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F O U N D A T I O N A L C O U R S E
April 6, 2022
Satellite Foundational Course for JPSS (SatFC-J)
MICROWAVE
F O U N D A T I O N A L C O U R S E
Introduction to Microwave Remote Sensing
(with a focus on passive sensing)
F O U N D A T I O N A L C O U R S E | 3
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Learning Objectives
1. Provide a general introduction to microwave remote sensing that
covers imagers vs. sounders, passive vs. active sensors, and
microwave frequency channels
2. Understand how microwave remote sensing complements visible
and infrared observation and why this is important
3. Briefly examine how absorption/emission, transmission, and
scattering influences the usage and interpretation of microwave
measurements
F O U N D A T I O N A L C O U R S E | 4
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Product Preview
ATMS MIRS Total Precipitable Water 2017-09-23
 A combination of
channels are used
to create products
• total precipitable
water
• cloud liquid water
• rain rate
• wind speed
• sea surface
temperature
• soil moisture
NOAA MiRS Products: https://www.star.nesdis.noaa.gov/jpss/EDRs/products_MiRS.php
ATMS MIRS Cloud Liquid Water 2017-09-23
ATMS MIRS Rain Rate 2017-09-23
AMSR2 Wind Speed 2017-09-23
AMSR2 Sea Surface Temperature 2017-09-23
AMSR2 Soil Moisture 2017-09-23
F O U N D A T I O N A L C O U R S E | 5
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Types of Microwave Instrumentation
Imager
 Horizontal detail
 2-D view
Ex: Advanced Microwave Scanning
Radiometer-2 (AMSR-2)
• 7 channels
Sounder
 Vertical detail
 “3-D view”
 Provides atmospheric profiles
Ex: Advanced Technology
Microwave Sounder (ATMS)
• 22 channels
vs
vs
F O U N D A T I O N A L C O U R S E | 6
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Passive
• Detects natural emission
• Used to measure atmospheric
profiles
• Radiometers and scanners
Active
• Provides source of radiation
and measures backscattered
signal
• Influence of other sources
complicates interpretation
Types of Microwave Sensors
F O U N D A T I O N A L C O U R S E | 7
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Global Coverage 2x Daily
Suomi National Polar–orbiting Partnership (S-NPP) Orbit Tracks
F O U N D A T I O N A L C O U R S E | 8
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Electromagnetic Spectrum
Additional Resource: SatFC-G Basic Principles of Radiation
https://www.meted.ucar.edu/training_module.php?id=1239#.WEcPZfkrKUl
Microwave wavelength = 0.1-30 cm (300-1 GHz)
Increasing: wavelength, sensor footprint
Decreasing: frequency, energy
109 Hz = 1 GHz
F O U N D A T I O N A L C O U R S E | 9
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Frequency (GHz)
Vertical
Transmittance
to
Space
Microwave Spectrum
In general:
 Window regions are used
to sense surface features
 Absorption regions are
used to derive temperature
and moisture profiles
source: COMET
F O U N D A T I O N A L C O U R S E | 1 0
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Window Regions
Absorption Regions
transmission
absorption /
emission
scattering
Clear Sky or
Non-Precipitating Clouds
• Temperature profiles
• Moisture profiles
Precipitating Clouds
• Ice particles Precipitating Clouds
• Precipitation type
• Rain rate
Clear Sky or
Non-Precipitating Clouds
• Land surface temp.
• Sea surface temp.
• Sea ice
• Soil moisture
• Cloud droplets
(< .1 mm radius)
• Ocean winds
Measured Brightness Temperature
F O U N D A T I O N A L C O U R S E | 1 1
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Window View of Surface Features
Ocean
 Low emissivity
(~0.5) provides
a uniform, cold
background
Land
 Variable
emissivity
(~0.95)
ATMS Ch 2 (31.4 GHz) 2017-9-23 1806Z
°C
-125
-105
-85
-65
-45
-25
-5
15
150
170
190
210
230
250
270
290
K
F O U N D A T I O N A L C O U R S E | 1 2
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
“Dirty” Window View
 Non-precipitating
clouds are
transparent
 Total atmospheric
column can be
observed
ATMS Ch 16 (88.2 GHz) 2017-9-23 1806Z
-125
-105
-85
-65
-45
-25
-5
15
°C
150
170
190
210
230
250
270
290
K
F O U N D A T I O N A L C O U R S E | 1 3
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Water Vapor Absorption
 Used to sense the
moisture at various
levels in the
atmosphere
ATMS Ch 20 (183.3 GHz) 2017-9-23 1806Z
-125
-105
-85
-65
-45
-25
-5
15
150
170
190
210
230
250
270
290
K
°C
F O U N D A T I O N A L C O U R S E | 1 4
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Oxygen Absorption
 Used to sense the
temperature at
various levels in
the atmosphere
ATMS Ch 10 (57.3 GHz) 2017-9-23 1806Z
-125
-105
-85
-65
-45
-25
-5
15
150
170
190
210
230
250
270
290
K
°C
Small temperature
variation across
the image
(~300 mb level)
F O U N D A T I O N A L C O U R S E | 1 5
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Vertical Profiles
 Displayed in AWIPS as
NUCAPS soundings
 NUCAPS = NOAA
Unique Combined
Atmospheric
Processing System
F O U N D A T I O N A L C O U R S E | 1 6
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Assimilation into Numerical Models
 Microwave and infrared sounders have huge impacts in forecasts
through assimilation into numerical weather prediction models
500 hPa geopotential height anomaly correlation
12-month running mean
1981 2017
%
F O U N D A T I O N A L C O U R S E | 1 7
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Advantages and Limitations
Microwave Advantages
• Non-precipitating clouds are transparent
• Precipitation rate estimation, ocean winds, soil moisture
• Atmospheric temperature and moisture profiles
• Blended with other high resolution measurements in products
and assimilated into models
Microwave Limitations
• Longer wavelength limits spatial resolution
• Variations in surface emissivity complicate interpretation
• Infrequent observations: 2x daily passes per satellite
F O U N D A T I O N A L C O U R S E | 1 8
MICROWAVE
CONSTELLATION
APPLICATIONS
INITIATIVES
Resources
 Microwave Remote Sensing: Overview (2nd Edition)
https://www.meted.ucar.edu/training_module.php?id=979
 A First Course in Atmospheric Radiation, 2nd Ed. (Petty 2006)
 Satellite Meteorology: An Introduction (Kidder and Vonder Haar 1995)
 Basics of Visible and Infrared Remote Sensing
https://www.meted.ucar.edu/training_module.php?id=1096#.WEmPA_krKUk
 SatFC-G Basic Principles of Radiation
https://www.meted.ucar.edu/training_module.php?id=1239#.WEcPZfkrKUl
Questions? Email: Bernie.Connell@colostate.edu
Narrator: Bernie Connell
Editors: Erin Dagg, Bernie Connell
Other Contributors: John Forsythe

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Sat fc j-intro_mw_remotesensing

  • 1. F O U N D A T I O N A L C O U R S E April 6, 2022 Satellite Foundational Course for JPSS (SatFC-J)
  • 2. MICROWAVE F O U N D A T I O N A L C O U R S E Introduction to Microwave Remote Sensing (with a focus on passive sensing)
  • 3. F O U N D A T I O N A L C O U R S E | 3 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Learning Objectives 1. Provide a general introduction to microwave remote sensing that covers imagers vs. sounders, passive vs. active sensors, and microwave frequency channels 2. Understand how microwave remote sensing complements visible and infrared observation and why this is important 3. Briefly examine how absorption/emission, transmission, and scattering influences the usage and interpretation of microwave measurements
  • 4. F O U N D A T I O N A L C O U R S E | 4 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Product Preview ATMS MIRS Total Precipitable Water 2017-09-23  A combination of channels are used to create products • total precipitable water • cloud liquid water • rain rate • wind speed • sea surface temperature • soil moisture NOAA MiRS Products: https://www.star.nesdis.noaa.gov/jpss/EDRs/products_MiRS.php ATMS MIRS Cloud Liquid Water 2017-09-23 ATMS MIRS Rain Rate 2017-09-23 AMSR2 Wind Speed 2017-09-23 AMSR2 Sea Surface Temperature 2017-09-23 AMSR2 Soil Moisture 2017-09-23
  • 5. F O U N D A T I O N A L C O U R S E | 5 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Types of Microwave Instrumentation Imager  Horizontal detail  2-D view Ex: Advanced Microwave Scanning Radiometer-2 (AMSR-2) • 7 channels Sounder  Vertical detail  “3-D view”  Provides atmospheric profiles Ex: Advanced Technology Microwave Sounder (ATMS) • 22 channels vs vs
  • 6. F O U N D A T I O N A L C O U R S E | 6 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Passive • Detects natural emission • Used to measure atmospheric profiles • Radiometers and scanners Active • Provides source of radiation and measures backscattered signal • Influence of other sources complicates interpretation Types of Microwave Sensors
  • 7. F O U N D A T I O N A L C O U R S E | 7 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Global Coverage 2x Daily Suomi National Polar–orbiting Partnership (S-NPP) Orbit Tracks
  • 8. F O U N D A T I O N A L C O U R S E | 8 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Electromagnetic Spectrum Additional Resource: SatFC-G Basic Principles of Radiation https://www.meted.ucar.edu/training_module.php?id=1239#.WEcPZfkrKUl Microwave wavelength = 0.1-30 cm (300-1 GHz) Increasing: wavelength, sensor footprint Decreasing: frequency, energy 109 Hz = 1 GHz
  • 9. F O U N D A T I O N A L C O U R S E | 9 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Frequency (GHz) Vertical Transmittance to Space Microwave Spectrum In general:  Window regions are used to sense surface features  Absorption regions are used to derive temperature and moisture profiles source: COMET
  • 10. F O U N D A T I O N A L C O U R S E | 1 0 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Window Regions Absorption Regions transmission absorption / emission scattering Clear Sky or Non-Precipitating Clouds • Temperature profiles • Moisture profiles Precipitating Clouds • Ice particles Precipitating Clouds • Precipitation type • Rain rate Clear Sky or Non-Precipitating Clouds • Land surface temp. • Sea surface temp. • Sea ice • Soil moisture • Cloud droplets (< .1 mm radius) • Ocean winds Measured Brightness Temperature
  • 11. F O U N D A T I O N A L C O U R S E | 1 1 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Window View of Surface Features Ocean  Low emissivity (~0.5) provides a uniform, cold background Land  Variable emissivity (~0.95) ATMS Ch 2 (31.4 GHz) 2017-9-23 1806Z °C -125 -105 -85 -65 -45 -25 -5 15 150 170 190 210 230 250 270 290 K
  • 12. F O U N D A T I O N A L C O U R S E | 1 2 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES “Dirty” Window View  Non-precipitating clouds are transparent  Total atmospheric column can be observed ATMS Ch 16 (88.2 GHz) 2017-9-23 1806Z -125 -105 -85 -65 -45 -25 -5 15 °C 150 170 190 210 230 250 270 290 K
  • 13. F O U N D A T I O N A L C O U R S E | 1 3 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Water Vapor Absorption  Used to sense the moisture at various levels in the atmosphere ATMS Ch 20 (183.3 GHz) 2017-9-23 1806Z -125 -105 -85 -65 -45 -25 -5 15 150 170 190 210 230 250 270 290 K °C
  • 14. F O U N D A T I O N A L C O U R S E | 1 4 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Oxygen Absorption  Used to sense the temperature at various levels in the atmosphere ATMS Ch 10 (57.3 GHz) 2017-9-23 1806Z -125 -105 -85 -65 -45 -25 -5 15 150 170 190 210 230 250 270 290 K °C Small temperature variation across the image (~300 mb level)
  • 15. F O U N D A T I O N A L C O U R S E | 1 5 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Vertical Profiles  Displayed in AWIPS as NUCAPS soundings  NUCAPS = NOAA Unique Combined Atmospheric Processing System
  • 16. F O U N D A T I O N A L C O U R S E | 1 6 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Assimilation into Numerical Models  Microwave and infrared sounders have huge impacts in forecasts through assimilation into numerical weather prediction models 500 hPa geopotential height anomaly correlation 12-month running mean 1981 2017 %
  • 17. F O U N D A T I O N A L C O U R S E | 1 7 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Advantages and Limitations Microwave Advantages • Non-precipitating clouds are transparent • Precipitation rate estimation, ocean winds, soil moisture • Atmospheric temperature and moisture profiles • Blended with other high resolution measurements in products and assimilated into models Microwave Limitations • Longer wavelength limits spatial resolution • Variations in surface emissivity complicate interpretation • Infrequent observations: 2x daily passes per satellite
  • 18. F O U N D A T I O N A L C O U R S E | 1 8 MICROWAVE CONSTELLATION APPLICATIONS INITIATIVES Resources  Microwave Remote Sensing: Overview (2nd Edition) https://www.meted.ucar.edu/training_module.php?id=979  A First Course in Atmospheric Radiation, 2nd Ed. (Petty 2006)  Satellite Meteorology: An Introduction (Kidder and Vonder Haar 1995)  Basics of Visible and Infrared Remote Sensing https://www.meted.ucar.edu/training_module.php?id=1096#.WEmPA_krKUk  SatFC-G Basic Principles of Radiation https://www.meted.ucar.edu/training_module.php?id=1239#.WEcPZfkrKUl Questions? Email: Bernie.Connell@colostate.edu Narrator: Bernie Connell Editors: Erin Dagg, Bernie Connell Other Contributors: John Forsythe