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  • 1
    Online Resource
    Online Resource
    London : IWA Publishing
    Description / Table of Contents: Cover -- Contents -- Editorial: Hydrology and water resources management in a changing world -- ACKNOWLEDGEMENTS -- REFERENCES -- A dynamic river network method for the prediction of floods using a parsimonious rainfall-runoff model -- ABSTRACT -- INTRODUCTION -- METHODOLOGY -- Study catchments and data -- The DDD rainfall-runoff model -- Subsurface -- Runoff dynamics -- Model parameters and calibration -- Dynamic river network routine -- Correlation between Ac and Fc with environmental factors -- RESULTS -- Performance of DDD with and without dynamic river network -- Correlation between Ac and Fc with environmental factors -- DISCUSSION -- Dynamic river networks -- Correlation of Ac and Fc with environmental factors -- CONCLUSIONS -- ACKNOWLEDGEMENTS -- REFERENCES -- Testing the applicability of physiographic classification methods toward improving precipitation phase determination in conceptual models -- ABSTRACT -- INTRODUCTION -- STUDY AREA -- METHODS -- Original-automated classification - all sites -- New-automated method - all sites -- Semi-manual method - all sites -- Relief versus elevation - mountain and hill sites only -- Station radius size - mountain and hill sites only -- Calculations -- RESULTS -- All sites - comparison of three methods -- Mountain and hill sites - relief versus elevation -- Mountain and hill sites - station radius size -- DISCUSSION -- Automated versus semi-manual methods -- Refinement of classification for topographically complex regions -- CONCLUSIONS -- SUPPLEMENTARY MATERIAL -- REFERENCES -- Precipitation phase uncertainty in cold region conceptual models resulting from meteorological forcing time-step intervals -- ABSTRACT -- INTRODUCTION -- METHOD -- RESULTS AND DISCUSSION -- CONCLUSIONS -- REFERENCES -- Can model-based data products replace gauge data as input to the hydrological model? -- ABSTRACT.
    Type of Medium: Online Resource
    Pages: 1 online resource (246 pages)
    Edition: 1st ed.
    ISBN: 9781789062175
    Series Statement: In Focus - Special Book Series
    DDC: 551.48
    Language: English
    Note: Description based on publisher supplied metadata and other sources
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  • 2
    Publication Date: 2021-07-19
    Description: In this study latent heat flux (λE) measurements made at 65 boreal and arctic eddy-covariance (EC) sites were analyses by using the Penman–Monteith equation. Sites were stratified into nine different ecosystem types: harvested and burnt forest areas, pine forests, spruce or fir forests, Douglas-fir forests, broadleaf deciduous forests, larch forests, wetlands, tundra and natural grasslands. The Penman–Monteith equation was calibrated with variable surface resistances against half-hourly eddy-covariance data and clear differences between ecosystem types were observed. Based on the modeled behavior of surface and aerodynamic resistances, surface resistance tightly control λE in most mature forests, while it had less importance in ecosystems having shorter vegetation like young or recently harvested forests, grasslands, wetlands and tundra. The parameters of the Penman–Monteith equation were clearly different for winter and summer conditions, indicating that phenological effects on surface resistance are important. We also compared the simulated λE of different ecosystem types under meteorological conditions at one site. Values of λE varied between 15% and 38% of the net radiation in the simulations with mean ecosystem parameters. In general, the simulations suggest that λE is higher from forested ecosystems than from grasslands, wetlands or tundra-type ecosystems. Forests showed usually a tighter stomatal control of λE as indicated by a pronounced sensitivity of surface resistance to atmospheric vapor pressure deficit. Nevertheless, the surface resistance of forests was lower than for open vegetation types including wetlands. Tundra and wetlands had higher surface resistances, which were less sensitive to vapor pressure deficits. The results indicate that the variation in surface resistance within and between different vegetation types might play a significant role in energy exchange between terrestrial ecosystems and atmosphere. These results suggest the need to take into account vegetation type and phenology in energy exchange modeling.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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