SMAPVEX08 Surface Roughness Data, Version 1
Surface roughness data for this data set were collected at several field sites as part of the Soil Moisture Active Passive Validation Experiment 2008 (SMAPVEX08) campaign.
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Geographic Coverage
Parameter(s): 


Spatial Coverage: 

Spatial Resolution: 

Temporal Coverage: 

Temporal Resolution:  Varies 
Data Format(s): 

Platform(s)  FIELD SURVEYS 
Sensor(s):  CAMERAS 
Version:  V1 
Data Contributor(s):  Cosh, M. and R. Bindlish. 
Metadata XML:  View Metadata Record 
Data Citation
As a condition of using these data, you must cite the use of this data set using the following citation. For more information, see our Use and Copyright Web page.
Cosh, M. and R. Bindlish. 2015. SMAPVEX08 Surface Roughness Data, Version 1. [Indicate subset used]. Boulder, Colorado USA. NASA National Snow and Ice Data Center Distributed Active Archive Center. doi: https://doi.org/10.5067/1UCIETYP0PUO. [Date Accessed].Detailed Data Description
Surface roughness measurements for this data set were collected at several field sites as part of the Soil Moisture Active Passive Validation Experiment 2008 (SMAPVEX08) campaign.
Data are provided in the ASCII tabdelimited text file, SMAPVEX08_SR.txt
. An associated Extensible Markup Language (XML) metadata file is also provided. The following table describes the column headings and contents in the data file.
Column Heading  Description 

Name  Field location and orientation (2 photos, 90 degrees from each other) 
np  Number of digitized points 
sigma  Root mean square error (mm) 
length  Correlation length (mm) 
asigma  Root mean square error adjusted for slope (mm) 
exponent  Power coefficient 
Data files are available at:
https://n5eil01u.ecs.nsidc.org/SMAP_VAL/SV08SR.001/
The data file is named SV08SR_SMAPVEX08_SR.txt
, where SR
indicates surface roughness.
The data file is approximately 1.6 KB.
Southernmost Latitude: 38.8°N
Northernmost Latitude: 39.1°N
Westernmost Longitude: 76.3°W
Easternmost Longitude: 75.6°W
A onemeter grid board was used for in situ measurements.
Photographs were acquired once per site from 29 September 2008 through 13 October 2008.
Parameters include root mean square of surface height variation (mm), correlation length (mm), and power coefficient
Parameter Range
Valid parameter values are as follows:
Root mean square of surface height variation: 0  30 mm
Correlation length: 0  300 mm
Power coefficient: 0  2 (dimensionless)
Software and Tools
No special tools are required to read these data. Any text editor or Web browser can read ASCII text files.
Data Acquisition and Processing
The soil roughness of the SMAPVEX08 data set is described using three parameters; root mean square height (rms height or sigma), correlation length (L) and the correlation function f(L). The root mean square height describes the random surface characteristics, while the correlation length and correlation function describe the periodicity of the soil surface. The correlation function is characterized by a power coefficient n ranging from 1 to 2, where 1 represents a Gaussian height distribution and 2 represents an exponential height distribution. The periodicity and random components of the soil surface roughness are schematically shown in Figures 1a and 1b.
In terms of the mean surface height and the second moment , the rms height is represented by:
(Equation 1)
where z is the surface height in cm.
To determine the correlation length and the correlation function, the surface autocorrelation curve needs to be computed. The surface autocorrelation is a measure of the degree of correlation between the height z(x) at point x and the height z(x+d) at point x + d. The following equation can be used to calculate the autocorrelation curve:
(Equation 2)
Once the autocorrelation curve has been computed, the correlation length can be determined. The correlation length is defined as the distance (d) at which the autocorrelation is less than e1 (ï‚» 0.3678). The computed correlation length can be used to fit the theoretical correlation function to the measured autocorrelation curve by optimizing the power coefficient (n). The correlation function is mathematically represented by:
(Equation 3)
Where L is the correlation length (cm) and n is the power coefficient describing the correlation function, which is dimensionless.
Sampling Strategy
At several sites, several representative locations were selected for roughness sampling. At each sampling location, one roughness picture along the row direction and one in the crossrow direction was taken. In the absence of row structure, the two pictures were taken at perpendicular angles. At some roughness sampling sites, one picture was taken. In other cases, pictures were missing.
Digitizing the Pictures
The commercial program Didger 3 was used to digitize the roughness pictures. Before scanning, the dimensions of the board were identified in Didger 3 using reference points on the board. The soil surface was digitized by taking a height measurement at every 1/2 cm (grid scanning). This scanning method provides a random (or normal) distribution of the surface height, which is required for a correct computation of the rms height. However, with this method of scanning some variation in the surface height is neglected, which could influence the computation of the correlation length.
Calculation of the Roughness Parameters
The roughness parameters were calculated using a simple spreadsheet program. Because of the variability in x increment of the digitized surface, the surface was resampled to the nearest 1 mm. The root mean square error was then calculated. Correlation length was calculated as the length at which the autocorrelation function is equal to e1. The power coefficient was determined by visual comparison of the autocorrelation curves and idealized power curves with some guidance by the root mean square error between the curves.
In regards to the placement of the measurement equipment in the field, human error is possible.
The roughness parameters are probably the most unreliable parameter in the process of soil moisture retrieval using microwave remote sensing. The first problem is that the scattering characteristics of natural surfaces are very complex and are still not completely understood; this makes validation of measured roughness parameters very difficult.
Second, the scale at which roughness is measured and the scale at which roughness affects microwave backscatter and emission are not the same. The typical resolution of microwave instruments is around or above ten meters, while the grid board is only one meter long. The values of the rms height and the correlation length (L) differ at each scale.
References and Related Publications
Contacts and Acknowledgments
Michael H. Cosh, Rajat Bindlish
United States Department of Agriculture  Agricultural Research Service (USDA ARS)
Hydrology and Remote Sensing Laboratory
10300 Baltimore Avenue
Bldg. 007, Rm. 104
BARCWest
Beltsville, MD 20705
Many graduate students and volunteers worked to collect these field photographs. We would like to thank the Soil Moisture Active Passive Science Team. Thanks to those who collected and analyzed the data, including Rajat Bindlish and Joanna Birch. We would also like to thank the National Aeronautics and Space Administration for their generous contributions to the study.
Document Information
DOCUMENT CREATION DATE
June 2015
DOCUMENT REVISION DATE
N/A
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