Simulated Geophysical Noise in Sea Ice Concentration Estimates of Open Water and Snow-Covered Sea Ice
Rasmus Tonboe, Vishnu Nandan, Marko Mäkynen, Leif Toudal Pedersen, Stefan Kern, Thomas Lavergne, Johanne Øelund, Gorm Dybkjær, Roberto Saldo, Marcus Huntemann
Abstract
Sea ice concentration algorithms using brightness temperatures (<i>T<sub>B</sub></i>) from satellite microwave radiometers are used to compute sea ice concentration (<i>c<sub>ice</sub></i>), sea ice extent, and generate sea ice climate data records (CDRs). Therefore, it is important to minimize the sensitivity of <i>c<sub>ice</sub></i> estimates to geophysical noise caused by snow/sea ice thermal microwave emission signature variations, and presence of water vapor and clouds in the atmosphere and/or near-surface winds. In this study, we investigate the effect of geophysical noise leading to systematic <i>c<sub>ice</sub></i> biases and affecting <i>c<sub>ice</sub></i> standard deviations (STD) using simulated top of the atmosphere (TOA) <i>T<sub>B</sub></i>s over open water and 100 % sea ice. We consider three case studies for the Arctic and the Antarctic and eight different <i>c<sub>ice</sub></i> algorithms, representing different families of algorithms based on the selection of channels and methodologies. Our simulations show that, over open water and low <i>c<sub>ice</sub></i>, algorithms using gradients between V-polarized 19 GHz and 37 GHz <i>T<sub>B</sub></i>s shows the lowest sensitivity to the geophysical noise, while the algorithms exclusively using near 90 GHz channels have by far the highest sensitivity. Over sea ice, the atmosphere plays a much smaller role than over open water and the <i>c<sub>ice</sub></i> STD for all algorithms is smaller than over open water. The hybrid and low frequency (6 GHz) algorithms have the lowest sensitivity to noise over sea ice, while the polarization type of algorithms have the highest noise levels.