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The Climatic Role of Interactive Leaf Phenology in the Vegetation- Atmosphere System of Radiative-Convective Equilibrium Storm-Resolving Simulations Cover

The Climatic Role of Interactive Leaf Phenology in the Vegetation- Atmosphere System of Radiative-Convective Equilibrium Storm-Resolving Simulations

Open Access
|Jun 2022

Figures & Tables

Table 1

List of conducted experiments with interactive leaves defined by their initial values of LAI, of soil moisture, and of soil saturation.

EXPERIMENT NAMELAI0(m2 m–2)θ0 (m3 m–3)θ0 (%)
INT_LAI04_SM270.40.1027
INT_LAI04_SM410.40.1541
INT_LAI04_SM540.40.2054
INT_LAI04_SM680.40.2568
INT_LAI04_SM810.40.3081
INT_LAI04_SM950.40.3595
INT_LAI30_SM273.00.1027
INT_LAI30_SM413.00.1541
INT_LAI30_SM543.00.2054
INT_LAI30_SM683.00.2568
INT_LAI30_SM813.00.3081
INT_LAI30_SM953.00.3595
Table 2

List of conducted sensitivity experiments.

EXPERIMENT NAMEVARIABLE THAT HAS FIXED LAI AT 0.4m2 m–2
INT_LAI04_SM54_gcgc, canopy conductance
INT_LAI04_SM54_cvCv, vegetation fraction
INT_LAI04_SM54_aα, albedo
Figure 1

Time series of (a) the difference between evapotranspiration (ET, mm day–1) and precipitation (P, mm day–1), and (b) surface temperature (Ts, K) for INT_LAI30_SM27 (gray), INT_LAI30_SM41 (yellow), and INT_LAI30_SM54 (green).

Figure 2

(a) Leaf area index (LAI, m2 m–2), (b) evapotranspiration (ET, mm day–1), and (c) surface temperature (Ts, K) as a function of initial soil saturation (θ0, %) at equilibrium for INT_LAI04_SMxx (light green circles), INT_LAI30_SMxx (dark green squares), FIX_LAI04_SMxx (light red triangles), and FIX_LAI30_SMxx (dark red triangles). The gray area indicates the sparsely vegetated equilibrium category.

Figure 3

Same as Figure 2 but for (a) transpiration (Tr, mm day–1) and (b) bare soil evaporation (Eb, mm day–1).

Figure 4

Same as Figure 2 but for (a) cloud water path (CWP, mm) and (b) surface net radiation (Rn, W m–2) only for the simulations with interactive leaves.

Figure 5

Differences in evapotranspiration, transpiration and bare soil evaporation between INT_LAI04_SM54 and FIX_LAI04_SM54, denoted as FIX04 on the x-axis, as well as the differences between INT_LAI04_SM54 and the three sensitivity experiments INT_LAI04_SM54_gc, INT_LAI04_SM54_cv, INT_LAI04_SM54_a, denoted gc, Cv and α on the x-axis.

Figure A1

Domain mean profiles of (a) potential temperature and (b) specific humidity at the initial time (dashed line) and at 6 hours for total turbulent energy scheme denoted TTE (blue line), 3D Smagorinsky scheme in the NWP version denoted NWP (black), and the newly implemented 3D Smagorinsky scheme denoted SMA (red).

Figure A2

Time series of (a, b, and c) resolved and (d, e, and f) sub-grid scale heat flux (shading, W m–2) using (a, d) total turbulent energy scheme, (b, e) 3D Smagorinsky scheme in the NWP physics package, and (c, f) the newly implemented 3D Smagorinsky scheme.

DOI: https://doi.org/10.16993/tellusb.26 | Journal eISSN: 1600-0889
Language: English
Page range: 164 - 175
Submitted on: Jan 26, 2022
Accepted on: May 2, 2022
Published on: Jun 21, 2022
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2022 Junhong Lee, Cathy Hohenegger, Andreas Chlond, Reiner Schnur, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.