ライフサイエンスコーパス: hydrology

1 stem properties including carbon balance and hydrology.

2 PSFs which are dependent on their unimpacted hydrology.

3 overturning circulation and tropical Pacific hydrology.

4 portant effects on the biosphere and surface hydrology.

5 applications in the medical sciences and in hydrology.

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

7 respond to changes in stream temperature and hydrology.

8 that link peat accumulation and groundwater hydrology.

9 volutionary time scales of geomorphology and hydrology.

10 s to capture the topography critical to soil hydrology.

11 obial community occurs at sites with varying hydrology.

12 cluded in the conceptual model of subglacial hydrology.

13 ctors, including temperature, irradiance and hydrology.

14 nteractions between subsurface chemistry and hydrology.

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

16 ith significant consequences for terrestrial hydrology.

17 ical processes such as seasonality and tidal hydrology.

18 at is relevant for climate change impacts on hydrology.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

44 complex feedbacks between peat accumulation, hydrology and vegetation.

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

69 Hydrology drives the carbon balance of wetlands by contr

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

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

103 Hydrology refers to the whole panoply of effects the wat

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

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

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

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

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

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

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

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

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

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

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

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

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

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

118 1500 km latitudinal transect that varied in hydrology, vegetation, and soil chemistry.

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

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

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

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