Introducing HYDRA – a Multispectral Data Analysis Toolkit Course in Costa Rica

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Transcript Introducing HYDRA – a Multispectral Data Analysis Toolkit Course in Costa Rica

Introducing HYDRA – a Multispectral Data Analysis Toolkit

Lectures for the Regional Training Course in Costa Rica 15 March 2005

Paul Menzel NOAA/NESDIS/ORA

Introducing HYDRA – a Multispectral Data Analysis Toolkit

Tom Rink 2 , Tom Whittaker 2 , Kevin Baggett 2 , Paolo Antonelli 2 , Liam Gumley 2 , and W. Paul Menzel 1 1 NOAA Satellite and Information Services / ORA 2 Cooperative Institute for Meteorological Satellite Studies Madison, Wisconsin, 53706 USA

Cooperative Institute for Meteorological Satellite Studies Madison, Wisconsin

Introducing HYDRA – a Multispectral Data Analysis Toolkit What is Hydra How to get it Starting the Hydra analysis toolkit Examples with MODIS data over India

HYperspectral viewer for Development of Research Applications - HYDRA

MSG, GOES MODIS, AIRS

http://www.ssec.wisc.edu/hydra/

HYperspectral viewer for Development of Research Applications HYDRA Freely available software For researchers and educators Computer platform independent Extendable to more sensors and applications Based in VisAD (Visualization for Algorithm Development) Uses Jython (Java implementation of Python) On-going development effort For more information and a copy of the freeware see http://www.ssec.wisc.edu/hydra/.

Hardware Recommendation

Drivers for graphics cards should be as up-to-date as possible, or Hydra may not work properly.

Hydra runs on most machines, but a minimum of 512MB of main memory and a graphics card with 32MB or more helps with performance.

Start executable from DOS Batch file

The Hydra Window

Load MODIS data over Caribbean

Use zoom tool To see details

Use color range adjustment to explore various image enhancements

Opening the Multi-Channel Viewer from the Hydra Window

The Multi-Channel Viewer Window

IRW

Using transect to plot BT along selected path Use transect to display brightness temperatures along indicated path

WV

Opening Linear Combinations

BT11 BT4-BT11 BT4-BT11 BT11

Scatterplot

Use color area boxes in toolbar at bottom of scatter plot to select pixels to be viewed on images

BT4-BT11 BT11 BT4-BT11 BT11 BT11

Use color area boxes in toolbar at bottom of image to select pixels to be viewed on scatter plot

Introducing HYDRA – a Multispectral Data Analysis Toolkit What is Hydra How to get it Starting the Hydra analysis toolkit Examples with MODIS data over India

VIIRS , MODIS , FY-1C , AVHRR O2 CO2 O3 O2 H2O O2 H2O H2O H2O H2O CO2 H2O

MODIS IR Spectral Bands

MODIS

MODIS spectral signatures from land, ocean, and atmosphere

Scatter plot of BT11(right) on x-axis and r0.6 (left) on y-axis

Vis Refl vs IRW Rad

BT8.6-BT11

BT8.6-BT11 as false color image

BT8.6-BT11 BT11 BT11

t = t =

Simulations of Ice and Water Phase Clouds 8.5 - 11

m

m BT Differences

High Ice clouds

• BTD[8.5-11] > 0 over a large range of optical thicknesses t •T cld = 228 K

Midlevel clouds

• BTD[8.5-11] values are similar (

i.e

., negative) for both water and ice clouds •T cld = 253 K

Low-level, warm clouds

• BTD[8.5-11] values always negative •T cld = 273 K

Ice: Cirrus model derived from FIRE-I in-situ data Water: r e =10 Angles

: q o m

m = 45 o ,

q

= 20 o , and

f =

40 o Profile: midlatitude summer ( Nasiri et al, 2002)

Optical properties of cloud particles: imaginary part of refraction index

Imaginary part of refraction index 0.6

Ice 0.5

0.4

0.3

0.2

0.1

Water 0 1 3 5 7 9 wavelength [microns] 11 13 8.6 & 11 um channel differences are used for cloud phase identification [BT8.6 - BT11] > 0 indicates ice cloud 15

Scatter of 2.3 um (right) on y-axis & 8.6-11 um (top middle) on x-axis

Scatter of 2.3 um (right) on y-axis & 8.6-11 um (left) on x-axis

False color of NDVI image from MODIS

NDVI vs BT11

NDVI vs BT11

SSC estimation from r0.55/r0.44

Phytoplankton concentration on left (from r0.55/r0.44) and SST on right (from BT11+{BT11-BT12})

Zoom of Phytoplankton on left (from r0.55/r0.44) and SST on right (from BT11+{BT11-BT12})

NDVI on left (from r0.8 & r0.6) and LST on right (from BT11 & BT12)

Looking at another data set over the southern tip of South America

Scatter of 2.3 um (top middle) on y-axis & 8.6-11 um (left) on x-axis

Clouds in Strat Scatter of BT6.7 - BT11 on y-axis & BT11 (right) on x-axis

Phytoplankton concentration on left (from r0.55/r0.44) and SST on right (from BT11+{BT11-BT12})

NDVI on left (from r0.8 & r0.6) and LST on right (from BT11 & BT12)

HYperspectral viewer for Development of Research Applications (HYDRA) Now a part of the WMO Virtual Lab For more information and a copy of the freeware see http://www.ssec.wisc.edu/hydra/.

Questions email [email protected]

Copy [email protected]

Accessing MODIS or AIRS data from GSFC DAAC at http://rapidfire.sci.gsfc.nasa.gov/realtime/

Accessing MODIS data from GSFC DAAC at http://rapidfire.sci.gsfc.nasa.gov/realtime/

View orbit tracks to select image over region of interest

Browse to image of interest

At bottom of image you can select to download hdf file onto your PC

Example with AIRS

Spectra in cloud near TC eye

Spectra in eye

Spectra in clear air

Isabel Eye Sounding with AIRS

Eye - Environment Temperature 100 200

Eye Sounding Environment Sounding

300 400 500 600 700 800 900 1000 0 2 4 6 8 10 12 14 16 18 Temperature Anomaly (C)

Integrate Hydrostatic Equation Downward from 100 hPa to Surface Environment Sounding: P s Eye Sounding: P s Aircraft Recon: P s = 1012 hPa = 936 hPa = 933 hPa DeMaria, CIRA, 2004

GOES view of Panama

SW-LW IRW

Extra slides

Table: MODIS Channel Number, Wavelength (mm), and Primary Application Reflective Bands 1,2 3,4 5-7 8-10 11-13 14-16 17-19 26 Emissive Bands 20-23 24,25 27,28 29 30 31,32 33-36 0.645, 0.865

0.470, 0.555

1.24, 1.64, 2.13

0.415, 0.443, 0.490

0.531, 0.565, 0.653

0.681, 0.75, 0.865

0.905, 0.936, 0.940

1.375

3.750(2), 3.959, 4.050

4.465, 4.515

6.715, 7.325

8.55

9.73

11.03, 12.02

13.335, 13.635, 13.935, 14.235

land/cld boundaries land/cld properties land/cld properties ocean color/chlorophyll ocean color/chlorophyll ocean color/chlorophyll atm water vapor cirrus clouds sfc/cld temperature atm temperature water vapor sfc/cld temperature ozone sfc/cld temperature cld top properties

MODIS Reflective Band Specifications

Table

: MODIS Spectral Band Specifications

MODIS Emissive Band Specifications

Primary Atmospheric Band Bandwidth 1 T typical Radiance 2 NE  T (K) NE  T (K) Application (K) at T typical Specification Predicted Surface Temperature Temperature profile Moisture profile Ozone Surface Temperature Temperature profile 20 22 23 24 25 27 28 29 30 31 32 33 34 35 36 3.660-3.840

3.929-3.989

4.020-4.080

4.433-4.498

4.482-4.549

6.535-6.895

7.175-7.475

8.400-8.700

9.580-9.880

10.780-11.280

11.770-12.270

13.185-13.485

13.485-13.785

13.785-14.085

14.085-14.385

300 300 300 250 275 240 250 300 250 300 300 260 250 240 220 0.45

0.67

0.79

0.17

0.59

1.16

2.18

9.58

3.69

9.55

8.94

4.52

3.76

3.11

2.08

0.05

0.07

0.07

0.25

0.25

0.25

0.25

0.05

0.25

0.05

0.05

0.25

0.25

0.25

0.35

0.05

0.05

0.05

0.15

0.10

0.05

0.05

0.05

0.05

0.05

0.05

0.15

0.20

0.25

0.35

1 m m at 50% response 2 W m -2 sr -1 m m -1

Example with MODIS

low refl at 1.6 um from snow in mountains

MODIS scatterplot of r1.6 (y-axis) and BT11 (x-axis)

R(0.6) R vis ~ 50 R IR (mW/m2/ster/um) R(11)

Spectral Characteristics of Energy Sources and Sensing Systems