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A First Look at the CloudSat Precipitation Dataset

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Nadir pointing, 94 GHz radar. 3.3 s pulse 500m vertical res. ... CPR is nadir-pointing providing only a 2D slice of the real world. 10/23/09. 3rd IPWG Workshop ... – PowerPoint PPT presentation

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Title: A First Look at the CloudSat Precipitation Dataset


1
A First Look at the CloudSat Precipitation Dataset
  • Tristan LEcuyer
  • S. Miller, C. Mitrescu, J. Haynes, C. Kummerow,
    and J. Turk

2
The CloudSat Mission
Primary Objective To provide, from space, the
first global survey of cloud profiles and cloud
physical properties, with seasonal and
geographical variations needed to evaluate the
way clouds are parameterized in global models,
thereby contributing to weather predictions,
climate and the cloud-climate feedback problem.
The Cloud Profiling Radar
  • Nadir pointing, 94 GHz radar
  • 3.3?s pulse ? 500m vertical res.
  • 1.4 km horizontal res.
  • Sensitivity -28 dBZ
  • Dynamic Range 80 dB
  • Antenna Diameter 1.85 m
  • Mass 250 kg
  • Power 322 W

3
but can it measure precipitation?
4
CloudSats First Image
25 km
1300 km
http//cloudsat.cira.colostate.edu/index.php Click
CURRENT STATUS
5
Applications
  • A few examples from other talks
  • Testing rainfall detection capabilities of PMW
    sensors
  • Calibrating high temporal resolution global
    rainfall datasets
  • Evaluating PMW rainfall estimates over land
    surface
  • Comparisons with global rainfall statistics from
    other sensors (particularly at higher latitudes)
  • Global statistics of frozen precipitation
  • Other science applications
  • Evaluating physical assumptions in PMW algorithms
    (eg. beamfilling/vertical structure/freezing
    level)
  • Assessing the significance of light rainfall and
    snowfall in the global energy and water cycles
  • Aerosol indirect effects on precipitation

6
Probabilistic Philosophy
  • Algorithm
  • infer vertical profile of precipitating LWC/IWC
    and surface rainrate from the observed
    reflectivity profile and an integral constraint
    (eg. PIA or precipitation water path)
  • Strengths
  • Probabilistic retrieval framework adopted
  • Allows formal inclusion of multiple forms of
    information including a priori knowledge and
    additional measurements and/or constraints
  • Explicitly accounts for uncertainties in all
    unknown parameters
  • Provides quantitative measures of uncertainties
    including relative contributions of all forms of
    assumed knowledge and measurement error
  • CPR offers higher spatial resolution than other
    sensors that directly measure precipitation
  • Sensitivity to continuum of clouds, drizzle,
    rainfall, and snowfall facilitates studying
    transition regions
  • Weaknesses
  • Strong attenuation at 94 GHz can lead to
    retrieval instability
  • Single-frequency method limits information
    regarding the dielectric properties of the
    melting layer and restricts DSD assumptions
  • CPR is nadir-pointing providing only a 2D slice
    of the real world

7
First Attempt at a Retrieval
South Carolina
8
Sanity Check
NEXRAD and CPR Rainfall
Default M-P Tropical CloudSat
Rainrate (mm h-1)
CPR Reflectivity (09/07/2006 1843 UTC)
B
A
Distance (km)
A
B
9
Tropical Storm Ernesto
http//www.nrlmry.navy.mil/nexsat_pages/nexsat_hom
e.html Click CloudSat
10
Applications
  • A few examples from other talks
  • Testing rainfall detection capabilities of PMW
    sensors
  • Calibrating high temporal resolution global
    rainfall datasets
  • Evaluating PMW rainfall estimates over land
    surface
  • Comparisons with global rainfall statistics from
    other sensors (particularly at higher latitudes)
  • Global statistics of frozen precipitation
  • Other science applications
  • Evaluating physical assumptions in PMW algorithms
    (eg. beamfilling/vertical structure/freezing
    level)
  • Assessing the significance of light rainfall and
    snowfall in the global energy and water cycles
  • Aerosol indirect effects on precipitation

11
The A-Train Constellation
Formation flying provides opportunities for
product inter-comparisons and the development of
multi-sensor algorithms.
12
Comparison with AMSR-E
16 days of direct pixel match-ups during August
2006
13
Global Rainfall Statistics
14
Tropics
15
Higher Latitudes
16
Pixel-Level Comparisons
157.7ºW
157.8ºW
17.95ºS
8.0 6.0 4.0 2.0 0.0
Rainrate (mm h-1)
Z (dBZ)
Zsfc (Black) PIA (green)
CloudSat
Rainrate (mm h-1)
18.42ºS
AMSR-E 37 GHz FOV (approximate)
17
Frozen Precipitation
15ºN
15ºS
  • CloudSats sensitivity makes it ideal for
    detecting snowfall.
  • The region poleward of 60º is sampled 4 times
    more frequently than an equal area region at the
    equator!

60ºS
90ºS
18
A First Look at Snowfall fromCloudSats
Perspective
19
Radar-Only Retrieval
  • Very preliminary inversion of CPR reflectivities
    to infer snowfall rate
  • Assumes exponential distribution of snow
    particles
  • Similar probabilistic retrieval framework as
    rainfall retrieval
  • First goal is detection and discrimination from
    light rainfall

20
Final Thoughts
  • Early results from CloudSat confirm its
    potential for detecting and quantifying light
    rainfall and snow toward answering the question
    How important are light rainfall and snow in the
    global hydrologic cycle and energy budget?
  • Two development streams (a) PIA-based detection
    and column-mean rainrate, (b) full probabilistic
    vertical structure retrieval. Ultimately merged
    into a single product.
  • First products from both algorithms for the
    first 6 months of operation may be available as
    early as years end.
  • More comprehensive validation of products is
    underway.

21
Outline
  • Applications highlight the need for these
    observations with particular emphasis on PMW and
    science apps. use the global distribution as a
    specific example
  • Briefly re-iterate CloudSats purpose and lead
    into What about rain?
  • First image confirms what sensitivity studies
    showed years earlier CloudSat CAN see rainfall
  • Algorithm VERY briefly point out measurements,
    retrieved parameters, and philosophy for getting
    from one to the other
  • Example point out that results are reasonable
    (only) not validation
  • Ernesto CloudSat even capable of seeing heavier
    precipitation
  • Point out advantage of A-Train co-located obs.
    from AMSR-E/CloudSat like a TRMM PR/TMI
  • Show two types of comparisons (a) Initial
    statistical comparisons over a 16 day period
    using a stripped-down PIA-based version of the
    algorithm, (b) more detailed pixel-level
    comparison (shows relative footprint sizes and
    demonstrates testing of detection, freezing
    level, vertical distribution, beamfilling, etc.).
  • Conclude with snowfall not many talks on this
    so far but CloudSat sampling sensitivity makes
    it a very useful snowfall sensor.
  • Results are VERY preliminary but demonstrate
    detection capability

22
Significance
CloudSats contribution to global precipitation
observations may be to assess the importance of
light rainfall and snow in the global energy
budget and hydrologic cycle.
23
Can Rainfall be MeasuredWith A Cloud Radar?
24
Global Light Rainfall Statistics
25
Science Applications
26
Aerosol Impacts?
GOCART Sulfate Aerosol (Feb. 01, 2000)
27
Implementation (NRL)
Level-0
Level-1B
Downlink Raw Telemetry
Kirtland AFB
CIRA/DPC
NRL Monterey
New CPR L1B File
MODIS, AMSR-E
CRON
NOGAPS T/Q
Sigma_0 Database
UPDATE s0 Database
Gas Extinction
IGBP Database
Particle Scattering
Linux Processing Cluster
N
LOOP OVER ALL SHOTS
ZgtZthresh?
Driver Defines Input Metadata
Read Ancillary Databases
Read CPR Data Cloud Mask/Class
Y
DO RETRIEVAL!
Calculate Error Stats Store All Data
Interpolate T/Q Profile
Determine Gas Extinction
Define Constraints (e.g., PIA, LWP)
First Guess (Z/R)
RETRIEVAL LOOP
N
Optimal Estimation
Y
Converged?
Compute Forward Model Sensitivity
Compute Sx and Increment R
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