WebOct 1, 2016 · Land-Surface Models (LSMs) exhibit large spread and uncertainties in the way they partition precipitation into surface runoff, drainage, transpiration and bare soil evaporation. To explore to what extent water isotope measurements could help evaluate the simulation of the soil water budget in LSMs, water stable isotopes have been … WebMay 8, 2024 · This paper discusses the capability of this new version of the ORCHIDEE land surface model to represent the water and heat transfers in Arctic environments, after evaluation against data from two instrumented sites located in a continuous permafrost area, especially instrumented for the WSibIso-Megagrant project ( www.wsibiso.ru ).
HESS - Testing water fluxes and storage from two …
WebWhile the paper focuses on a comparison of the soil moisture dynamics simulated by ORCHIDEE land-surface model with ESA-CCI soil moisture product, the analysis is done … WebDec 20, 2024 · In this study, we investigated how well the land surface model (LSM) Organising Carbon and Hydrology In Dynamic Ecosystems (ORCHIDEE) (v7266) simulates … cis mitsubishi
Confronting Soil Moisture Dynamics from the ORCHIDEE Land Surface Model …
WebImpact model: ORCHIDEE Impact model: ORCHIDEE ... Wang F, Wang T, Wang X, Wang Y, Yin Z, Lauerwald R, Joetzjer E, Qiu C, Kim H, Ciais P et al. ORCHIDEE-MICT (revision 4126), a land surface model for the high-latitudes: model description and validation. Geoscientific Model Development Discussions,None,1-65,2024 WebPermafrost models are either developed as stand-alone algorithms or as modules that are incorporated into Land Surface Models (LSMs) and General Circulation Model (GCMs) [ 34 ]. One such LSM is ORCHIDEE (ORganizing Carbon and Hydrology in Dynamic EcosystEms). This model is designed to represent terrestrial fluxes (carbon, water and energy budget). WebFigure 1b illustrates how ORCHIDEE (ORganizing Carbon and Hydrology In Dynamic EcosystEms: the land-surface model) represents the surface water budget. Rainfall is partitioned into interception by the canopy and through-fall rain. Through-fall rain, snow melt, dew and frost fill the soil. The soil is represented by two water reservoirs: cism online prep