Rennie Selkirk, NASA GSFC/GESTAR Mark Schoeberl , STC

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Variability of TTL water vapor A filtered CFH climatology and MLS water vapor for Ticosonde/Costa Rica Rennie Selkirk, NASA GSFC/GESTAR Mark Schoeberl, STC ATTREX Science Team Meeting NCAR – 24 October 2013

description

Variability of TTL water vapor A filtered CFH climatology and MLS water vapor for Ticosonde /Costa Rica . Rennie Selkirk, NASA GSFC/GESTAR Mark Schoeberl , STC. ATTREX Science Team Meeting NCAR – 24 October 2013. Sonde processing. Objectives: - PowerPoint PPT Presentation

Transcript of Rennie Selkirk, NASA GSFC/GESTAR Mark Schoeberl , STC

Page 1: Rennie  Selkirk, NASA GSFC/GESTAR Mark  Schoeberl , STC

Variability of TTL water vapor

A filtered CFH climatology andMLS water vapor for Ticosonde/Costa

Rica

Rennie Selkirk, NASA GSFC/GESTARMark Schoeberl, STC

ATTREX Science Team MeetingNCAR – 24 October 2013

Page 2: Rennie  Selkirk, NASA GSFC/GESTAR Mark  Schoeberl , STC

Sonde processing

• Objectives: – Highlight the large seasonal variability in TTL WV– Need to remove CFH noise in at scale of ~100 m

• Approach:– Low-pass filter – with attention to data gaps– Apply to all variables– Calculate seasonal climo on data from 2005-2011– Will soon add 2012 and 2013

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Temperatures at Costa Rica

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CFH Water Vaporwith previous season

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RH ice

Both seasons show rapid fall off of mean RHice profile at mean coldpoint (dashed lines)

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WV tape recorder at Costa Rica(seasonal time averages)

Season Min T (“coldpoint tropopause

”)

WV at Tmin

1st WV tape recorder min

(“hygropause”)

1st WV tape recorder max

Upper WV tape

recorder min

DJF -82.6° C (17.4 km)

2.7 ppmv 2.5 ppmv (17.9 km)

4.4 ppmv (20.5 km)

3.4 ppmv (23 km)

MAM -81.3° C (17.2 km)

3.3 ppmv 2.9 ppmv (17.4 km)

4.5 ppmv (22 km)

n/a

JJA -76.7° C (16.1 km)

6.5 ppmv 3.5 ppmv (19.7 km)

4.9 ppmv (24.1 km)

n/a

SON -79.3° C (16.7 km)

4.2 ppmv 4.2 ppmv (16.8 km)

5.3 ppmv (17.8 km)

3.5 ppmv (21.6 km)

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Water Vapor vs Ozone

DJF JJA

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MLS water vapor intecomparisons

• Long-term average data – MLS WV, version 3, interpolated via MERRA to San Jose

and in potential temperature– Can be used to compare to CFH seasonal climatology

• MLS RDFs:– Back-trajectory-based product– Synthetic high-vertical resolution water vapor (and

ozone) profiles– Use to infer day-to-day variability at a sounding

location

Page 9: Rennie  Selkirk, NASA GSFC/GESTAR Mark  Schoeberl , STC

Sondes vs. MLS v.3

Winter composite

(36 sondes)

Summer composite

(60 sondes)

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MLS RDF @ SJOSummer 2007

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MLS RDFs vs CFH

****

* *

*MLS RDF

profile(previous

slide)

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Summary

• Strong seasonal cycle of water vapor in UTLS at Costa Rica Low-pass filtering of CFH data– Tape recorder prominent

• Low-pass filtering reduces instrumental noise– But may reduce frequency of high RH in TTL too strongly

• Seasonal average fields consistent with MLS, v.3• MLS RDFs promising technique for reproducing

vertical structure seen in sondes