DIFAX Maps / Upper Air Charts

Slides:



Advertisements
Similar presentations
Atmospheric Forces Wind Relationships.
Advertisements

Constant Pressure Analysis Chart
What Makes the Wind Blow?
Meteo 3: Chapter 7 Analyzing weather above Earth’s surface Read: pp (ignore confluence)
SO441 Synoptic Meteorology
Chapter 6 Section 6.4 Goals: Look at vertical distribution of geostrophic wind. Identify thermal advection, and backing and veering winds. Look at an example.
UPPER AIR DYNAMICS (continued) MSC 243 Lecture #8, 10/22/09.
The 500mb Chart and Shortwave vs. Longwave Troughs.
ATS/ESS 452: Synoptic Meteorology
Introduction to Upper Air Data
Jet stream. Jet stream and other upper air winds Jet stream formation Jet stream position Why the jet stream is important –Cyclones.
MET 61 1 MET 61 Introduction to Meteorology MET 61 Introduction to Meteorology - Lecture 10 Atmospheric Dynamics Dr. Eugene Cordero Ahrens: Chapter 9 W&H:
MAPH40410 Synoptic Meteorology Meteorology M.Sc. Peter Lynch Meteorology & Climate Centre School of Mathematical Sciences University College Dublin.
Jet Streams.
AOS 100: Weather and Climate Instructor: Nick Bassill Class TA: Courtney Obergfell.
ATMO 251 Special Thanks to Dr. Russ Schumacher who originally developed these slides for a guest lecture. Fronts and Frontogenesis.
Lessons 22,23,24 Upper Level Winds
Upper Air. Using just the surface is like diagnosing a sick person using only an examination of the soles of the feet.
How do the blizzards from?. Review of last lecture Tropical climate: Mean state: The two basic regions of SST? Which region has stronger rainfall? What.
General Circulation & Thermal Wind
ATS/ESS 452: Synoptic Meteorology
DIFAX Maps DIFAX maps are weather maps generated by the National Weather Service. Before the Internet or AWIPS, these were the basic weather analysis and.
ATS/ESS 452: Synoptic Meteorology Friday 09/26/2014 Continue Review Material Geopotential Thickness Thermal Wind.
Upper Air Charts By Tom Collow November 8, Reading Upper Air Charts Temperature (°C) Dewpoint Depression (°C) Height Wind direction and speed (knots)
DIFAX Maps Weather maps generated by the NWS Before the Internet or AWIPS, these were the basic weather analysis and forecast charts used by meteorologists.
Section 02 Lesson 5/6/7 Atmospheric Pressure, Temperature and Density
ADVENTURE IN SYNOPTIC DYNAMICS HISTORY
What set the atmosphere in motion?. Review of last lecture Thickness of the atmosphere: less than 2% of Earth’s thickness Thickness of the atmosphere:
Thickness and Thermal Wind /aos101/wk12.html /aos101/wk12.html.
1 IPV and the Dynamic Tropopause John W. Nielsen-Gammon Texas A&M University
ATS/ESS 452: Synoptic Meteorology
Jet Stream. 250 mb isotach Main Upper Tropospheric Jets Closely Associated with the Tropopause.
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.
COMET Feb. 20, 2002 IPV and the Dynamic Tropopause John W. Nielsen-Gammon1 Outline PV basics Seeing the world through PV Waves and vortices Nonconservation.
ATS/ESS 452: Synoptic Meteorology
METR February Why use Temp. Advection? The temperature at a location may change in two ways: –The air parcel which is being sampled might.
Dynamic tropopause analysis; What is the dynamic tropopause?
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.
Surface 850 mb 700 mb 500 mb 300 mb NEMOC Training Department Chart Format.
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.
Vertical Cyclone Structure AOS Section 302 Ross A. Lazear May 1, 2007.
Air Masses. Definition Large body of air having similar temperature and moisture Air masses extend several miles up and cover lots of “ground” There can.
ATS/ESS 452: Synoptic Meteorology Friday 08 January 2016 Review Material Overview of Maps Equations of Motion Advection Continuity.
Potential vorticity and the invertibility principle (pp ) To a first approximation, the atmospheric structure may be regarded as a superposition.
Upper Air Charts Before the Internet or AWIPS, DIFAX maps were the basic weather analysis and forecast charts used by meteorologists They were only available.
Class #17 Monday, February 16, Class #17: Monday, February 16 Surface pressure and winds Vertical motions Jet streams aloft.
ThermodynamicsM. D. Eastin We need to understand the environment around a moist air parcel in order to determine whether it will rise or sink through the.
PV Thinking and the Dynamic Tropopause
Part I Maps and Numbers.  Station Models  Isoline Maps.
The Course of Synoptic Meteorology
SO441 Synoptic Meteorology
Principles of weather forecasting
Upper Air Analysis 850, 700, 500, 250 hPa charts.
MID-LATITUDE WEATHER SYSTEMS: PART IV: SURFACE-UPPER AIR LINKAGE
Meteorological charts
ATS/ESS 452: Synoptic Meteorology
Jets Dynamics Weather Systems – Fall 2017
Constant Pressure Maps
Surface Weather Map a.k.a: Surface Synoptic Chart.
A jet stream (or jet) is a narrow current of strong winds.
Climate Factors.
Upper air Meteorological charts
The Course of Meteorological Instrumentation and Observations
Jet Stream.
A jet stream (or jet) is a narrow current of strong winds.
The Course of Synoptic Meteorology
Surface Weather Map a.k.a: Surface Synoptic Chart.
Robert Fovell Meteorology – Lecture 16 Robert Fovell
Representing Climate Data
The Course of Synoptic Meteorology
Presentation transcript:

DIFAX Maps / Upper Air Charts Weather maps generated by the NWS Before the Internet or AWIPS, these were the basic weather analysis and forecast charts used by meteorologists They were only available through a fax machine connected to a dedicated landline

DIFAX maps are gradually being phased out; however, the most important ones are still produced These maps are unique and contain information which is priceless for operational meteorologists All meteorology students benefit from knowledge of these maps and their interpretation If you understand how to interpret the black&white DIFAX chart, you should have no problem interpreting pretty colored charts from other sources

DIFAX Map Access National Weather Service: http://weather.noaa.gov/fax/nwsfax.html Colorado State Archive: http://ldm.atmos.colostate.edu/ SUNY Albany: http://www.atmos.albany.edu/weather/difax.html

Surface Charts Analyzed charts issued every 3 hours (00Z – 21 Z) Data includes Hourly synoptic stations Ship reports Buoy reports Maps can be found from the HPC: http://www.hpc.ncep.noaa.gov/html/sfc2.shtml

Surface Charts Isobar analysis: Frontal Analysis 4 mb increments labeled with tens and units digits Lows and Highs labeled with L and H with the pressure value labeled nearby (in whole mb) Frontal Analysis http://www.hpc.ncep.noaa.gov/html/fntcodes2.shtml Used for current depiction of surface weather features (most valuable weather chart)

Today’s Sfc Chart (23 Sept 2014)

Upper Air Analysis Generated every 12 hours with 00Z and 12Z data Produced from the NAM Model analysis The NAM Model uses a first guess from the previous model run 6 or 12 hours earlier as a basis for constructing the analysis fields Data is incorporated into the first guess field and the analysis is created via Optimal Interpolation (OI) or 4-D Data Assimilation Actual data is plotted on the chart, but may not agree with chart’s analysis field

850 mb Chart Isoheights (solid contours) Isotherms (dashed contours) 30 m intervals with 1500 m (150 decameters) reference line contour labels in decameters plotted heights are in meters (generally add 1 in thousands digit) Isotherms (dashed contours) 5oC intervals with 0oC reference line

850 mb Chart Uses: Caution: Low Level Jets Lower tropospheric temperature advection and thermal profile (thermal ridges and troughs) Lower tropospheric moisture advection and profiles (moist and dry tongues) Height changes Caution: Sometimes underground near high terrain

Today’s 850mb Chart (23 Sept 2014)

700 mb Chart Isoheights (solid contours) Isotherms (dashed contours) 30 m intervals with 3000 m (300 decameters) reference line contour labels in decameters plotted heights are in meters (generally add 2 or 3 in thousands digit) Isotherms (dashed contours) 5oC intervals with 0oC reference line

700 mb Chart Uses: Caution: Elevated tropospheric moisture advection and profiles (elevated dry intrusions; moist tongues) Mid-tropospheric temperature advection and thermal profile (thermal ridges and troughs) Mid-level jets Height changes Caution: Sometimes near surface in higher terrain

Today’s 700mb Chart (23 Sept 2014)

500 mb Chart (North America) Isoheights (solid contours) 60 m intervals with 5400 m (540 decameters) reference line Contour labels in decameters Plotted heights are in decameters Isotherms (dashed contours) 5C intervals with 0C reference line

500 mb Chart (North America) Uses: Mid-tropospheric temperature advection and thermal profile Mid-tropospheric moisture profile Wave pattern in the westerlies ID of longwaves and shortwaves LND and approximate steering level for surface synoptic systems Height changes and wave motion Vertical and horizontal tilt of waves

Today’s 500mb Chart (23 Sept 2014)

500 mb Chart (Hemispheric) Contains same contours as the 500 mb North American analysis, except void of data plots Additional Uses: Circumpolar vortex Planetary wave number and pattern Wave ID

Today’s 500mb Hemis (23 Sept 2014)

300 mb Chart Isoheights (solid contours) 120 m intervals with 9000 m (900 decameter) reference line Contour labels in decameters Plotted heights in decameters Isotachs (light dashed contours) 20 knot intervals with 10 knot reference line Stippled regions represent: 70-110 knot winds 150-190 knot winds

300 mb Chart Uses: Polar jet stream location/configuration/intensity 4-quadrant jet/divergence relationship Upper tropospheric wave pattern Regions of difluence and confluence Regions of upper-tropospheric vertical shear

Today’s 300mb Chart (23 Sept 2014)

250 mb Analysis Isoheights (solid contours) 120 m intervals with 10,000 m (1000 decameter) reference line contour labels in decameters plotted heights are in decameters (add 0 in ones digit for meters, and possibly a 1 for the ten-thousands digit [if first plotted number is a 0]) Isotherms (dashed heavy contours) 5oC intervals with -50oC reference line

200/250 mb Analysis Isotachs (light dashed contours) 20 knot intervals with a 10 knot reference line Stippled regions represent: 70-110 knot winds 150-190 knot winds

200/250 mb Analysis Uses: Sub-tropical jet stream location/configuration/intensity the 4-quadrant jet/divergence relationship Upper-tropospheric wave pattern Regions of Difluence and Confluence (convection/severe weather) Regions of upper-tropospheric vertical shear (tropical cyclones) Tropopause folds and breaks

Today’s 200mb Chart (23 Sept 2014)

1000-500 Thickness / MSLP Chart Thickness Values (usually dashed contours) Vertical distance in m between 1000mb and 500mb pressure levels Function of avg virtual temperature of 1000mb to 500mb layer Increments of 60 gpm MSLP (solid black contour)

1000-500 Thickness / MSLP Chart Uses Temperature advection Thickness is proportionally to temperature Use MSLP contours as proxy for wind (assume geostrophic 5400 (540) line generally divides polar air from mid-latitude air (first guess for the rain-snow line)