Upload
kalb
View
25
Download
0
Embed Size (px)
DESCRIPTION
Integration of Advanced Satellite Cloud Products into an Icing Nowcasting System. Julie Haggerty, Gary Cunning, Ben Bernstein, Michael Chapman, David Johnson, Marcia Politovich, Cory Wolff National Center for Atmospheric Research Boulder, Colorado USA Patrick Minnis and Rabindra Palikonda - PowerPoint PPT Presentation
Citation preview
Integration of Advanced Integration of Advanced Satellite Cloud Products into Satellite Cloud Products into an Icing Nowcasting Systeman Icing Nowcasting System
Julie Haggerty, Gary Cunning, Ben Bernstein, Michael Chapman, Julie Haggerty, Gary Cunning, Ben Bernstein, Michael Chapman, David Johnson, Marcia Politovich, Cory WolffDavid Johnson, Marcia Politovich, Cory WolffNational Center for Atmospheric Research National Center for Atmospheric Research
Boulder, Colorado USABoulder, Colorado USA
Patrick Minnis and Rabindra PalikondaPatrick Minnis and Rabindra PalikondaNASA Langley Research Center, Hampton, Virginia USANASA Langley Research Center, Hampton, Virginia USA
WWRP Symposium on Nowcasting and Very Short Range Forecasting, 5-9 September 2005
The NCARThe NCARCurrent Icing Potential (CIP) Current Icing Potential (CIP)
System:System:A Basic DescriptionA Basic Description
Hourly diagnosis of icing potential Hourly diagnosis of icing potential and the potential for supercooled and the potential for supercooled large drops over a three-large drops over a three-dimensional domain over the dimensional domain over the continental United Statescontinental United States
Experimental version estimates Experimental version estimates icing severityicing severity
Data sources include surface Data sources include surface observations, pilot reports, model observations, pilot reports, model forecasts, radars, and lightning forecasts, radars, and lightning sensorssensors
Limited satellite data currently Limited satellite data currently used (cloud mask and cloud top used (cloud mask and cloud top temperature)temperature)
CIP Icing Potential at 825 mb16 February 2005 at 1600 UTC
NASA Langley Satellite-derived NASA Langley Satellite-derived Cloud ProductsCloud Products
GOES Imager visible, GOES Imager visible, near-infrared, and infrared near-infrared, and infrared channelschannels
Products include cloud Products include cloud droplet phase, liquid water droplet phase, liquid water path, particle size path, particle size
These variables can These variables can indicate possible icing indicate possible icing conditions conditions potential potential improvement to CIP improvement to CIP products products
Represent conditions Represent conditions primarily near cloud topprimarily near cloud top Liquid water path at 1615 UTC on
16 February 2005 as derived from GOES-12 imagery.
Integration PlanIntegration PlanCIP-Satellite Cloud ProductsCIP-Satellite Cloud Products
Forecasters’ experience using satellite productsForecasters’ experience using satellite products Selection of satellite products likely to improve Selection of satellite products likely to improve
icing detection, i.e., phase, liquid water path, icing detection, i.e., phase, liquid water path, particle sizeparticle size
Objective assessment of satellite productsObjective assessment of satellite products Modification of CIP algorithms to include satellite Modification of CIP algorithms to include satellite
productsproducts Case studies using modified version of CIPCase studies using modified version of CIP Refinement of integration methodsRefinement of integration methods
Satellite Product ValidationSatellite Product Validation
Case studies – comparison of phase, LWP, Case studies – comparison of phase, LWP, cloud top height, particle size with research cloud top height, particle size with research aircraft and ground-based radiometer dataaircraft and ground-based radiometer data
Long-term intercomparison of satellite and Long-term intercomparison of satellite and CIP products with pilot reportsCIP products with pilot reports
Statistical characterization of satellite Statistical characterization of satellite products to verify forecasters’ guidelinesproducts to verify forecasters’ guidelines
Satellite-Aircraft Comparisons from AIRS-II
Cloud Phase
0
1
2
3
4
5
0 1 2 3 4 5
Aircraft-derived category
Sat
ellit
e-d
eriv
ed c
ateg
ory
1 = liquid1.5 = mixed2 = ice4 =clear
(10)
(3)
(1) (1)
(2)(2)
Aircraft cloud-top penetrations
• 13 aircraft-detected liquid cases
−10 classified correctly by satellite
− 2 classified as ice (overlying cirrus?)
− 1 as clear (varied conditions)
• 2 aircraft-detected mixed phase cases
− both classified as ice by satellite
• 4 aircraft-detected ice cases
− 3 classified correctly by satellite
− 1 classified as clear
MWR Mean = 238.5
GOES Mean = 264.0
MWR Stddev = 156.6
GOES Stddev = 169.2
Correlation coefficient = 0.72
AIRS-II: LWP at Montreal
0
100
200
300
400
500
600
700
800
900
0 100 200 300 400 500 600 700 800 900
GOES-derived LWP (g/m^2)
MW
R L
WP
(g
/m^
2)
Comparison of Satellite Product with Ground-based Microwave Radiometer
CIP Icing Severity IndexCIP Icing Severity Index
Severity product intended Severity product intended to characterize rate of ice to characterize rate of ice accumulation accumulation
Current data sources are Current data sources are model estimates (vertical model estimates (vertical velocity, liquid water, velocity, liquid water, temperature), pilot reports, temperature), pilot reports, and CIP icing potentialand CIP icing potential
Good candidate for Good candidate for improvement by advanced improvement by advanced satellite products because satellite products because of liquid water and particle of liquid water and particle size dependence size dependence
Severity Severity IndexIndex
DefinitionDefinition
00 No icingNo icing
0.1250.125 TraceTrace
0.250.25 Trace-lightTrace-light
0.3750.375 LightLight
0.50.5 Light-moderateLight-moderate
0.6250.625 ModerateModerate
0.750.75 Moderate-severeModerate-severe
0.8750.875 HeavyHeavy
11 SevereSevere
Case StudiesCase StudiesNortheastern United StatesNortheastern United States
Six cases identified with icing conditions and in situ Six cases identified with icing conditions and in situ measurements by a research aircraftmeasurements by a research aircraft
16 February 2005; non-precipitating, single layer 16 February 2005; non-precipitating, single layer stratus cloud; cloud top temperature -10 to -15 stratus cloud; cloud top temperature -10 to -15 ººCC
19 January 2005; widespread liquid cloud with high 19 January 2005; widespread liquid cloud with high liquid water content; cloud top temperature -10 liquid water content; cloud top temperature -10 ººCC
Adjustment of CIP Severity Index Adjustment of CIP Severity Index with Satellite Productswith Satellite Products
Cloud drop phase, 16 February 2005, 1545 UTC
Phase product locates pixels with liquid or supercooled liquid at cloud top
LWP product LWP product assumed to represent assumed to represent liquid water content in liquid water content in highest cloud layerhighest cloud layer
Adjustment of CIP Severity Index Adjustment of CIP Severity Index with Satellite Productswith Satellite Products
Liquid Water Path, 16 February 2005, 1545 UTC
Adjustment of CIP Severity Index Adjustment of CIP Severity Index with Satellite Productswith Satellite Products
Empirical scaling factor used to estimate Empirical scaling factor used to estimate liquid water content (LWC) in cloud layer liquid water content (LWC) in cloud layer using LWP estimateusing LWP estimate
New severity index calculated from LWC New severity index calculated from LWC estimate for pixels with positive icing estimate for pixels with positive icing potentialpotential
Original CIP severity index adjusted upward Original CIP severity index adjusted upward or downward by half the difference or downward by half the difference
CIP Icing Severity Index 16 February 2005 at 1600 UTC
Original estimate Modified by inclusion of satellite-derived phase and liquid water path products
Areas of high LWP
CIP Icing Severity Index 19 January 2005 at 1915 UTC
Original estimate Modified by inclusion of satellite-derived phase and liquid water path products
Interim Conclusions and Interim Conclusions and Future WorkFuture Work
Advanced satellite products appear to have skill in Advanced satellite products appear to have skill in estimating icing-related cloud variablesestimating icing-related cloud variables
Integration of phase and LWP products for Integration of phase and LWP products for adjustment of CIP severity index produces results adjustment of CIP severity index produces results consistent with aircraft measurementsconsistent with aircraft measurements
Analysis of additional, more complex cases Analysis of additional, more complex cases Refinement of integration methods and use of Refinement of integration methods and use of
additional products such as particle sizeadditional products such as particle size