Inferring Mesoscale Information From Synoptic Scale NWP Guidance Interactions of Synoptic Scale features can create Responses on the Mesoscale 0 1 5 6.

Slides:



Advertisements
Similar presentations
February 19, 2004 Texas Dryline/Dust Storm Event.
Advertisements

How to “Grow” a Storm Temperature advection is key!
Stratus. Outline  Formation –Moisture trapped under inversion –Contact layer heating of fog –Fog induced stratus –Lake effect stratus/strato cu  Dissipation.
Atmospheric Destabilization Processes Upper Level Mixed Layer Synoptic Lifting Dynamic Destabilization Differential Advection.
Orographic Storms in the Southern Europe Heavy precipitating storms resulting from proximity to Mediterranean Sea Fall season particularly dangerous because.
Seeder-Feeder Mechanism When topography is too shallow to force a pure orographic cloud, a seeder-feeder mechanism may operate: –Ice crystals produced.
Midlatitude Cyclones Equator-to-pole temperature gradient tilts pressure surfaces and produces westerly jets in midlatitudes Waves in the jet induce divergence.
Analysis of Rare Northeast Flow Events By Joshua Beilman and Stephanie Acito.
Thunderstorm Ingredients ©Oklahoma Climatological Survey EarthStorm 2009.
Thunderstorms.
#4095. How much colder than standard temperature is the actual temperature at 9,000 feet, as indicated in the excerpt from the Winds and Temperature Aloft.
Stability and Severe Storms AOS 101 Discussion Sections 302 and 303.
Stability & Movement Figure 7.1 A rock, like a parcel of air, that is in stable equilibrium will return to its original position when pushed. If the rock.
Characteristics of Isolated Convective Storms
The Well Mixed Boundary Layer as Part of the Great Plains Severe Storms Environment Jonathan Garner Storm Prediction Center.
Introduction to Upper Air Data
Kari Murray.  This article is extending on a 10-year climatological study done by Rose et al.  Rose et al. found that tornadoes most commonly occur.
More Thunderstorms. Today Homework in Wind shear More multicellular storms.
A brief synopsis of Johnson and Mapes: Mesoscale Processes and Severe Convective Weather From Severe Convective Storms sections 3.3b, 3.3c.1, 3.4 By Matt.
Chapter 3 Mesoscale Processes and Severe Convective Weather Meteorology 515/815 San Francisco State University Spring 2006 Christopher Meherin.
Stability & Skew-T Diagrams
Mesoscale Processes and Severe Convective Weather Richard H. Johnson and Brian E. Mapes Presentation by Chris Medjber Severe Convective Storms, Meteorological.
Convective Weather Thunderstorms Lightning Tornadoes… …and more.
An Examination of the Tropical System – Induced Flooding in Central New York and Northeast Pennsylvania in 2004.
. Severe Weather Indices Variables used to ‘summarize’ the potential for Severe Weather formation Evolved over past 60 years Based on long history of severe.
Deep Convection A review of processes “Everything we hear is an opinion, not a fact. Everything we see is a perspective, not truth” Marcus Aurelius: AD
Characteristics of Isolated Convective Storms Meteorology 515/815 Spring 2006 Christopher Meherin.
Determining Favorable Days for Summertime Severe Convection in the Deep South Chad Entremont NWS Jackson, MS.
Severe Weather Soundings and Wind Shear Environments.
How to get the most from the Internet briefings NWS Boise, Id.
General Circulation & Thermal Wind
Things to look for on the weather maps Visible and IR satellite images (& radar too): Look at cloud movements and locations - do they correlate with what.
The Ageostrophic Wind Equation Remember from before: – The “forcing” terms in the QG omega equation are geostrophic – “Weather” results from ageostrophic.
II. Synoptic Atmospheric Destabilization Processes Elevated Mixed Layer (EML) Synoptic Lifting Dynamic Destabilization Differential Advection.
Lapse Rates and Stability of the Atmosphere
1 Lake-Effect Snow (LES). 2 Overview of the Lake-Effect Process n Occurs to the lee of the Great Lakes during the cool season n Polar/arctic air travels.
Formation of the Extratropical Cyclone (Cyclogenesis)
Tropical Meteorology I Weather Center Event #4 Tropical Meteorology What is Tropical Meteorology? – The study of cyclones that occur in the tropics.
Atmospheric Stability & Instability
Unit 4 – Atmospheric Processes. Necessary Atmospheric Conditions 1. Water vapour must be available in the lower atmosphere to feed clouds and precipitation.
Cumulus Clouds. What goes on inside a cumulus cloud?
Lecture 2a Severe Thunderstorm Primer Synoptic Laboratory II – Mesoscale Professor Tripoli.
Lecture 11 (11/18) Winter Storms and Lake Effect Snow.
Nature of Storms Chapter 13.
Soundings and Adiabatic Diagrams for Severe Weather Prediction and Analysis Continued.
METR March Review Hydrostatic balance Ideal gas law p = ρ R d T v, ρ = p / R d T v Take layer average virtual temperature, R and g as constants.
ATS/ESS 452: Synoptic Meteorology
Key Terms and Concepts ELR--Environmental Lapse Rate 5°C-6.5°C/1000 m – temperature of the STILL air as you ascend through the troposphere. ALR--Adiabatic.
Soundings and Adiabatic Diagrams for Severe Weather Prediction and Analysis.
Tropical Severe Local Storms Nicole Hartford. How do thunderstorms form?  Thunderstorms result from moist warm air that rises due to being less dense.
Jets Dynamics Weather Systems – Fall 2015 Outline: a.Why, when and where? b.What is a jet streak? c.Ageostrophic flow associated with jet streaks.
Principles of Convection. BACKGROUND When vertical shear is weak, the main influence on convective updrafts & downdrafts is bouyancy. As the vertical.
Forecasted 700 hPa Low (Blizzard of 2006) The RUC was saying “watch out.” This model is becoming a great short range model for East coast snowstorms (courtesy.
Frontogenesis Frontogenesis: The generation of intensity of a front Warm air merged onto colder air Temperature gradient amplified at least one order of.
Conditions for Convection The Ingredients Method.
UNIT 1: Weather Dynamics Chapter 1: Inquiring about Weather The Causes of Weather Chapter 2: Weather Forecasting.
Anatomy of a windy day. What keeps a cyclone or anticyclone going? Jet Streams Global Rivers of Air.
Skew T Log P Diagram AOS 330 LAB 10 Outline Static (local) Stability Review Critical Levels on Thermodynamic Diagram Severe Weather and Thermodynamic.
Weather Basics Air Pressure and Winds. Air Pressure Air has a mass and exerts a force called atmospheric pressure Air pressure is measured in millibars.
Chapter 6 Stability and Cloud Development. Stability & Cloud Development This chapter discusses: 1.Definitions and causes of stable and unstable atmospheric.
Defining a Threat Area and Miller Techniques
SO254 Extratropical cyclones
Common Severe Weather Weather Soundings
Characteristics of Isolated Convective Storms
AOS 101 Severe Weather April 1/3.
Atmospheric Destabilization Processes
Thunderstorms and Severe Weather Part I
Thermodynamic Diagrams and Severe Weather
Stability and Cloud Development
Presentation transcript:

Inferring Mesoscale Information From Synoptic Scale NWP Guidance Interactions of Synoptic Scale features can create Responses on the Mesoscale hours

What are we looking for? 1 – An environment that is already conducive to (will support) thunderstorm growth Remember, Convective Parameterizations do NOT predict realistic convection patterns

What are we looking for? 1 – An environment that is already conducive to (will support) thunderstorm growth Classic Severe Thunderstorm Sounding

What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future Need to develop (for thunderstorms): a)Abundant low level moisture b)A capping inversion (to prevent convection from forming too early) c)Dry air at middle levels d)Diurnal heating e)Development of Low-level lift f)Development of Upper-level divergence g)For heavy precipitation - add a continuous supply of additional low-level moisture h)For strong winds – a continuous supply of mid-level dryness

The US NWS has developed ‘check lists’ for use in various parts of the country

How do we find What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Does the NWP guidance already have the signatures that we need? Look at model soundings and their evolution, but... Remember that if the Convective Parameterization in the model has been triggered the atmospheric stability was becoming too weak, the model will 1)stabilize and 2) moisten the sounding. Check to see if the model is producing convective precipitation

Model Soundings show important information in addition to Temperature, Moisture and Wind Profiles, including surface and multi-level stability parameters (In severe weather situations, Model Soundings will typically underestimate strengths of inversions (temp and moisture), wind shears (vertical and horizontal),...

What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future (even if the models don’t depict correct it at small enough scales) Need to develop (for thunderstorms): a)Abundant low level moisture (Model may make area of moisture too wide and moist high enough)

Display of low-level moisture (mixing ratio, g/kg), winds and surface topography, with high amounts of moisture highlighted. Plot done for 850 hPa layer of model – good for mean moisture in low levels

Display of low-level moisture (mixing ratio, g/kg), winds and surface topography, with high amounts of moisture highlighted. Plot done for bottom-most 30-hPa deep layer of model to capture near-surface moisture sources - good in areas affected by sloping terrain

What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future Need to develop (for thunderstorms): a)Abundant low level moisture Another measure of the total thermal energy in Equivalent Potential Temperature  E which combines: the temperature of a parcel of air and the total latent heat present in the parcel

Display of low-level Equivalent Potential Temperature (C), winds and surface topography, with high  E highlighted. Plot done for bottom-most 30-hPa deep layer of model to capture near-surface moisture sources - good in areas affected by sloping terrain

What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future Need to develop (for thunderstorms): a)Abundant low level moisture b)A capping inversion (to prevent convection from forming too early) (Model will probably underestimate strength of both temperature and moisture inversions) Diagnosed either from model sounding at a point Or By looking at the difference in Temperature from 850 to 700 (or 600) hPa Or By looking at the difference in Potential Temperature from 850 to 700 (or 600) hPa

Display of Temperature difference between 850 and 700 hPa Lower values indicate more stable Lapse Rates, since temperature normally decreases with height

Display of Potential Temperature difference between 850 and 700 hPa Lower values indicate more stable Lapse Rates, since potential temperature always increases with height

What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future Need to develop (for thunderstorms): a)Abundant low level moisture b)A capping inversion (to prevent convection from forming too early) c)Dry/cold air at middle levels + High tropopause (Model may underestimate extreme dry values and smooth out horizontal gradients)

Display of Tropopause Pressure (hPa) Lower values indicate potential for deeper storm growth

Display of 600 hPa mixing ratio (green, g/kg), Winds (blue) and Mixing Ratio difference between 600 and 850 hPa (<-10 g/kg – dashed white) Lower values indicate greater drying between lower to upper levels

Display of 600 hPa Equivalent Potential Temperature difference between 600 and the layer 30 hPa above the ground (C) Larger values (highlighted) indicate greater drying from lower to upper levels

Vertical circulations ahead and behind a propagating Jet Streak can produce localized upper-level convergence and produce drying by subsidence below the jet level. Contributes both to mid-level drying and warming needed to create ‘capping inversion’

Southern Hemisphere Ideal Jet Parcels entering Jet Streak accelerate and move toward lower heights Parcels leaving Jet Streak decelerate and move toward higher heights

Entrance Region Thermally Direct Circulation Warm air risesCold air sinks

Exit Region Thermally Indirect Circulation Warm air sinks Cold air rises

Vertical circulations ahead and behind a propagating Jet Streak can produce localized upper-level convergence and Subsidence of dry air below the jet level. Contributes both to mid-level drying and ‘capping inversion’ Entrance Region Exit Region J Convergence Divergence

As a Jet Streak moves past a point (X) that was originally below the left exit region, It transitions from a thermally direct regime of upper- level convergence and subsidence of dry air which supports the “capping inversion” or “Lid” to A dynamically forced, thermally indirect regime with upper-level divergence, which forces low-level convergence and lifting of the column of air X X

Convective Available Potential Energy (CAPE) is a measure of parcel buoyancy, while Convective INhabition (CIN) is a measure of “Lid” strength CAPE CIN

What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future Need to develop (for thunderstorms): a)Abundant low level moisture b)A capping inversion (to prevent convection from forming too early) c)Dry air at middle levels d)Diurnal heating (Model may under- or overestimate daily temperature range do to incorrect clouds, soil moisture, vegetation,... )

Display of near surface Temperature difference between 00 and 12 UTC Larger values highlighted Beware – incorrect clouds or precipitation in model can cause surface temperature to be too cool!!!

Display of near surface Temperature difference between 00 and 12 UTC Larger values highlighted Beware – incorrect clouds or precipitation in model can cause surface temperature to be too cool!!!

What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future Need to develop (for thunderstorms): a)Abundant low level moisture b)A capping inversion (to prevent convection from forming too early) c)Dry air at middle levels d)Diurnal heating e)Development of Low-level lift

Development of Low-Level Lifting Here’s where things get interesting Remember, we are NOT ONLY looking for areas where the model has forecast rain, but also Areas where convection is likely to occur

Development of Low-Level Lifting Here’s where things get interesting Options: Model low-level Vertical Motion Can be affected by model precipitation fields – are they correct?

Development of Low-Level Lifting Here’s where things get interesting Options: Model low-level Vertical Motion Can be affected by model precipitation fields – are they correct?

Development of Low-Level Lifting Here’s where things get interesting Options: Model low-level Convergence Can be affected by model precipitation fields – are they correct?

Development of Low-Level Lifting Here’s where things get interesting Options: Model low-level cyclonic circulations/vorticity Not affected as much by model precipitation fields

Development of Low-Level Lifting Here’s where things get interesting Options: Orographic lifting diagnosed from model (upslope) Calculate uplift using low level wind (above friction layer) and surface topography

Development of Low-Level Lifting Here’s where things get interesting Options: Model low-level Vertical Motion Small-scale cyclonic circulations and short waves Orographic lifting diagnosed from model (upslope) In bands head of and parallel to cold fronts Right-exit or left-entrance region of jet streak Along outflow boundaries of previous convection Along “sea breeze” fronts (likely to extend MUCH too far inland) Water / Land Wet Soil / Dry Soil In afternoon between areas that had been cloudy (foggy) and clear in morning Gravity Waves,... Jet Streak Entrance Region Jet Streak Exit Region

What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future Need to develop (for thunderstorms): a)Abundant low level moisture b)A capping inversion (to prevent convection from forming too early) c)Dry air at middle levels d)Diurnal heating e)Development of Low-level lift f)Development of Upper-level divergence (Model may underestimate wind maxima, wind shears (especially on equator-ward (left) side of jet), ageostropic circulations,...)

Vertical circulations ahead and behind a propagating Jet Streak can produce localized upper-level convergence and Subsidence of dry air below the jet level. Contributes both to mid-level drying and ‘capping inversion’ Entrance Region Exit Region J Convergence Divergence

What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future Need to develop (for thunderstorms): a)Abundant low level moisture b)A capping inversion (to prevent convection from forming too early) c)Dry air at middle levels d)Diurnal heating e)Development of Low-level lift f)Development of Upper-level divergence g)For heavy precipitation - add a continuous supply of additional low-level moisture

What are we looking for? For heavy precipitation - add a continuous supply of additional low-level moisture Combine low-level mixing ratio and wind field

What are we looking for? For heavy precipitation - add a continuous supply of additional low-level moisture Combine low-level mixing ratio and wind field to determine Moisture Flux

What are we looking for? For heavy precipitation - add a continuous supply of additional low-level moisture Combine low-level mixing ratio and wind field to determine Moisture Flux and Moisture Flux Convergence (at small scale)

What are we looking for? 1 – Environments that are already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future Need to develop (for thunderstorms): a)Abundant low level moisture b)A capping inversion (to prevent convection from forming too early) c)Dry air at middle levels d)Diurnal heating e)Development of Low-level lift f)Development of Upper-level divergence g)For heavy precipitation - add a continuous supply of additional low-level moisture h)For strong winds – add a continuous supply of mid-level dryness

What are we looking for? For strong winds – add a continuous supply of mid-level dryness Combine mid-level mixing ratio and wind field to determine moisture (dryness) advection

Summary of factors for diagnosing Severe Storms Surface Hourly surface mesoscale analysis is critical in severe forecasting and necessary to monitor model accuracy. Detailed analysis can uncover features such as boundaries, mesolows, bubble highs, strong pressure falls, and moisture pooling. Optimal surface features for severe weather include: · Dew Points 18°C · Theta E ridge and positive Theta-E advection · Low-level moisture flux convergence · Thermal ridge over or west of the moisture axis · Areas experiencing strong temperature and dew point rises · Rapidly developing cumulus congestus within areas · Areas reaching convective temperature · Focusing mechanisms (fronts, troughs, gust fronts, dry lines, outflow boundaries, etc.) · Surface pressure 1005 mb · Areas with concentrated pressure falls of 5 mb over 12 hours.

Aloft Forecasters should start with a 4-dimensional mental picture of the atmosphere (Doswell, 1982). Upper air and surface maps can and should be enhanced to emphasize features of importance to convective storm forecasting (Maddox, 1979b). Optimum upper air features for severe weather include: mb (near surface) · Areas under and just west of the low level jet (winds 25 kts) · Thermal ridge west of moisture axis · Significant warm air advection · Strong moisture flux convergence · Focusing mechanisms (fronts, troughs, and dry lines) mb (above surface) · Areas under and just west of the low level jet (winds 35 kts) or on the nose of the jet · Thermal ridge west of moisture axis · Dew Point 8°C · Significant warm air advection · The greater the angle of the winds from dry to moist air, the greater the instability. · Strong moisture flux convergence · Focusing mechanisms (fronts and troughs) · Moisture transport axis

Aloft Forecasters should start with a 4-dimensional mental picture of the atmosphere (Doswell, 1982). Upper air and surface maps can and should be enhanced to emphasize features of importance to convective storm forecasting (Maddox, 1979b). Optimum upper air features for severe weather include: mb · Wind veering 30 degrees between surface and 700 mb · Dry air intrudes at a 40 degree angle and speeds of at least 25 knots. Look at Skew- T’s, model soundings, and gridded data for significant entrainment. · Dew point depression > 6°C. Significant dry air in mid levels may signal possibility of strong downdrafts. · Winds cross 12 hr temperature no change line at > 40 degrees · Focusing mechanisms (fronts and troughs) · Significant upward vertical velocity (UVV) mb · Wind speeds of 50 knots · Short Waves, especially negatively tilted rapidly moving short waves · Cyclonic Vorticity Advection with contours crossing vorticity pattern > 30 degrees · Significant cold pool aloft (-16oC June-Aug; -14°C Sept-Oct and Apr-May; -12 °C Nov- Dec; -10°C Jan-Mar) – (changed to be applicable to southern hemisphere) · Horizontal shear over 90 miles is 30 kts

Aloft Forecasters should start with a 4-dimensional mental picture of the atmosphere (Doswell, 1982). Upper air and surface maps can and should be enhanced to emphasize features of importance to convective storm forecasting (Maddox, 1979b). Optimum upper air features for severe weather include: and 200 mb (corrected for sougthern hemisphere) · Wind speeds 40 ms -1 (Probably less in sub-tropics) · Diffluent areas · Right exit region and left entrance region of straight jet streaks; right exit region of cyclonically curved jet streak; left entrance region in anticyclonic jet streak · Most severe weather occurs north of the polar jet, and south of the subtropical jet (coupled jet) or in the right exit region of a jet · Severe weather outbreaks often occur in the diffluent zone between the polar and subtropical jet streams · Long wave troughs and strong synoptic scale lift · Significant height falls and or a deepening of an upper level low

FORECASTING LARGE HAIL The four primary forecasting keys for hail are: · Strength of Updraft (CAPE) · Height of freezing level (WBZ) · Environmental wind structure · Remembering that supercells (especially HP supercells) can produce prodigious hail Some operational considerations include the size and distribution of CAPE, using a reasonable lifted parcel, and the environmental lapse rates. Another important factor is the melting of the hailstone as it falls to the surface from the freezing level. Forecasters should look for a cold pool at 500 mb (usually associated with a closed low) as it moves into an area of moderate low level moisture

FORECASTING DAMAGING WINDS The four primary forecasting keys for damaging winds with environments with weak shear are: · Amount of dry mid-level air · Strength of the updraft · Amount of low-level moisture · Downdraft instability. When the environmental shear is weak, the thermodynamic profile is a primary signal for identifying when strong convectively induced winds are likely to occur. Operational forecasters should look for Inverted-V soundings, steep low level Theta-E lapse rates, and the strength of the CAPE. Sometimes high CAPE and weak shear environments can lead to derecho development.

FORECASTING DAMAGING WINDS The four primary forecasting keys for damaging winds of air-masses with moderate to strong shear are: · Amount of low and mid level helicity · Degree of instability · Amount of dry mid level air · Rapid storm motion (> 40 knots) Precipitation loading and negative buoyancy due to evaporative cooling are recognized factors in initiating and sustaining downdrafts. Once a downdraft is established, continued entrainment of unsaturated air in the mid levels aids in evaporation and consequently stronger downdrafts. Storms in moderate to strong shear can turn into supercells, bow echos, and derecho.

Summary of what are we looking for to Inferring Mesoscale Information From Synoptic Scale NWP Guidance 1 – Environments that are already already conducive to (will support) thunderstorm growth Or 2 - Synoptic flow patterns that will produce this kind of environment in the near future Need to develop (for thunderstorms): a)Abundant low level moisture b)A capping inversion (to prevent convection from forming too early) c)Dry air at middle levels d)Diurnal heating e)Development of Low-level lift f)Development of Upper-level divergence g)For heavy precipitation - add a continuous supply of additional low-level moisture h)For strong winds – a continuous supply of mid-level dryness Must use real time data to monitor model performance and to detect a variety of trigger (low level lifting) mechanisms