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The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models Summary of field research in Leticia, Colombia, Feb. 18 th – 26 th , 2011

The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

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The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models. Summary of field research in Leticia, Colombia, Feb. 18 th – 26 th , 2011. Outline. Assess feasibility of acquiring sounding data in the Amazon basin What is sounding data? Why do we need it? - PowerPoint PPT Presentation

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Page 1: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Summary of field research in Leticia, Colombia, Feb. 18th –

26th, 2011

Page 2: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Outline

Assess feasibility of acquiring sounding data in the Amazon basin What is sounding data? Why do we need it? What are the constraints?

Page 3: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Climate vs. Weather

Weather: recent or current conditions (ex. Cloud cover, precipitation)• Short term

Climate: typical weather for a given location• Long term• Includes weather extremes• Ex. Monthly rainfall, snowfall, normal temp extremes

Page 4: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

What is Sounding Data?

Real time data for atmospheric variables Temperature Pressure Relative Humidity Winds

Page 5: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Atmospheric General Circulation Models (AGCMs)

Included in Global Climate Models AGCMs differ in spatial resolutions Variables

temperature pressure humidity winds water and ice condensate in cloud

Page 6: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Limited-Area Models/RegionalClimate Models (RCMs)

Studying climatic processes and interactions on scales too fine for typical GCM resolutions.

RCMs can give more intense events that will be smoothed in coarser-resolution GCMs.

Page 7: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Environmental Lapse Rate Environmental Lapse Rate • the decrease

in temperature with altitude (-dT/dz or -dT/dp)

Atmospheric layers are defined by the change of sign of the lapse rate

Page 8: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Data Collection Methods Surface

Stations or ships Radiosonde

Tether System High – Altitude Balloon

Satellite Microwave Radiation

Page 9: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Radiosondes

Many varieties Include instrument

and ground station Some are mobile

Expendable Includes:

Temperature Relative Humidity Pressure Wind

Page 10: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models
Page 11: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models
Page 12: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models
Page 13: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Balloon Sounding Constraints

Cost Mobility Accuracy of data

Page 14: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Cost Constraints

AnaSonde

Vaisala

Page 15: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models
Page 16: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models
Page 17: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Mobility Constraints

Page 18: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Requirements of Climate Studies

•Temperature• ±2.5°C at ambient

temperature

•Relative Humidity• ±2% for 10°C<T<20°C• ±5% for T<10°C

•Pressure• ±2%

AnaSonde Accuracy

Page 19: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models
Page 20: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models
Page 21: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Current Findings:

Christy et al. 2010: What Do Observational Datasets Say about Modeled Tropospheric Temperature Trends since 1979?

Thorne et al. 2011: Tropospheric temperature trends: history of an ongoing controversy

Preliminary Manaus analysis: Surface increase over last 10 years = .5 degrees C Sounding to 10km increase over same period is

only .15 degrees C

Page 22: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models
Page 23: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

30 Year Sounding Analysis

Assign weight to each year at each altitude Increments of 100m

At each altitude, divide the sum of weight by the sum of % available

Page 24: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

30 Year Sounding Analysis

Find difference at each altitude

Find the average difference

Find the average of the monthly trends

Page 25: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Monthly ELR Change

1 2 3 4 5 6 7 8 9 10 11 12

-0.6

-0.4

-0.2

0

0.2

0.4

0.6

Natal ELR

Dry season ELR average changeWet season ELR average changeST average changeELR average changeMonthly ELR change

Month

ELR

Chan

ge (

deg

C)

Page 26: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

MONTH   1 2 3 4 5 6 7 8 9 10 11 12                           

AVERAGE CHANGE   -0.073820.109067 -0.14193 -0.12137 -0.15117 -0.498670.1925740.2873940.0588290.1276730.241961 -0.22174

AVERAGE ST CHANGE   0.1894480.6477450.0858280.7554890.7670180.1790160.8134740.2952060.2268070.871011 0.646140.437116AVERAGE DRY   -0.10192 -0.10192 -0.10192 -0.10192 -0.10192 -0.10192 -0.10192 -0.10192 -0.10192 -0.10192 -0.10192 -0.10192

AVERAGE WET   0.07005 0.07005 0.07005 0.07005 0.07005 0.07005 0.07005 0.07005 0.07005 0.07005 0.07005 0.07005AVERAGE   -0.01593 -0.01593 -0.01593 -0.01593 -0.01593 -0.01593 -0.01593 -0.01593 -0.01593 -0.01593 -0.01593 -0.01593

AVERAGE ST   0.4928580.4928580.4928580.4928580.4928580.4928580.4928580.4928580.4928580.4928580.4928580.492858

AVERAGE SURFACE TEMP   28.69 28.67 28.55 28.15 27.67 26.32 25.64 26.13 27.56 28.44 28.89 28.94

AVERAGE 10KM TEMP   -5.34 -5.09 -4.53 -4.19 -4.2 -4.76 -5.6 -5.16 -4.92 -4.81 -4.9 -5.16

AVERAGE 02KM TEMP   14.71 14.67 15.31 15.48 15.27 14.38 13.53 13.45 13.79 14.57 14.78 13.53AVERAGE ELR   -5.85167 -5.82833 -5.70667 -5.56 -5.51333 -5.37 -5.415 -5.39833 -5.59 -5.71 -5.815 -5.89333

AVERAGE DRY ELR   -5.56556 -5.56556 -5.56556 -5.56556 -5.56556 -5.56556 -5.56556 -5.56556 -5.56556 -5.56556 -5.56556 -5.56556

AVERAGE WET ELR   -5.70972 -5.70972 -5.70972 -5.70972 -5.70972 -5.70972 -5.70972 -5.70972 -5.70972 -5.70972 -5.70972 -5.70972

Natal 12Z

Page 27: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

MONTH   1 2 3 4 5 6 7 8 9 10 11 12

                           AVERAGE CHANGE   0.583342 #DIV/0! #DIV/0! #DIV/0! #DIV/0! -0.69287 #DIV/0! 1.2259920.4658121.4963310.865918 #DIV/0!

AVERAGE ST CHANGE   1.01119 #DIV/0! #DIV/0! #DIV/0! #DIV/0! -0.04101 #DIV/0! 1.0713281.1604341.1665391.162777 #DIV/0!

AVERAGE DRY   #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0!

AVERAGE WET   #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0!

AVERAGE   #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0!

AVERAGE ST   #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0! #DIV/0!

AVERAGE SURFACE TEMP   26.97 27.56 27.46 27.63 26.38 25.39 24.66 24.63 25.1 26.14 26.53 26.83

AVERAGE 10KM TEMP   -34.53 -33.63 -33.22 -32.43 -32.77 -33.45 -34.85 -34.38 -34.46 -34.14 -33.99 -35.09

AVERAGE 02KM TEMP   15.43 15.57 15.42 15.65 15.24 13.99 13.73 13.64 13.87 14.95 15.33 15.37

AVERAGE ELR   -5.56667 -5.61667 -5.57833 -5.5 -5.34167 -5.36333 -5.19 -5.10667 -5.22 -5.34 -5.43333 -5.53833AVERAGE DRY ELR   -5.43167 -5.43167 -5.43167 -5.43167 -5.43167 -5.43167 -5.43167 -5.43167 -5.43167 -5.43167 -5.43167 -5.43167

AVERAGE WET ELR   -5.3675 -5.3675 -5.3675 -5.3675 -5.3675 -5.3675 -5.3675 -5.3675 -5.3675 -5.3675 -5.3675 -5.3675

Natal 00Z

Page 28: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models
Page 29: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Further Research

Accuracy and precision of sensors Quantifying uncertainties in sounding

data Acquiring reliable and cost-effective

sounding data for the Amazon rainforest Increase in the amount of data

Page 30: The Implications of Increased Sounding Data in the Amazon Basin for Global Climate Models

Acknowledgements UM Office of Research and Sponsored Programs UM Excellence Fund: Office of the Provost and

Vice President for Academic Affairs UM Department of Physics and Astronomy Montana Space Grant Consortium Entropika Anasphere Jennifer Fowler