IMAPP Remote Sensing Workshop
28 Feb. - 2 Mar. 2006
And¿ya Rocket Range, Andenes, Norway
Useful Material Handout
Table: Summary
of Hydra Commands
Hydra menu
Displays world map with image control
functions indicated on the bottom
Reset
Zoom in (left click plus drag)
Zoom
out (left click plus drag)
Rubber
band zoom (left click plus drag to create box for enlargement)
Translate (left click plus drag)
Pick
image (left click plus drag displays location of the chosen pixel)
Subset
image (left click plus drag to create subset of image; this is automatically
transferred from Hydra into the Multichannel viewer when both are engaged)
Also shows menus for Data, Settings, and Start at top
Data menu:
Local allows you to scroll through local
directories to find data
á Remote allows you to find an AIRS granule
from a remote server (a) MODIS Direct Broadcast
or (b) Goddard DAAC
Exit
After a MODIS or AIRS granule is selected
hydra displays the infrared window on a world map
Settings menu
Set color range (left click shows VisAD histogram – color range can
be altered with
á a right click plus drag at either end of
the color scale)
o Set color scale gives choice of color, grey, or
inverse grey (which produces white clouds)
Start opens Multichannel Viewer
á wherein a spectra (wavenumber on
x-axis and radiance on y-axis) is displayed along with a spectral band
superimposed on a world map. Left
click on pick image in bottom tool bar the allows you to see the pixel value
for a given lat-lon (using left click and drag)
Tools menu
Linear Combinations opens channel combination tool display
where you can specify
á linear combinations of spectral bands
a,b,c and d
á (a ±«ü b) ±«ü (c ±«ü d)
o Compute creates an image of the selected linear
combination (indicate at the
¤ bottom preference for this linear
combination to be x- or y-axis in the scatter plot)
Scatter
allows you to create
a scatter plot of the chosen x- and y-axis linear
á combinations. Five color area boxes (or area curves) can be initiated at
o the bottom of the scatter plot; a left
click drag in the scatter plot highlights the chosen points in the scatter plot
and simultaneously in the x- and y-axis images. Conversely left click drag in the x- or y- axis images shows
the locations of the chosen pixels in the scatter plot. Each color area box (or area curve) can
be erased with a left click when the color box is engaged; after erasure
another area box (or area curve) can be selected for this color.
Transect allows you to create a line on the image
and see the temperatures or
á radiances of the transect. This is enabled with a left click drag.
Capture Display makes jpeg in location you specify
Statistics allows you to display min and max values
and locations on image (toggle on
á or off)
Settings menu
Set color range opens VISAD histogram of brightness
temperature (BT) values
Radiance – BT allows you to select radiance or
brightness temperature in the display
Projection allows you to put the data in a given
projection (mercator is the default)
Set Color Scale gives you the choice of color, grey, or
inverted grey
Figure 1 Black: Earth IR Emission
Spectrum at high spectral resolution. Red VIIRS IR bands. Green: MODIS IR bands
Figure 2. Black: Atmospheric
Transmittance. Red: VIIRS bands. Green: MODIS bands.
Figure 3. Top
left: Surface Albedo; Top middle:
Surface Reflactance. Top right: MODIS Weighting functions. Bottom left:
Absorpion Coefficient for Water and ICE. Bottom Middle: Surface Emissivity in
the IR portion of the Spectrum. Bottom right: Absorption characteristics for
water and chlorophyll.
Figure 4. Reflectance of Ocean Water.
Figure 5. Planck functions for different
black body temperature values.
MODIS Instrument Characteristics
MODIS Reflected Solar Bands |
MODIS Thermal Emissive Bands |
||||
Band |
Wavelength (micron) |
Primary application |
Band |
Wavelength (micron) |
Primary application |
1,2 |
0.645, 0.866 |
Land, Clouds |
20-23 |
3.75(2), 3.95, 4.05 |
Surface / cloud temperature |
3,4 |
0.470, 0.555 |
Land, Clouds |
24,25 |
4.46, 4.51 |
Atmospheric temperature |
5-7 |
1.24, 1.64, 2.13 |
Land, Clouds |
27,28 |
6.71, 7.32 |
Water vapor |
8-10 |
0.450, 0.443, 0.490 |
Ocean color |
29 |
8.55 |
Surface / cloud temperature |
11-13 |
0.531, 0.565, 0.653 |
Ocean color |
30 |
9.73 |
Ozone |
14-16 |
0.681, 0.750, 0.865 |
Ocean color |
31,32 |
11.03, 12.02 |
Surface / cloud temperature |
17-19 |
0.905, 0.936, 0.940 |
Water vapor |
33,34 |
13.33, 13.63 |
Cloud top properties |
26 |
1.375 |
Cirrus clouds |
35,36 |
13.93, 14.23 |
Cloud properties |
Table: Summary of some MODIS Cloud
Tests
Scene |
Solar/Reflectance |
Thermal |
Comments |
|
|
|
|
Low cloud over water |
R0.86, R0.67/R0.86, BT11-BT3.7 |
Difficult, Compare BT11 to daytime mean clear-sky values
of BT11; BT11 in combination with BT difference tests; Over oceans, expect a relationship between [BT11-BT8.6], [BT11-BT12]
due to water vapor correlation to SST |
Spatial and temporal uniformity tests sometimes used over
water scenes; Beware of Sun-glint regions |
High Thick cloud over water |
R1.38, R0.86, R0.67/R0.86, |
BT11 ;
BT13.6 ; BT6.7 [BT11-BT8.6], [BT11-BT12] |
Easy, good contrast in vis and IR |
High Thin cloud over water |
R1.38, DR0.86, [R0.65–R1.6]/[R0.65+R1.6]; |
BT6.7
; BT13.9 [BT11-BT12], [BT3.7-BT12], [BT8.6-BT11] |
For R1.38, be careful of surface reflectance
for atmospheres with low total water vapor amounts. For BT difference tests, beware of variations in surface
emissivity. |
Low cloud over snow |
[R0.65–R1.6]/[R0.65+R1.6]; R2.1
back up to 1.6 [BT11-BT3.7]<<0 |
Difficult, look for inversions in clr sky BT11-BT6.7 < 0 |
NDSI (Normalized Difference Snow Index) is ratio test. R2.1 is also dark over snow and bright for low
cloud. |
High thick cloud over snow |
R1.38; [R0.65–R1.6]/[R0.65+R1.6] |
BT11 ; BT13.6 ; BT6.7 Look for inversions, suggesting cloud-free. |
Usually easy |
High thin cloud over snow |
R1.38; [R0.65–R1.6]/[R0.65+R1.6] |
BT11 ; BT13.6 ; BT6.7 Look for inversions, suggesting clear sky. |
|
Low cloud over vegetation |
R0.86,
R0.67/R0.87, BT11-BT3.7; [R0.86–R0.65] /[R0.86+R0.65] |
Difficult, BT11 in combination with BT
difference tests. |
NDVI (Normalized Difference Vegetation Index). Other ratio tests also are good. Can make tests a function of
ecosystem. |
High Thick cloud over vegetation |
R1.38, R0.86, R0.67/R0.86, [R0.86–R0.65]
/[R0.86+R0.65] |
BT11 ;
BT13.9; BT6.7 [BT11-BT8.6], [BT11-BT12] |
Can make tests a function of ecosystem to account for
variations in surface emittance and reflectance. |
High Thin cloud over vegetation |
R1.38, R0.86, R0.67/R0.86, [R0.86–R0.65]
/[R0.86+R0.65] |
BT13.9;
BT6.7 [BT11-BT8.6], [BT11-BT12] |
Beware of variations in surface emittance and reflectance. |
Low cloud over bare soil |
R0.86, R0.67/R0.86, [BT11-BT3.7] |
BT11 in combination with brightness temperature
difference tests. [BT3.7-BT3.9] |
Difficult due to brightness and spectral variation in
surface emissivity. Surface reflectance at 3.7 and 3.9 mm
is similar. |
High Thick cloud over bare soil |
R1.38, R0.86, R0.67/R0.86 |
BT13.9; BT6.7 BT11 in combination with brightness temperature
difference tests. |
|
High Thin cloud over bare soil |
R1.38, R0.86, R0.67/R0.87,
[BT11-BT3.7] |
BT13.9; BT6.7 BT11 in combination with brightness temperature
difference tests, for example [BT3.7-BT3.9] |
Difficult; be careful of surface reflectance at 1.38 mm.
and variations in surface emittance. |
Cloud-top pressure |
|
Channels in absorption band of carbon dioxide (13-14mm) |
CO2 slicing |
Cloud phase |
Combination of R0.86; R1.6 and R2.1 |
[BT8.6 – BT11]>0 for ice
and <0 for water. [BT11 – BT12] for water clouds
> [BT8.6 – BT11]. Conversely, [BT8.6 – BT11] for ice cloud
> [BT11 – BT12]. |
Watch out for cloud overlap Determine phase by using observations that test for high
cloud versus those that test for low. |
Cloud particle size |
Combination
of R0.86; R1.6 ,
R2.1; & R3.7 |
[BT8.6 – BT11] values versus
[BT11 – BT12] is useful for thin high clouds. |
Arches |