Abstract

Spectroradiometric satellite observations of the ocean are commonly referred to as “ocean color” remote sensing. NASA has continuously collected, processed, and distributed ocean color datasets since the launch of the Sea-viewing Wide-field-of-view Sensor (SeaWiFS) in 1997. While numerous ocean color algorithms have been developed in the past two decades that derive geophysical data products from sensor-observed radiometry, few papers have clearly demonstrated how to estimate measurement uncertainty in derived data products. As the uptake of ocean color data products continues to grow with the launch of new and advanced sensors, it is critical that pixel-by-pixel data product uncertainties are estimated during routine data processing. Knowledge of uncertainties can be used when studying long-term climate records, or to assist in the development and performance appraisal of bio-optical algorithms. In this methods paper we provide a comprehensive overview of how to formulate first-order first-moment (FOFM) calculus for propagating radiometric uncertainties through a selection of bio-optical models. We demonstrate FOFM uncertainty formulations for the following NASA ocean color data products: chlorophyll-a pigment concentration (Chl), the diffuse attenuation coefficient at 490 nm (Kd,490), particulate organic carbon (POC), normalized fluorescent line height (nflh), and inherent optical properties (IOPs). Using a quality-controlled in situ hyperspectral remote sensing reflectance (Rrs,i) dataset, we show how computationally inexpensive, yet algebraically complex, FOFM calculations may be evaluated for correctness using the more computationally expensive Monte Carlo approach. We compare bio-optical product uncertainties derived using our test Rrs dataset assuming spectrally-flat, uncorrelated relative uncertainties of 1, 5, and 10%. We also consider spectrally dependent, uncorrelated relative uncertainties in Rrs. The importance of considering spectral covariances in Rrs, where practicable, in the FOFM methodology is highlighted with an example SeaWiFS image. We also present a brief case study of two POC algorithms to illustrate how FOFM formulations may be used to construct measurement uncertainty budgets for ecologically-relevant data products. Such knowledge, even if rudimentary, may provide useful information to end-users when selecting data products or when developing their own algorithms.

Highlights

  • National Aeronautics and Space Administration (NASA) has continually collected, processed, archived, and distributed global ocean color data since the launch of the Seaviewing Wide Field-of-View Sensor (SeaWiFS) in 1997

  • In this paper we demonstrated a FOFM-based method for estimating uncertainties in a selection of NASA OC and IOP products, namely: Chl, Kd,490, POC, nflh, anw,440, aφ,440, adg,440, and bbp,440, due to sensor-observed radiometric uncertainty

  • Using a high quality hyperspectral Rrs dataset subsampled to our target wavelengths, we first appraised the FOFM methodology by comparing FOFM-derived uncertainty estimates with uncertainties estimated from MC simulations with an assumed relative spectrally flat, uncorrelated uncertainty in Rrs of 5%

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Summary

Introduction

NASA has continually collected, processed, archived, and distributed global ocean color data since the launch of the Seaviewing Wide Field-of-View Sensor (SeaWiFS) in 1997. This two decades-long multi-sensor data climatology continues to provide unprecedented synoptic-scale insight into near-surface oceanographic processes. Following formal definitions outlined in the Guide to Uncertainty in Measurement (JCGM, 2008), we can outline the objective of ocean color remote sensing as, to measure oceanographic quantities or measurands. We note that the measurement procedure involves a number of mathematical steps and assumptions that derive the measurand from sensorobserved top-of-atmosphere radiances. A derived ocean color data product is a result of measurement and should always be treated as an estimate of the measurand which has inherent uncertainty

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