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  • Late-Holocene soil toposequence in Stroud Basin, Central Wind River Mountains, western Wyoming
  • Argile ; Biogéochimie ; Chaîne de sols ; Etats-Unis ; Granulométrie ; Géographie de l'Amérique ; Minéralogie ; Montagne ; Pédologie ; Rocky Mountains ; Sol ; Toposéquence ; Wind River Range ; Wyoming
  • Effects of climate change on soils in glacial deposits, Wind River Basin, Wyoming
  • In a detailed study of soils in the Wind River Range and Wind River Basin, characteristics of near-surface horizons do not follow age trends. However, the underlying carbonate-bearing horizons do have age-related characteristics. This soil paradox
  • may be related to glacial-interglacial cycles in which 1) wind erodes near-surface horizons and then provides new parent material and 2) cryoturbation disrupts carbonate horizons, remobilizing carbonate and changing carbonate morphology but with only
  • Analyse de sensibilité ; Années 1960-2007 ; Bassin-versant ; Chine ; Donnée climatique ; Espace-temps ; Evapotranspiration ; Radiation ; Température ; Tendance du climat ; Vitesse du vent
  • China ; Climatic data ; Climatic trend ; Evapotranspiration ; Radiation ; Sensitivity analysis ; Space time ; Temperature ; Watershed ; Wind speed
  • This paper dealt with sensitivity of potentiel evapotranspiration (Eo) over China, which was divided into 10 drainage systems, including Songhua River basin, Liaohe River basin, Haihe River basin, Yellow River basin, Yangtze River basin, Pearl River
  • basin, Huaihe River drainage system, Southeast river drainage system, Northwest river drainage system and Southwest river drainage system. In addition, the calculation method of global radiation in Penman-Monteith formula was improved by optimization
  • , and the sensitivities of Penman-Monteith potential evapotranspiration to the daily maximum temperature (STmax), daily minimum temperature (STmin), wind speed (SU2), global radiation (SRs ) and vapor pressure (SVP) were calculated and analyzed based on the long-term
  • Barrage ; Bassin-versant ; Biogéographie ; Colonisation végétale ; Cours d'eau ; Distribution spatiale ; Dynamique de la végétation ; Eau ; Etats-Unis ; Great Plains ; Montana ; Nebraska ; North Dakota ; Siècle 20 ; South Dakota ; Tamaris ; Vent
  • Biogeography ; Dam ; Montana ; Nebraska ; North Dakota ; Plant colonization ; South Dakota ; Spatial distribution ; Stream ; Twentieth Century ; United States of America ; Vegetation ; Vegetation dynamics ; Water ; Watershed ; Wind ; Wyoming
  • control plantings in central Wyoming; and 3) to predict where saltcedar could invade next if it is not controlled at its advancing fronts. The AA. believe that the Wind/Bighorn River in central Wyoming was an early introduction location for saltcedar
  • in the northern Great Plains. This was followed by rapid natural dispersal northward by water and wind through the Wind/Bighorn system and into the Yellowstone and Missouri rivers in Montana.
  • Albedo ; Analyse d'image ; Correction radiométrique ; Etats-Unis ; Généralités sur la géographie ; Landsat ; Optique atmosphérique ; Radiation ; Thematic Mapper ; Télédétection ; Wind River Basin ; Wyoming
  • Assessing the impact of climate change on potential evapotranspiration in Aksu River Basin
  • Aksu ; Années 1960-2007 ; Bassin-versant ; Changement climatique ; Chine ; Espace-temps ; Evapotranspiration ; Impact ; Montagne ; Tendance du climat ; Vitesse du vent ; Xinjiang
  • China ; Climatic change ; Climatic trend ; Evapotranspiration ; Impact ; Mountain ; Space time ; Watershed ; Wind speed ; Xinjiang
  • In this paper, based on the daily meteorological data from 1960 to 2007 within and around the Aksu River Basin, reference evapotranspiration (RET) was estimated with the FAO Penman-Monteith method. The temporal and spatial variations of RET were
  • elevation areas where relative humidity predominated the change of the RET, the variations of wind velocity predominated the changes of RET almost throughout the basin.
  • analyzed by using ARCGIS and Mann-Kendall method. Multiple Regression Analysis was employed to attribute the effects of the variations of air temperature, solar radiation, relative humidity, vapour pressure and wind speed on RET. Except in some high
  • Soil catenas of calcareous tills, Whiskey Basin, Wyoming, USA
  • Bassin-versant ; Carbonate ; Catena ; Etats-Unis ; Moraine ; Pente de versant ; Propriétés du sol ; Pédogenèse ; Roche carbonatée ; Sol ; Wyoming
  • The AA. describe catenas developed on calcareous moraines of Pinedale and Bull Lake ages at Whikey Basin on the eastern flank of the Wind River Range, Wyoming, in 2 separate valleys. Both catenas in both valleys contain primary carbonates
  • Evolutions naturelles et anthropiques des paysages arides du bassin du Tarim
  • Air temperature ; Arid area ; Asia ; Central Asia ; Chemical pollution ; Desertification ; Hydrological regime ; Natural landscape ; Precipitation ; River basin ; Stream ; Water erosion ; Wind erosion ; Years 1950-59 ; Years 1990-99
  • Années 1950 ; Années 1990 ; Asie ; Asie centrale ; Bassin fluvial ; Cours d'eau ; Domaine aride ; Désertification ; Erosion hydrique ; Erosion éolienne ; Paysage naturel ; Pollution chimique ; Précipitation ; Régime hydrologique ; Tarim
  • Aeolian modification of moraine soils, Whiskey Basin, Wyoming, USA
  • Soils along catenas of Pinedale and Bull Lake at Whiskey Basin, in the Wind River Range, were sampled to assess the effects of aeolian processes on soil development. Aeolian processes appear to have influenced soils by both depositing sediments
  • and eroding topsoils. Pedogenic silt (often used as an indicator of wind deposition) accumulated in the Bluff Lake soils moderately correlate with pedogenic clay accummulated, suggesting that fine sediments may have been deposited and incorporated into soil
  • formation here. The AA. suggest that aeolian modification of soils also can be demonstrated on moraines at Whiskey Basin.
  • River sediment supply, sedimentation and transport of the highly turbid sediment plume in Malindi Bay, Kenya
  • Baie ; Bassin-versant ; Courant littoral ; Kenya ; Littoral ; Malindi ; Mousson ; Transport sédimentaire ; Turbidité ; Utilisation du sol
  • to be due to the Ekman transport generated by the onshore monsoon winds. The high sediment discharge into Malindi Bay can be attributed to land use change in the Athi-Sabaki River Basin in addition to rapid population increase which has led to clearance
  • in a period of high intensity South East Monsoon (SEM) winds that generate strong north flowing current that transports the river sediment plume northward. The mechanism of advection of the sediment plume north or south of the estuary is mainly thought
  • terrigenous sediment load. The river freshwater supply into the bay is highly variable. Relatively low peak flows occurred in November during the North East Monsoon (NEM). The discharge of highly turbidity river water into the bay in April and May occurs
  • Decreasing potential evapotranspiration in the Huanghe River Watershed in climate warming during 1960–2010
  • Années 1960-2010 ; Bassin-versant ; Changement climatique ; Chine ; Evapotranspiration ; Evapotranspiration potentielle ; Huanghe ; Précipitation ; Réchauffement climatique ; Régression multiple ; Température ; Vitesse du vent
  • China ; Climatic change ; Climatic warming ; Evapotranspiration ; Huang He ; Multiple regression ; Potential evapotranspiration ; Precipitation ; Temperature ; Watershed ; Wind speed
  • , relative humidity and average wind speed. The decrease of wind speed in the Huanghe River Watershed may be the dominating factor causing potential evapotranspiration decreasing.
  • According to the meteorological observation data of 72 stations from 1960 to 2010 in the Huanghe (Yellow) River Watershed, China, the long-term variations of potential evapotranspiration, calculated in the modified Penman-Monteith model were
  • paradox in the Huanghe River Watershed. Calculated in multiple regressions, the contribution to potential evapotranspiration change of related meteorological factors was discussed, including mean pressure, maximum and minimum temperature, sunshine hours
  • Application of stream ordering to the Ardeche River basin, southern France. Quantitative relief classification in the Ardeche River basin, southern France
  • Ardèche ; Ardèche, bassin ; Bassin-versant ; Classification ; Cours d'eau ; France ; Géographie de l'Europe ; Géomorphométrie ; Ordonnancement ; Relief ; Rhône, bassin ; Rhône-Alpes ; Réseau de drainage
  • Holocene loess and its deposition dynamics in the upper reaches of the Huaihe River
  • Bassin-versant ; Chine ; Eolien ; Granulométrie ; Géochronologie ; Hebei ; Holocène ; Loess ; Paléoclimat ; Paléosol ; Poussière éolienne ; Quaternaire ; Stratigraphie ; Susceptibilité magnétique ; Transport éolien ; Variation climatique ; Yinhe
  • the upper reaches of the Huaihe River and the Loess Plateau. The loess in the upper reaches of the Huaihe River was a wind blown deposition of near source, while the coarser dust mainly came from loose alluvial deposits of alluvial and proluvial fans
  • of the Yellow River. The yielding and carrying dynamics of the dust in the Huaihe River is the northeast wind prevails in the winter half year.
  • This paper aims to explore the pedogenic process, dust source, and transport dynamics of the loess-soil sequences in the upper reaches of the Huaihe River, based on comparison of the geographical setting, magnetic susceptibility, grain size between
  • Suivi de la vitesse du vent sur le bassin-versant de la Volga et de l'Oural au XXème siècle
  • Climatic data ; European part of Russia ; Seasonal variation ; Twentieth Century ; Ural River ; Volga ; Watershed ; Wind ; Wind speed ; Years 1930-39 ; Years 1990-99
  • Années 1930 ; Années 1990 ; Bassin-versant ; Donnée climatique ; Russie d'Europe ; Siècle 20 ; Ural fleuve ; Variation saisonnière ; Vent ; Vitesse du vent ; Volga
  • Evaluation et analyse pour la période de 1936 à 2000 et pour des périodes plus courtes des tendances linéaires de vitesse du vent sur le bassin-versant des cours d'eau de la Volga et de l'Oural.
  • Erosion and sediment yields as influenced by coupled eolian and fluvial processes : the Yellow River, China
  • Bassin-versant ; Bilan sédimentaire ; Charge en suspension ; Chine ; Domaine aride ; Eolien ; Erosion fluviatile ; Huanghe ; Transport sédimentaire
  • Based on data from the middle Yellow River, a model of erosion and sediment yield is proposed to describe coupled eolian and fluvial processes in a transitional zone from arid to sub-humid climates, and to explain rapid erosion and a high sediment
  • yield in the zone. As a result, most of the previously stored eolian sand and material supplied by mass-wasting of loess can be transported to the major tributaries and the main stream of the Yellow River, resulting in the high specific sediment yield
  • . There exists an optimal grain size composition which maximizes suspended sediment concentration in the study area, resulted from the combined wind-water processes.
  • Unimpaired and regulated discharge in the Sacramento River Basin, California
  • Aménagement hydraulique ; Barrage ; Bassin-versant ; California ; Débit ; Etats-Unis ; Hydrologie fluviale
  • Reservoirs alter monthly and annual discharge quantities in the Sacramento River Basin of northern California and this practice obscures the natural variability of river discharge. - (DWG)
  • Suspended and solute transport in a small glaciated catchment, Bertram River, Central Spitsbergen, in 2005-2006
  • Arctique ; Bassin-versant ; Charge en solution ; Charge en suspension ; Eau de fonte ; Fluvioglaciaire ; Foehn ; Hydrochimie ; Périglaciaire ; Région polaire ; Spitsbergen ; Svalbard ; Vent
  • Arctic Region ; Fluvioglacial features ; Foehn ; Hydrochemistry ; Meltwater ; Periglacial features ; Polar region ; Solution load ; Spitsbergen ; Suspended load ; Svalbard ; Watershed ; Wind
  • This paper presents data on hydrochemistry and suspended sediment dynamics from a small glaciated catchment in Svalbard. Bertram River is distinguished by a system of waterfalls which divides the catchment in 2 parts : an upper glaciated part
  • located on mountainous plateau, and a lower part where an abraided plain has been formed within the bottom of the Ebba River valley. On the basis of observations it is concluded that a particular role in the conditioning of glaciofluvial transport
  • was played by an extreme weather event in the form of föhn-type wind, observed in the decline of ablation season and also by waterfalls which diversified the fluvial activity.
  • Action biogène ; Analyse du paysage ; Bassin-versant ; Colorado ; Couverture végétale ; Etats-Unis ; Forêt ; Incendie de forêt ; Insecte ; Montagne ; Paysage ; Siècle 15 ; Siècle 20 ; Vent
  • Biogenic process ; Colorado ; Fifteenth Century ; Forest ; Forest fire ; Insect ; Landscape ; Landscape analysis ; Mountain ; Plant cover ; Twentieth Century ; United States of America ; Watershed ; Wind
  • This study uses dendrochronological evidence to investigate the disturbance history of the Middle Fork Elk River watershed, and examines the spatial and temporal relationships among disturbance events of varying severity : blowdown, insect outbreaks
  • Annual variation ; China ; Evapotranspiration ; Potential evapotranspiration ; Seasonal variation ; Solar radiation ; Spatial variation ; Water cycle ; Wind speed
  • and the temporal trends of the regional means for 10 major river basins and whole China are analyzed. Through a partial correlation analysis, the major climate factors which affect the temporal change of the potential evapotranspiration are analyzed. Decline
  • tendencies of sunshine duration and/or wind speed in the same period appear to be the major causes for the negative trend of the potential evapotranspiration in most areas.
  • Characteristics of silt deposition in the Kosi river basin
  • Bassin-versant ; Fluviatile ; Géographie de l'Asie ; Inde ; Kosi ; Silt ; Sédimentation