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Anticipating Geostationary High Spectral Resolution Infrared - - PowerPoint PPT Presentation

Anticipating Geostationary High Spectral Resolution Infrared Measurements Paul Menzel UW/CIMSS Contributions from Bob Aune, Liam Gumley, Jun Li, Jinlong Li, Bill Line, Jason Otkin, Ralph Petersen, Hank Revercomb, Tom Rink, Dave Santek, Tim


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Anticipating Geostationary High Spectral Resolution Infrared Measurements

Paul Menzel UW/CIMSS Contributions from Bob Aune, Liam Gumley, Jun Li, Jinlong Li, Bill Line, Jason Otkin, Ralph Petersen, Hank Revercomb, Tom Rink, Dave Santek, Tim Schmit, Bill Smith, Nadia Smith, Gary Wade, Elisabeth Weisz

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Geo Sounding introduced in 1980 with the Visible Infrared Spin Scan Radiometer (VISSR) Atmospheric Sounder (VAS) 12 Infrared Channels (1 Visible Channel) * NOAA sustained continuity of operational imaging services * NASA conducted the VAS Demonstration funded out of the Operational Satellite Improvement Program (OSIP) by implementing Transparent VAS Operations * Venetian blinding enabled the sounding demonstration (1/3 time share with operational imager, cancelled in RISOP)

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Multispectral Probing of the Atmosphere

The first VAS sounding Smith et al 1981

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Nowcasting with VAS

Hourly Total-Totals Index (degree Centigrade) on 20 July 1981 showed locations of subsequent severe convective storms. Thunderstorms (TRW)

  • bserved at 21 GMT are

just beginning to appear at 18 GMT.

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Operational GOES Sounder

  • GOES-I had 18 broad

spectral bands

  • Transition to FTS

sounder (GHIS) was to

  • ccur in GOES-L
  • Seeking balance of

horizontal, vertical, and temporal resolutions

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GOES-12 Sounder – Brightness Temperatures (Radiances) – 12 bands

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Hourly coverage from two GOES- Sounders * radiances 4 to 15 um * clear sky temperature and moisture profiles * cloud amount and height * motion from moisture and cloud features Raob coverage 2x/day * all weather temperature and moisture profiles * wind profiles along ascent path

GOES sounders provide regional coverage every hour

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GOES Sounder derived T(p) & Q(p) in 3-4 km layers

co-located GOES & balloon temperature & moisture soundings: GOES (black) smoothes the atmospheric profile compared to radiosonde (red)

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Improving Depiction and Real-time Providing Predictions

  • f Moisture Processes using Geo-Sounder
  • Short-Range Precipitation skill remains poor

in the warm months

  • Monitoring Moisture is critical,

Predicting Moisture flux is even more important

  • Need to use both moisture and winds from IRS
  • Ideally, all IRS observations should be assimilated at full resolution (both spectrally,

spatially and temporally) into storm-scale mesoscale NWP models. This, however, is likely to be very expensive to accomplish, is decades away from completion and may be difficult to do in all member States.

  • Alternatives tools, developed for GOES and SEVIRI, can be enhanced using IRS

sounding to help fill this information/development gap and provide forecasters with improved guidance tools in real time. Petersen, Aune, Line

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  • A Lagrangian trajectory model that dynamically projects GOES temperature

and moisture observations forward in time out to 9 hours.

  • Built around under-utilized satellite moisture observations
  • Extends the use of GOES moisture data from observations to forecasts and

preserves the GOES data at full resolution without smoothing.

  • Provides information about the moisture and stability structure of the pre-

convective environment 1-9 hours in advance

  • This helps us to make predictions about where convection is most likely (and

least likely) to occur.

  • Long time step (10-15 minutes) => quick run times (~minutes) => little

latency.

Equations of motion do not include the highly non-linear advection terms.

  • Model updates whenever data becomes available (every hour).
  • Analyzes and forecasts the moisture and stability even after clouds form

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Filling the information Gap: NearCasting Model

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  • Initial severe convection rapidly

developed in E Nebraska around 22z and moved through NW Iowa before dissipating quickly in NC Iowa. 13

  • Second round of non-severe convection

developed in southern Minnesota around 02z and moved through central Wisconsin producing widespread heavy rainfall.

April 09, 2011 - Two Types of Convection

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Evolving the Operational GOES Sounder

* GHIS was cancelled * GIFTS was built, but never launched to be a NASA Sounder Demonstration for NOAA * HES feasibility study for GOES-R was deemed too risky * Simulations show hope for approaching Storm Scale Data Requirements

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Local Forecast and Warnings - Storm Scale Requirements

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Anticipating Geostationary High Spectral Resolution Infrared Measurements

Paul Menzel UW/CIMSS Contributions from Bob Aune, Liam Gumley, Jun Li, Jinlong Li, Bill Line, Jason Otkin, Ralph Petersen, Hank Revercomb, Tom Rink, Dave Santek, Tim Schmit, Bill Smith, Nadia Smith, Elisabeth Weisz

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Jun Li, Jinlong Li, Jason Otkin, and Tim Schmit

Red = extreme instability

True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar

Simulating the Geo-IRS perspective

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True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar 1300 UTC

Extreme instability indicated

OSSE of GEO advanced IR sounder for storm nowcasting

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True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar 1400 UTC

OSSE of GEO advanced IR sounder for storm nowcasting

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True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar 1500 UTC

OSSE of GEO advanced IR sounder for storm nowcasting

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True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar 1600 UTC

OSSE of GEO advanced IR sounder for storm nowcasting

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True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar 1700 UTC Start to see extreme instability 4 hours later

OSSE of GEO advanced IR sounder for storm nowcasting

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True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar 1800 UTC Extreme instability clearly shown 5 hours later

OSSE of GEO advanced IR sounder for storm nowcasting

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True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar 1900 UTC

OSSE of GEO advanced IR sounder for storm nowcasting

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True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar 2000 UTC

OSSE of GEO advanced IR sounder for storm nowcasting

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True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar 2100 UTC Rain line shows in radar 8 hours later

OSSE of GEO advanced IR sounder for storm nowcasting

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OSSE of GEO advanced IR sounder for storm nowcasting

Red = extreme instability True GIFTS/HES/IRS ABI/GOES Sounder like Simulated Radar

GIFTS/HES/IRS provides needed instability and warning information hours earlier than current GOES Sounder (+4-5 hrs) and Radar (+8 hrs)

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Nearcasting Severe Weather using a Hyperspectral Environmental Sounder (~IRS)

A WRF model simulation of the June 12, 2002 IHOP case was used to generate simulated radiances from an Advanced Baseline Imager (ABI - left), a geostationary Hyper-spectral Environmental Sounder (HES - right), and simulated radar reflectivity (below). Temperature and moisture profiles were retrieved from the radiance datasets and assimilated by the CIMSS Nearcast Model and compared. HES provided more detailed vertical and horizontal Theta-E gradients.

5-hour NearCast prediction for 2000 UTC Low level Theta-E 5-hour NearCast prediction for 2000 UTC Convective Instability Rapid Development of Convection over Texas and Nebraska began between 2000 and 2100 UTC 12 June 2002

Strong low-level Theta-E gradients are indicated by HES which can better detect low-level moisture.

5-hour NearCast prediction for 2000 UTC Convective Instability 5-hour NearCast prediction for 2000 UTC Low level Theta-E

Simulated composite reflectivity from nature run indication the formation of convection.

Simulated ABI (~SEVIRI) Simulated ABI Simulated HES (~IRS) Simulated HES

Weak gradients of low-level Theta-E are indicated by ABI which has only two water vapor channels.

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Introducing new Commercial Initiative

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Factoring the Improvements from a Geo High Spectral Resolution IR Sounder

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Anticipating Geostationary High Spectral Resolution Infrared Measurements

Paul Menzel UW/CIMSS Contributions from Bob Aune, Liam Gumley, Jun Li, Jinlong Li, Bill Line, Jason Otkin, Ralph Petersen, Hank Revercomb, Tom Rink, Dave Santek, Tim Schmit, Bill Smith, Nadia Smith, Elisabeth Weisz

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CO2 Lines

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H2O Lines

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High resolution IR spectra reveal rotational absorption lines

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calculated versus measured spectra CO2 H2O O3

High resolution IR spectra reveal rotational absorption lines

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Longwave IR Window Region On-line/off-line “signal”

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High resolution IR spectra fix spectral location of measurement Broad band-width uncertainty is alleviated

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“AIRS or IASI-like”

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Longwave IR Window Region

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Longwave IR Window Region

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Longwave IR Window Region

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Longwave IR Window Region

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Longwave IR Window Region

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“Current GOES-like”

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Longwave IR Window Region

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High resolution IR spectra show low level moisture gradients

CrIS VIIRS

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High resolution IR spectra reveal low level inversions

x

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Ability to detect inversions disappears with broadband observations (> 3 cm-1)

45

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Twisted Ribbon Found in CO2 Spectrum

Tropopause inversion causes off-line BTs to be less than on-line BTs Blue between-line Tb warmer for tropospheric channels, colder for stratospheric channels Signature not available at low resolution 15 m CO2 Spectrum strat tropopause trop

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High resolution IR spectra reveal target characteristics

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Moisture Weighting Functions

Pressure (hPa) Pressure (hPa)

Advanced Sounder (2000+) GOES (18)

1000 1000 100 100

UW/CIMSS

High spectral resolution IR advanced sounder will have more and better defined weighting functions compared to current GOES sounder. Retrievals will have better vertical resolution.

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High resolution IR spectra reveal vertical moisture profiles

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Cloud top pressures indicated where clear and cloudy spectra separate

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Suomi NPP/JPSS Aqua Metop A & B

Working with time sequences of Leo measurements

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21:29 UTC 23:19 UTC 23:47 UTC

IASI, CrIS and AIRS (01 Nov 2012)

Weather Forecast Applications – Viewing Time Changes From Sequential Overpasses

Multi-satellite retrievals provide time tendency of atmospheric variables Smith, Weisz, and Smith

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Specific humidity retrievals. All winds (blue); Quality controlled winds(yellow)

AIRS and ATMS H2O Retrieved Winds at 400hPa

AIRS 20 July 2012 0505 UTC ATMS 20 July 2012 0551 UTC

Consecutive Water Vapor Soundings Provide Altitude Resolved Atmospheric Motion Vectors Santek

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Metop A – Metop B (global 48 min tendencies)

500 hPa T and LI Example (10 March 2013 over USA)

IASI-A minus IASI-B Lifted Index [°C/hr]

  • 4
  • 2

2 4

Metop-A minus Metop-B IASI Can Provide Pre-convection Stability Tendencies

Stability Decrease Stability Increase Slight Warming

[K/hr]

IASI-A minus IASI-B Temp Change [K/hr] IASI-A minus IASI-B LI Change [K/hr]

Smith, Weisz, and Smith

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Anticipating Geostationary High Spectral Resolution Infrared Measurements

IRS should provide data and products with radiometric (0.2 K), horizontal (4 km), vertical (1-2 km), and temporal (30-60 min) resolutions in appropriate proportions for the first time ever – the opportunities for improved nowcasting appear to be many and significant

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Viewing AIRS, IASI, and CrIS data with HYDRA

Rink, Gumley, Menzel

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HYperspectral viewer for Development of Research Applications – HYDRA2

VIIRS, CrIS, ATMS MODIS, AIRS, IASI

Developed at CIMSS by Tom Rink With programming support from Tommy Jasmin, Ghansham Sangar (ISRO) With guidance from Liam Gumley Kathy Strabala Paul Menzel Freely available gui-driven software For researchers and educators Computer platform independent Extendable to more sensors and applications On-going development effort Uses the Java-NetCDF library (from Unidata) for accessing HDF5/4, NetCDF4/3 local product files. Interactive, high-performance 2D/3D animations derived from SSEC VisAD api 59

ftp://ftp.ssec.wisc.edu/rink/HYDRA2