Temperature and surface lapse rate change: a study of the UK's longest upland instrumental record
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Organic sediment pulses impact rivers across multiple levels of ecological organizationHydrological hotspots in blanket peatlands: Spatial variation in peat permeability around a natural soil pipeRotational vegetation burning effects on peatland stream ecosystemsThe dynamics of natural pipe hydrological behaviour in blanket peatCatchment-scale peatland restoration benefits stream ecosystem biodiversityMorphological change of natural pipe outlets in blanket peatNatural pipes in blanket peatlands: major point sources for the release of carbon to the aquatic systemVariable source and age of different forms of carbon released from natural peatland pipesGreenhouse gas losses from peatland pipes: A major pathway for loss to the atmosphere?Spatial and seasonal variability of peatland stream ecosystemsMid-21st century projections in temperature extremes in the southern Colorado Rocky Mountains from regional climate models
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Temperature and surface lapse rate change: a study of the UK's longest upland instrumental record
description
article
@en
wetenschappelijk artikel
@nl
наукова стаття, опублікована у квітні 2011
@uk
name
Temperature and surface lapse ...... est upland instrumental record
@en
Temperature and surface lapse ...... est upland instrumental record
@en-gb
Temperature and surface lapse ...... est upland instrumental record
@nl
type
label
Temperature and surface lapse ...... est upland instrumental record
@en
Temperature and surface lapse ...... est upland instrumental record
@en-gb
Temperature and surface lapse ...... est upland instrumental record
@nl
prefLabel
Temperature and surface lapse ...... est upland instrumental record
@en
Temperature and surface lapse ...... est upland instrumental record
@en-gb
Temperature and surface lapse ...... est upland instrumental record
@nl
P356
P1154
2-s2.0-79954580289
P1476
Temperature and surface lapse ...... est upland instrumental record
@en
P304
P356
10.1002/JOC.2136
P577
2011-04-15T00:00:00Z