 limatic gradient, indicating that subsurface hydrology mediates species' experience of drought, and t

172 -peatland areas by using a process-based eco-hydrology model (ecosys) and publicly available data for

173 al downscaling via WRF and the WEHY-HCM snow-hydrology model with a lead-time-dependent exponential-s

174 ios and projections from a three-dimensional hydrology model, we simulated coho smolt production over

175 plicit, mechanistic, coupled biogeochemistry-hydrology model.

176 roundwater at 30" global grids with a global hydrology model.

177 We utilize a coupled economy-agroecology-hydrology modeling framework to capture the cascading im

178 of scalable hydrologic datasets or scalable hydrology models that can inform the fire forecasting mo

179 d alter basic ecosystem properties, changing hydrology, nutrient cycles, soil chemistry, fire suscept

180 ipitation, elevation, vegetation cover, soil hydrology, oceanographic productivity, and wave energy.

181 ig data applications in three subdisciplines-hydrology, oceanography, and atmospheric science.

182 ve analysis of climate change impacts on the hydrology of 19 river basins from different geographical

183 e complex fracture networks proposed and the hydrology of both the subducting topography and the asso

184 which floods modify planetary surfaces, the hydrology of early Mars and abrupt changes in climate.

185 these deposits, in the context of the global hydrology of early Mars, using numerical simulations, an

186 es a robust framework for characterizing the hydrology of freshwater ecosystems and improving water m

187 Here, we investigate the paleo-hydrology of Lake Zonar (southern Iberia) by using the s

188 sidence does have significant effects on the hydrology of polygonal tundra.

189 ical characteristics of peat, as well as the hydrology of PSFs are affected after a fire, during whic

190 Thus, hydrology of shallow soils did not decouple from hydrolo

191 Under semiarid conditions, hydrology of shallow soils is expected to decouple from

192 be sensitive to human-caused changes in the hydrology of the lake, with human impacts such as dredgi

193 As the hydrology of the northern high-latitudes continues to ch

194 addition, irrigation plays a key role in the hydrology of the Yakima sub-basin - with flow reductions

195 ke the floodplain forests found upriver, the hydrology of these ecosystems is driven largely by large

196 ology of shallow soils did not decouple from hydrology of trees even in the driest period.

197 an monsoon system and remote control of IPWP hydrology on centennial-millennial timescales, rather th

198 s of CH4 , and investigating effects of soil hydrology on CH4 fluxes is of great importance for predi

199 d climate conditions, tropical cyclones, and hydrology on the seasonal variability in soil and river

200 lative impact of a deep-seated, global-scale hydrology on the surface evolution.

201 opogenic sources, modifications to catchment hydrology or habitats, and internal biogeochemical proce

202 ttle understanding of Antarctic-wide surface hydrology or how it will evolve.

203 As a general feature of western IPWP hydrology, our data suggest similar rainfall amounts dur

204 the associated impacts on the ecosystem and hydrology over the largest contiguous wetlands in the wo

205 ailed reconstruction of West African monsoon hydrology over the past 155,000 years suggests a close l

206 at reflect changes in west Pacific warm pool hydrology over the past 27,000 years.

207 stic emissions to sites estimated from local hydrology, population density, and waste production.

208 scale droughts is one of the unsolved global hydrology problems, which is important for understanding

209 Our detailed characterization of inundation hydrology provides a unique perspective that the regulat

210 Hydrology refers to the whole panoply of effects the wat

211 s of Sphagnum drought responses for peatland hydrology, restoration and wildfires are also outlined.

212 econnection driven by surface and subsurface hydrology, resulting in both adaptive and nonadaptive po

213 illslopes (for example, revegetation) and in hydrology, sediment characteristics and transport proces

214 both seasons, suggesting that variations in hydrology, sediment composition, and vegetation influenc

215 Given the direct effects of their dams on hydrology, sediment storage, and vegetation, beaver are

216 iable Infiltration Capacity, and Distributed Hydrology Soil Vegetation Model) of different complexity

217 gradients arising from sea-salt deposition, hydrology, soil chemistry and plant traits.

218 Variables describing geology, hydrology, soil properties, and hydrologic position were

219 develop a probability model based on surface hydrology, soil properties, geology, and sedimentary dep

220 ement and other external factors that affect hydrology, soil, and species patterns.

221 Topographically linked hydrology-soil-vegetation sequences, or catenas, underpi

222 idly receding glaciers are driving shifts in hydrology, species distributions and threatening microbi

223 mpact of microplastic (MP) pollution on soil hydrology, specifically in retaining and releasing moist

224 These findings are important for hydrology study in observation scarce mountainous areas,

225 cluding morphology, water residence time and hydrology, such as the influence of Lake Okeechobee disc

226 ramatically alters biogeochemical processes, hydrology, surface energy balance, and vegetation cover.

227 st-century regime shifts in the coupled soil-hydrology system and rapid intensification of wildfires

228 host a high-pressure distributed subglacial hydrology system in between lower-pressure subglacial ch

229 Similarly, altered hydrology, temperature, CO2 concentration and land use w

230 Plot-scale CH(4) emissions were driven by hydrology, temperature, vegetation, and wetland size.

231 ematic spatial covariation of topography and hydrology that are linked to aging volcanic bedrock, sug

232 hanging demographics and climatic impacts on hydrology that drive nutrient transport.

233 poral coupling between biodiversity and soil hydrology that is useful to enhance ecohydrological mode

234 rocesses in response to changing climate and hydrology that may not manifest in changes in net annual

235 ty were caused by spatial variations in soil hydrology, the change from local groundwater to snowmelt

236 ng season length and simulated subdaily soil hydrology to parameterize ring width increment simulatio

237 nt strategy that restores the predevelopment hydrology to prevent increased stormwater runoff from la

238 informed by landscape ecology and catchment hydrology to quantify spatiotemporal variability across

239 energy processes with surface and subsurface hydrology to study transpiration partitioning at the con

240 Chamber-based fluxes were complemented with hydrology, total fluxes (diffusion + ebullition), and su

241 made possible by widespread data mapping of hydrology, transportation infrastructure, population dis

242 ven lakes in northern Wisconsin that vary in hydrology, trophic status, and landscape position.

243 lity as a function of climate, lithology and hydrology using regional aerial dieback surveys and site

244 1500 km latitudinal transect that varied in hydrology, vegetation, and soil chemistry.

245 e arctic landscape, including aspects of the hydrology, vegetation, permafrost, and glaciers, but eff

246 River water levels (RWLs) are fundamental to hydrology, water resource management, and disaster mitig

247 ollected over 4 years and calibrated modeled hydrology, we calculated methylmercury (MeHg) and total

248 the importance of climate-driven changes in hydrology when assigning attribution to decadal changes

249 nt a unique wetland ecosystem of distinctive hydrology which support unique biodiversity and globally

250 negatively impacted significantly more than hydrology, wildlife and fire dynamics, but equal to vege

251 ses in 5 broad categories: soil, vegetation, hydrology, wildlife, and fire dynamics.

252 model was developed to integrate subsurface hydrology with reactive salt transport for a 1,400-km(2)

253 device offering new insights into soil-plant hydrology, with applications for functional root phenoty

254 ean state changes in climate on the region's hydrology, with clear implications for the study site (a

255 tic warming is affecting snow cover and soil hydrology, with consequences for carbon sequestration in