Add this suggestion to a batch that can be applied as a single commit.
This suggestion is invalid because no changes were made to the code.
Suggestions cannot be applied while the pull request is closed.
Suggestions cannot be applied while viewing a subset of changes.
Only one suggestion per line can be applied in a batch.
Add this suggestion to a batch that can be applied as a single commit.
Applying suggestions on deleted lines is not supported.
You must change the existing code in this line in order to create a valid suggestion.
Outdated suggestions cannot be applied.
This suggestion has been applied or marked resolved.
Suggestions cannot be applied from pending reviews.
Suggestions cannot be applied on multi-line comments.
Suggestions cannot be applied while the pull request is queued to merge.
Suggestion cannot be applied right now. Please check back later.
TYPE: New feature
KEYWORDS: convection, forecast, cloud, precipitation
SOURCE: Ivan Ristic (Weather2 - www.weather2.rs)
DESCRIPTION OF CHANGES:
To improve cloud and precipitation forecast we developed new convective scheme and we implemented it in WRF model. Convective clouds have always been a great challenge for meteorologists, among other things, due to the inability to describe processes of cloud formation, development and dissipation in a satisfactory manner. Applying parameterization in to the models has lead to simpler form of equations that could be used in practice, and thus different types of convective schemes in numerical weather prediction models appeared. Proposed convective scheme is based on basic elements that affect convection such as convective available potential energy (CAPE), vertical velocity at the base of the cloud, the amount of ice in the cloud and important assumptions. The scheme is conceived as a wet vertical turbulent diffusion and a logical continuation of dry vertical planetary boundary layer (PBL) turbulent diffusion. The scheme determines the vertical levels in the model where the convective cloud begins and ends. Integrated in the model this scheme showed good results in practice.
A complete description is now found in Ristic I., Kordic I., April 2022: Convective velocity scale and its application in convective parameterization
which can be found at ResearchGate:
https://www.researchgate.net/publication/359716993_Convective_velocity_scale_and_its_application_in_convective_parametrization
LIST OF MODIFIED FILES:
Registry/Registry.EM_COMMON
phys/Makefile
phys/module_cu_ristic.F
phys/module_cumulus_driver.F
phys/module_physics_addtendc.F
phys/module_physics_init.F
TESTS CONDUCTED:
Test 1 ( Naples, Italy 11th August, 2016)
Night summer convection developed in Tyrrhenian sea moved slowly toward east and arrived around 12 UTC to the city of Naples, (Figure 1). Convection and clouds over Naples can be seen both on the cloud maps from the model as well as from satellite images and they correspond well (Figure 2 and Figure 3).
Figure 1. (WRF Ristic micro+conv scheme, precipitation from 06-12 UTC, 11.8.2016.)
Figure 2. ( WRF Ristic micro+conv scheme clouds at 12 UTC, 11.8.2016.) Figure 3. (Satelite image 11.8.2016., sat24.com)
Test 2 ( Sicily, Italy 8th September, 2017)
Mix of stratiform and convective clouds formed over Mediterranean sea (between Sicily and Africa) and caused precipitation over Sicily that lasted for couple of hours.This situation was forecasted well with proposed scheme (Figure 4). The cloud cover from the model with proposed convective scheme (Figure 5) correspond well with the satellite image (Figure 6).
Figure 4. (WRF Ristic micro+conv scheme, precipitation from 12-18 UTC, 8.9.2017.)
Figure 5. (WRF Ristic micro+conv scheme clouds at 12 UTC, 8.9.2017.) Figure 6. (Satelite image 12 UTC , 8.9.2017., sat24.com)