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The LES ARM Symbiotic Simulation and Observation (LASSO) Activity

Today’s presenter: William I. Gustafson Jr.

Core LASSO Team: William I. Gustafson Jr.1, Andrew M. Vogelmann2, Xiaoping Cheng3,

Mark Delgado2, Satoshi Endo2, Tami Fairless2, Krista Gaustad 1, Karen Johnson2,

Carina Lansing1, Zhijin Li3, John Rausch2, Eddie Schuman1, Heng Xiao1, Damao Zhang1

1 Pacific Northwest National Laboratory; 2 Brookhaven National Laboratory; 3JPL/UCLA; 4U. of Maryland Baltimore County

https://www.arm.gov/capabilities/modeling/lasso

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What is LASSO?

https://www.arm.gov/capabilities/modeling/lasso

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LASSO = Large-Eddy Simulation (LES) Atmospheric Radiation Measurement (ARM) Symbiotic Simulation and Observation activity

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Big picture motivation for LASSO

  • Intent of LASSO: leverage high-resolution modeling to enhance the value of ARM’s suite of observations for researchers

  • Motivated by goal of bridging the gap between observations and scales used in forecast and climate models
    • Increase understanding of linkages between different observations
    • Advancement of cloud and boundary layer theories and parameterizations
    • Enable model development and better link observations and models

  • Vetted large-eddy simulation (LES) provides a plausible proxy for unobservable details in the context of the observations

https://www.arm.gov/capabilities/modeling/lasso

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LASSO’s library approach

  • Targets specific weather regimes with libraries of LES cases

  • Curates a suite of relevant observations associated with the chosen regime

  • Provides a basic comparison between the observations and the LES to aid selection of simulations

  • Simplifies downloading and use, e.g., bundling of data, online tools targeting key details and download LASSO data

https://www.arm.gov/capabilities/modeling/lasso

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Current LASSO scenarios

  1. Shallow-convection: Generated 5 years of cases
    • Focus on daytime, continental, shallow convection
    • Southern Great Plains, Oklahoma

  • LASSO-CACTI: Beta release was available with full release later in 2023
    • Focus on convective initiation and early stages of convective upstage growth for deep convection
    • Córdoba, Argentina

  • LASSO-ENA: In development with staged data release in 2024-25
    • Focus on maritime stratiform and related precipitation processes
    • Graciosa Island, Azores

https://www.arm.gov/capabilities/modeling/lasso

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LASSO being applied to a range of atmospheric topics

  • Published examples using LASSO
    • Quantifying shallow convection statistics
    • Understanding shallow convection processes
    • Cloud-radiation connections
    • 1D vs. 3D radiation methodologies
    • Parameterization development & evaluation
    • Radar scan strategies for shallow clouds
    • Understanding dust transport in boundary layer
    • Included within the Global Modeling Testbed (GMTB) for parameterization evaluation and single-column model use
  • Also a great tool for teaching!

https://www.arm.gov/capabilities/modeling/lasso

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Cloud Number Densities

Cloud Size Distributions

Cloud Size

Simulated cloud field each hour

Time

Neggers et al. (2019, JAS)

Time

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Large-eddy simulations for shallow convection: LASSO-ShCu

Gustafson et al., 2020, BAMS, https://doi.org/10.1175/BAMS-D-19-0065.1

Nitty gritty details: LASSO-ShCu Technical Description: https://www.arm.gov/publications/tech_reports/doe-sc-arm-tr-216.pdf

https://www.arm.gov/capabilities/modeling/lasso

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Available shallow-convection simulations

  • 5 years of cases at the Southern Great Plains (SGP) atmospheric observatory
  • ShCu season lasts roughly from April to September
  • Cases picked based on presence of shallow convection and avoidance of synoptic complications
  • Ensembles generated for each date

https://www.arm.gov/capabilities/modeling/lasso

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Year

Number

of Cases

2015

5

2016

13

2017

30

2018

30

2019

17

Total

95

Available ShCu Cases

>760 simulations

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LASSO’s shallow-convection LES methodology

  • Use WRF model with added LES capabilities (early years also include SAM runs)
  • Provide a statistical representation of the clouds; a traditional LES approach with doubly periodic boundaries and homogeneous surface
  • dx = 100 m, domain width = 25 km (early runs use 14 km)
  • Initialized with observed sounding at ~6 LST
  • Large-scale forcing ensemble to inform forcing uncertainty and cloud sensitivity
  • Output saved every 10 minutes

https://www.arm.gov/capabilities/modeling/lasso

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Domain configuration

  • Grid spacing: dx=100 m; dz=30 m up to 5 km, then stretches to 300 m at domain top
    • Captures shallow convection processes sufficiently to provide a good representation of the clouds
    • Resolution chosen to capture the clouds—grid spacing too large to capture stable conditions and boundary layer transitions, particularly during evening
    • Implications
      • Simulations good to use during midday
      • Avoid first several hours due to model spin-up and evenings when turbulence does not decay accurately
      • Timing of cloud decay can be off due to not capturing turbulence decay timing

https://www.arm.gov/capabilities/modeling/lasso

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10-Jun-2016, Sim. ID 20

Spin-up period

PBL collapse

ARSCL

WRF

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Handling of the lower boundary conditions

  • Flat, uniform lower boundary for the LES
    • No terrain or vegetation variability
  • Time-dependent, specified sensible and latent heat fluxes imposed from Variational Analysis VAP
    • Averages surface flux measurements from around SGP
    • Eddy correlation system (ECOR) uses a sonic anemometer with an open-path infrared gas analyzer to measure vertical wind and water vapor
    • Energy balance Bowen ratio station (EBBR) calculates bulk aerodynamic fluxes from soil and atmospheric measurements
    • VARANAL: https://www.arm.gov/capabilities/science-data-products/vaps/varanal

  • Implications for the LES results
    • No feedback between land and atmosphere
    • Radiation has no impact on surface fluxes or energy balance
    • Surface gradients across the region are not represented

https://www.arm.gov/capabilities/modeling/lasso

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ECOR Instruments

EBBR Station

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Lateral boundary conditions

  • Doubly periodic lateral boundary conditions
  • Assuming a scale separation between larger, mesoscale conditions and the LES domain
    • Connection to larger scales achieved through a uniform, domain-wide, large-scale forcing tendency
  • Implications
    • Largest scales of simulated variability and motion are on the order of the domain size, 25 km (14 km for early years)
    • Each model column is statistically identical
      • Cannot think in terms of one-to-one comparisons to point locations
      • LES represents the average conditions around the SGP

https://www.arm.gov/capabilities/modeling/lasso

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LASSO employs an ensemble of forcings to capture the range of possible conditions

  • Large-scale forcing (LSF) datasets generated from 3 sources

    • Variational Analysis: ARM product, 300 km spatial scale

    • ECMWF IFS model: ~16, 115, & 413 km spatial scales

    • Multiscale Data Assimilation (MSDA): 75, 150, & 300 km scales;
      • GSI 3DVar data assimilation package at dx=2.5 km
      • Directly incorporates ARM observations into the analysis
        • RWP wind profiles
        • Surface meteorology

  • Total of 8 LSF ensemble members per case (includes 1 no-LSF)

https://www.arm.gov/capabilities/modeling/lasso

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Gustafson et al. (2020, BAMS)

Spread in Cloud Fraction

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Observations: ‘data scales’

https://www.arm.gov/capabilities/modeling/lasso

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20 May 2023

ARM Met and OK Mesonet Stations

13 Stations

~60 km

2018-07-04

Regional LCL Heights

~45 km

Doppler Lidar Network

2018-07-04

Regional Cloud-Base Heights

Height range ~ ± 100 m

Example of extreme variability

Regional Networks

‘Point’ or Pencil-beam

In situ or column obs

Ka-Band ARM Zenith Radar (KAZR)

Active Remote Sensing of Clouds (ARSCL) VAP

‘Local’

Total-Sky Imager (TSI)

COGS (Clouds Optically Gridded by Stereo) VAP

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Observations: variables

https://www.arm.gov/capabilities/modeling/lasso

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Variable

‘Point’

Local

Domain

Comments

In-cloud liquid water path (LWP)

X

 

 

Combined (1) AERIoe & (2) MWRRet

Cloud fraction

ARSCL

TSI or COGS*

 

To be discussed

2-D Time-height cloud mask

ARSCL

COGS*

 

To be discussed

Cloud-base height

 

X

Doppler lidar network

Lifting condensation level (LCL) height

X

X

Met stations (CF or Met Network)

Thermo state variables: T, Qv, and RH

At the surface

X

Central Facility met. station

Middle of the boundary layer (BL)

(500-700 m average)

X

Blended Raman lidar & AERIoe profiles

*COGS available for 2018 & 2019 only

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Observations: cloud fraction sources and comments

Cloud fraction

    • Sources
      • Total-Sky Imager (TSI)
      • ARSCL (z < 5 km)
      • COGS (Romps and Öktem, BAMS, 2018)
    • Comments
      • TSI can be contaminated by upper-level cloud
      • ARSCL too sensitive and is pencil-beam obs
      • Good correlation between TSI and ARSCL time series

indicates no upper-level cloud influencing the TSI

      • COGS (when available) reliable for cloud frac < ~0.5-0.6

2-D time-height cloud mask

    • Sources
      • ARSCL
      • COGS (when available)
    • Comments
      • ARSCL is a pencil-beam obs and can be contaminated by insects (correction method in progress by Christopher Williams et al.)

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ARSCL

2-D Time-Height Cloud Frequency/Fraction

COGS

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LASSO Metadata Table for identifying simulations

  • LASSO data bundles identified by combination of
    1. Case date
    2. Simulation ID

  • Identify the simulation ID when publishing!

  • Metadata associated with each simulation ID can change between case dates

  • Metadata Table helps identify metadata and search for relevant simulations

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The LASSO Bundle Browser

https://adc.arm.gov/lassobrowser

Developed and/or maintained by

    • Kyle Dumas
    • Michael Giansiracusa
    • Bhargavi Krishna

Enables:

    • Interactive querying of LASSO sims & skill
    • Contains diagnostic plots
    • Ordering of data bundles

https://www.arm.gov/capabilities/modeling/lasso

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E

D

E

C

B

A

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Deep convection during CACTI:�LASSO-CACTI

William Gustafson

Pacific Northwest National Laboratory

https://www.arm.gov/capabilities/modeling/lasso

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CACTI & RELAMPAGO field campaigns

  • CACTI = Cloud, Aerosol, and Complex Terrain Interactions
    • DOE ARM funded
    • October 2018 through April 2019

  • RELAMPAGO = Remote sensing of Electrification, Lightning, And Mesoscale/Microscale Processes with Adaptive Ground Observations
    • NSF funded
    • June 2018 through April 2019

https://www.arm.gov/capabilities/modeling/lasso

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Map of CACTI Deployment

in Argentina

Flights

RELAMPAGO Assets

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Why Córdoba, Argentina?

  • Córdoba region has a very high frequency of initiating mesoscale convective systems (MCSs)

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TRMM Statistics for MCS Frequency

Freq. of large MCS initiation based on Tb

Freq. of IR Tb<235 K for initiated MCSs

6 hours later…

12 hours later…

9%

50%

50%

50%

Varble et al. (CACTI Science Plan, 2018)

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CACTI Approach

  • Varble, A. C., et al., 2021: Utilizing a Storm-Generating Hotspot to Study Convective Cloud Transitions: The CACTI Experiment. BAMS, 102, E1597-E1620, doi:10.1175/BAMS-D-20-0030.1.

  • Nesbitt S. W., et al., 2021: A Storm Safari in Subtropical South America: Proyecto RELAMPAGO. BAMS, 102, E1621-E1644, doi:10.1175/BAMS-D-20-0029.1.

  • AMS special collection: https://journals.ametsoc.org/collection/RELAMPAGO-CACTI

https://www.arm.gov/capabilities/modeling/lasso

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The CACTI �Observing Facilities

  • Core instrumentation from the ARM Mobile Facility #1 (AMF1)
    • Surface suite
    • Total-sky imager
    • Micropulse lidar
    • Doppler lidar
    • Ceilometer
    • Radiometer suite
    • Aerosol suite

  • G-1 aircraft

  • Radars: e.g., C-band scanning, Ka/X-band scanning, Ka-band zenith pointing, radar wind profiler

  • See list in Varble et al. (BAMS, 2021, doi:10.1175/BAMS-D-20-0030.1)

https://www.arm.gov/capabilities/modeling/lasso

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Science drivers guide LASSO-CACTI scenario design

  • Convective cloud dynamics
    • e.g., thermal-like structures, updraft strength, and entrainment; the relationship to critical features like updraft and downdraft mass fluxes, vertical transport, and the shallow-to-deep convective transition
    • Convection-environment interactions, e.g., cold pools
    • Convective drafts in turbulent flow
  • Microphysics-dynamics interactions
    • Especially in the context of cloud-scale eddies and smaller-scale turbulence

  • Science drivers chosen to balance relevant science with computational capacity
    • LES resolution governed by cloud core requirements
    • Domain size determines portion of lifespan simulated
    • Limiting ensembles to mesoscale simulations with the potential for a small number of LES ensemble members for specific cases

https://www.arm.gov/capabilities/modeling/lasso

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Case dates target a selection of convective behavior

  • Chosen days have convection form and grow within view of ARM’s scanning radar

  • Identified 20 case dates meeting our criteria
    • Convection ranges from short-lived convection to large MCSs

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240 K

180 K

320 K

Some of the mesoscale simulations for different case dates, all plotted at the same time of day, 19 UTC

Simulated

Brightness Temperature

at 19 UTC

Δx = 2.5 km (D02)

AMF

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Mesoscale ensembles for case selection and LES boundary condition choices

  • Mesoscale ensembles run for each case date (example for 10-Nov-2018 at right)
    • 33 ensemble members based on ERA5, ERA5 Ensemble, FNL, and GFS Ensemble
    • Nested down to 2.5 km grid spacing
    • Best performing ensemble members identified based on cloud comparison to GOES-16 IR data
    • Down-selected ensemble members get final vetting using bulk CSPAR2 statistics, e.g., 20 dBZ echo-top height

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300

150

200

250

100

10-Nov-2018 21 UTC

Shading = OLR (W m-2)

Contours = 500 &

1000 m terrain height

OLR: Ensemble of ∆x=2.5 km Runs

AMF

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Modeling stages to achieve Δx=100 m

  • Stage 1: Mesoscale ensembles with Δx=7.5 & 2.5 km
    • For selecting boundary conditions and case selection

  • Stage 2: LES setup with Δx=500 & 100 m
    • For selected cases, some with several LES per case

  • Stage 3: Post-process data to simplify usage

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WRF Model Domains

∆x = 7.5 km, 2.5 km, 500 m, & 100 m

= AMF location

D01

D02

D03

D04

Δx =

D01

7.5 km

D02

2.5 km

D03

500 m

D04

100 m

Nx

130

258

750

2145

Ny

136

306

865

2775

Domain Sizes

Meso

LES

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LES domains

  • “Ndown” from D02 to D03
  • Nesting permits starting domains at different times to save resources and smooth spin-up process
    • D03 starts at 6 UTC
    • D04 can start at 12 UTC
  • Primary LES run based on best-performing mesoscale ensemble member(s)
    • Some additional LES runs for testing other BCs or physics
  • ~25 h wall time per model hour on 7168 cores of Cumulus-2

https://www.arm.gov/capabilities/modeling/lasso

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Comparison of 500 hPa Vertical Velocity at Each Grid Spacing

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Summary of what is available for LASSO-CACTI

  • Simulations
    • 33-member ensembles of kilometer-scale simulations to evaluate forcings and sensitivity of convection for 20 days, ∆x = 7.5 and 2.5 km
    • 9 days with LES simulations for a handful of forcings/physics options each day, ∆x = 500 and 100 m

  • Model data
    • Raw model output for restarts and traditional output
    • Variable subsets by category of variable, e.g., clouds, radiation, PBL
    • Input files for reproducing each run

  • Skill scores and quick-look plots

https://www.arm.gov/capabilities/modeling/lasso

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Multiscale Observational Datasets

  • Regional: Satellite-based
    • Sources
      • VISST: IR brightness temperatures (11.2 μm channel)
    • Application
      • Time-dependent areal coverage of the convective cores
  • Local: Scanning C-Band Radar-based
    • Sources
      • CSAPR-2/Taranis
    • Applications
      • Locate AMF-storm position within the LES grid
      • Time series of surface rain rates, and of radar echo-top heights
  • Point Measurements
    • Sondes (ARM & RELAMPAGO)

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Skill scores to evaluate simulations

  • Satellite brightness temperatures (Tb) for convective area development

  • Radar echo-top heights for local convective intensity

  • Radar-retrieved precipitation averaged over region

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Cloud Masks Based on Tb = 240 K Threshold

GOES-16 Observation

WRF Model

WRF Model

Scoring based on Critical Success Index, Frequency Bias, RMSD

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Where to find more information

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Additional Slides�LASSO-ShCu

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LASSO’s version of WRF model

  • Available at https://code.arm.gov/lasso/lasso-wrf
    • In the “wrf_faster” branch of the repository
  • Traces heritage back to the Fast-physics System Testbed and Research (FASTER) project at BNL circa 2010
  • Based on WRF v3.8.1
  • Added features over default WRF in a new ‘em_crm’ build category
    • Extra LES-related output
      • Time averaging between output times
      • Volumes, profiles, and column-integrated quantities; spatial averaging
      • Specialized LES diagnostics, e.g., vertical fluxes of heat and moisture, in-cloud vs. all-domain averages
    • Streamlined handling of LES initialization and large-scale forcing
    • Ability to use large-scale forcing and/or nudging toward profiles
    • Customized Morrison microphysics with 4-mode aerosol inputs (used during LASSO testing phase)

https://www.arm.gov/capabilities/modeling/lasso

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Physics configuration settings for “production years”

https://www.arm.gov/capabilities/modeling/lasso

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Category

Setting

Microphysics

Thompson (8, most cases)

Radiation

RRTMG SW & LW (4)

Surface Layer

Revised MM5 Monin-Obukhov (1)

Surface Physics (Land)

Thermal Diffusion (1)

SGS Scheme (km_opt)

1.5 order TKE (2)

  • Ice microphysics activates even though we focus on shallow convection because of tall model top
    • Attempt to capture cirrus clouds with varying success
    • Some ensemble members transition to deep or mid-level cloud

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Model data available in LASSO data bundles

  • LASSO “data bundles” organize data into a series of tar files
    • sgplassodiagconfobsmod#C1.m1.YYYYMMDD.tar
    • sgplassodiagraw#C1.m1.YYYYMMDD.tar
  • Other obs-related bundle files
    • sgplassohighfreqobsC1.c1.YYYYMMDD.000000.tar
    • sgplassocogsC1.c1.YYYYMMDD.000000.tar

https://www.arm.gov/capabilities/modeling/lasso

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Model inputs

Post-processed

model output

Raw model

output

~70 MB

~70 GB

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config directory of “confobsmod” tar

  • Contains input files necessary for reproducing the simulation
    • Initial sounding: wrfinput_d01.nc
    • Large-scale forcing: input_ls_forcing.nc
    • Surface fluxes: input_sfc_forcing.nc
    • WRF’s configuration file: namelist.input

  • Script to convert WRF inputs to SAM inputs: sam_input_generation.py

https://www.arm.gov/capabilities/modeling/lasso

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Formatted for em_crm option

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raw_model directory of “raw” tar

  • Contains all the raw model output from WRF
    • Every 10 minutes
    • Separate wrfout files for each model hour, i.e., 6 times per file
    • One wrfstat file per run with all times in it

  • wrfout_d01… = Standard WRF output format in netCDF

https://www.arm.gov/capabilities/modeling/lasso

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Model inputs

  • Initial conditions
    • Temperature, moisture, and wind profiles from 12 UTC sounding (5 or 6 LTC depending on day of year)
    • Random perturbations to potential temperature in lowest 33 model layers (~990 m), 0.1 K max. amplitude
  • Surface forcing
    • Regionally averaged sensible and latent heat fluxes from EBBR and ECOR stations via Variational Analysis VAP, updated hourly
  • Large-scale forcing
    • Provided as a domain-wide tendency for temperature and moisture profiles
    • Represents large-scale horizontal advection and heating/drying due to subsidence
    • Nudging to observations not used for LASSO
    • Implications
      • Synoptic changes impact whole domain at the same time—they do not propagate across the region
      • Large-scale winds not updated after initial time

https://www.arm.gov/capabilities/modeling/lasso

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wrfstat_d01 files = LES diagnostic output

  • Variables averaged/accumulated between 10-min. output times
  • Meteorological state, turbulent fluxes, cloud details, radiation, etc.
  • Variable suffixes indicate type of averaging (CS refers to “CRM statistic” from the em_crm build mode)
    • CSV = volume variable, i.e., cell-by-cell for whole volume, only time averaged and no spatial averaging
    • CSP = domain-wide horizontally averaged profile
    • CSS = slab variable, i.e., a horizontal surface either from column integrated or a surface variable
    • CST = time series, i.e., single point per time from horizontal averaging of column-integrated or surface variables

https://www.arm.gov/capabilities/modeling/lasso

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Types of wrfstat Variables

CSV is to CSP as CSS is to CST

LASSO Domain

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obs_model directory of “confobsmod” tar

  • Contains post-processed and summarized model data
    • Generated via the LASSO-O workflow that will be presented in Part 3

  • Consists of a subset of values used to calculate the skill scores

  • Three file variations
    • sgplassomod = “ingested” wrfout data on original time 10-min. interval; diagnostic variables
    • sgplassodiagobsmod = adds time reduction to hourly time sampling & side-by-side with observations
    • sgplassodiagobsmodz = height-dependent cloud fractions, model+observations, 10-min. interval

  • Much easier to download confobsmod file if you do not need detailed raw output

https://www.arm.gov/capabilities/modeling/lasso

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LASSO Bundle Browser: Upper half (A, B, D)

A. Select date(s), Model config, Measurement 🡪

B. Static plots for selected date summarizing model behavior

    • Heat maps, Skill score plots for all simulations and variables, GOES vis satellite loop

D. Interactive plots showing results for selected Measurement and choices in (C)

    • Clockwise: Taylor diagram, Plot of Taylor score vs. Relative Mean, Regression, Time series

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Taylor diagram

Taylor score vs. Relative Mean

Time series

Regression

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LASSO Bundle Browser: Lower half (C, E)

C. Slide rulers to choose the range of net skill scores that are displayed in (D) and (E)

    • Measurement Skill, 1D Cloud Skill, 2D Cloud Skill, Total Cloud Skill

E. Tabulated results are given for the selections from (A) and (C)

    • Save table values
    • Summary of the simulation run configuration
    • Diagnostic plots per simulation: Time series, Taylor diagram, Regression, 2D Cloud Mask, Soundings
    • Ordering data

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C

Config Obs Model Tar

Raw Model Tar

High-freq Obs Tar

Use GLOBUS for file transfer whenever possible to avoid corruption of downloaded files (e.g., via ftp).

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Where to find more information

  • High-level description and primary citation: BAMS article
  • Nitty gritty details: LASSO Technical Description
  • Web page: https://www.arm.gov/capabilities/modeling/lasso
  • Technical support
    • lasso@arm.gov (goes to Andy and Bill)
      • Works for any sort of question
      • Best for reporting something broken
      • Not publicly searchable
    • LASSO Discussion Forum on new ARM Discourse website: https://discourse.adc.arm.gov/
      • Encouraging folks to use this for general questions and discussion
      • Content will build over time and become a community asset
  • LASSO email list: http://us11.campaign-archive1.com/home/?u=74cd5b8a5435b8eca383fc18c&id=38f02e1568

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Additional Slides�LASSO-CACTI

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Soil initial conditions for LASSO-CACTI

  • Soil initialized with WRF-Hydro to establish a spun-up soil state consistent with WRF physics
    • Continuous WRF-Hydro run from August 2018 to April 2019 using Δx=2.5 km
    • Driven by ERA5

https://www.arm.gov/capabilities/modeling/lasso

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Soil temperatures are similar between ERA5 and WRF-Hydro

Soil comparison for 26-Oct-2018 0 UTC:

ERA5

WRF-Hydro

Topmost Soil Layer Temperature [K]

Soil moisture has stronger gradient in ERA5 versus WRF-Hydro

Topmost Soil Layer Moisture [m3/m3]

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Grid spacing choice for deep convection

  • ∆x ~ 250 m is a threshold for cloud behavior
    • > 250 m is more plume-like
    • < 250 m is more bubble-like
  • Too coarse and updrafts are not mixed sufficiently, making them more like hoses to the free troposphere

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Winds for Different Grid Spacing

2 km

1 km

500 m

250 m

100 m

66.7 m

33.3 m

Lebo & Morrison (2015)

Color = w

Contour = u

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Model output strategy

  • Mesoscale ensembles have 33 members (20 dates), LES have several per case (9 dates)
  • Total dataset for the scenario ~2 PB

https://www.arm.gov/capabilities/modeling/lasso

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Category

Domain(s)

Δx

Frequency

Period

Purpose

Meso

D01,

D02

7.5 km,

2.5 km

15 min.

0–24 UTC

Full model state and diagnostics

Bridge

D03

500 m

15 min.

6–24 UTC

Full model state and diagnostics

LES

D04

100 m

5 min.

12–24 UTC

Full model state and diagnostics

Restart

D03 and D04

30 min.

Enable users to do restarts

WRF Model Data

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We want to make it as easy as possible for users,� but…

  • Using these runs will be non-trivial due to the data size!
  • Raw output sizes
    • Mesoscale ensemble for D02
      • ~325 GB per ensemble member
      • >100 TB for full set of cases and members
    • LES runs for D04
      • Raw output >35 TB per run
      • >1 PB raw model output for 10 cases & 2 LES/case
    • Subsets add to above sizes

https://www.arm.gov/capabilities/modeling/lasso

49

20 May 2023

Δx =

D01

7.5 km

D02

2.5 km

D03

500 m

D04

100 m

Nx

130

258

750

2145

Ny

136

306

865

2775

Snapshot Size

0.6 GB

2.8 GB

19 GB

171 GB

Rough File Sizes for Each Domain

50 of 50

Subsets generated in post-processing

  • Goal of reducing file sizes for users not needing whole raw files
  • Extra diagnostics provided, e.g., LWP, CAPE, destaggered winds, heights, pressure
  • Variable subsets grouped by theme in separate files*:

https://www.arm.gov/capabilities/modeling/lasso

50

20 May 2023

    • Static data, constant in time like terrain height, 0.1 GB
    • Meteorological state, 28 GB (with staggered variables interpolated to cell centers)
    • Meteorological state for staggered variables, 8 GB
    • Cloud data, 2 GB
    • Surface data, 0.4 GB
    • Boundary layer data, 5 GB
    • Radiation data, 0.2 GB
    • Aerosol data, 4 GB
    • Tendency data, 10 GB (e.g., microphysics tendencies & process rates)
    • Tracer data, 8 GB
  • Subsets available on different height coordinates
    • Height above ground level
    • Height above sea level
    • Pressure levels
    • Raw model levels

* File sizes given are per output time for a typical D04 subset file on raw model levels. Note that a wrfout_d04 is 171 GB.