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@INPROCEEDINGS{Zhang:1021923,
author = {Zhang, Yikui and Wangner, Niklas and Görgen, Klaus and
Kollet, Stefan},
title = {{A}nalysis of {C}loud {W}ater {S}caling to {S}urface
{M}oisture {F}luxes from {F}ully {C}oupled {T}errestrial
{S}imulations},
reportid = {FZJ-2024-01071},
year = {2023},
abstract = {Land-atmosphere (L-A) coupling is important for
understanding regional climate functioning and influencing
hydrometeorological extremes such as droughts and heatwaves,
but accurate determination of L-A coupling strength is
difficult due to complex feedback loops and varying
background atmospheric conditions. The role of clouds is
often ignored or simplified in previous L-A coupling
studies, and the non-linear control of evapotranspiration
(ET) on cloud formation and convection is poorly
understood.This study aims to diagnose the feedback between
surface moisture fluxes and cloud moisture under different
atmospheric conditions to improve our understanding of L-A
coupling, based on simulations with a fully coupled regional
climate model, the Terrestrial Systems Modelling Platform
(TSMP), over the COrdinated Regional Downscaling EXperiment
(CORDEX) EUR-11 domain at about 12 km resolution from 1979
to 2021. We investigated the L-A coupling strength by
calculating the Pearson correlation coefficient and
estimating the scaling relationship between ET, boundary
layer variables, cloud water content and its dynamics
(ΔTQC/Δt) under dry/wet and low/medium/high atmospheric
moisture dynamic regimes. In addition, the co-variability of
ΔTQC/Δt on ET and moisture flux dynamics is quantified
based on the quantile phase plot.The analysis indicates a
positive role of surface moisture flux in influencing cloud
moisture dynamics. The coupling hotspots between surface
moisture flux and cloud moisture in Europe are mainly
identified in the water-limited regions of Eastern Europe
and the Mediterranean. Two types of scaling relationships
were classified by K-means clustering over all grid points
with a clear north-south contrast, and local dry/wet
conditions could be the determining factor. Furthermore, the
coupling analysis highlights the role of enhanced moisture
flux dynamics in reducing the strength of the local L-A
moisture flux coupling, and it can determine the scaling
types of ET-ΔTQC/Δt at the local scale.},
month = {Dec},
date = {2023-12-11},
organization = {American Geophysical Union Fall
Meeting 2023, San Francisco (USA), 11
Dec 2023 - 15 Dec 2023},
subtyp = {Other},
cin = {IBG-3},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217) / SFB 1502 D02 - Simulation anthropogen bedingter
Veränderungen in regionalen Wasser- und Energiekreisläufen
(D02) (495897999)},
pid = {G:(DE-HGF)POF4-2173 / G:(GEPRIS)495897999},
typ = {PUB:(DE-HGF)6},
doi = {10.34734/FZJ-2024-01071},
url = {https://juser.fz-juelich.de/record/1021923},
}