Evaluation the MOD10A1 daily snow albedo product (v. 6) on Livingston Island, Antarctica
- 1Remote Sensing Applications (RSApps) Research Group, Department of Mining Exploitation and Prospecting, University of Oviedo. Polytechnic School of Mieres, C/ Gonzalo Gutiérrez Quirós s/n, 33600 Mieres, Asturias, Spain (corbeaalejandro@uniovi.es)
- 2Remote Sensing Applications (RSApps) Research Group, Department of Physics, University of Oviedo. Polytechnic School of Mieres, C/ Gonzalo Gutiérrez Quirós s/n, 33600 Mieres, Asturias, Spain
- 3Department of Geology, University of Oviedo. Campus de Oviedo (Llamaquique), C/ Jesús Arias de Velasco s/n, 33005 Oviedo, Asturias, Spain
One of the factors that can most influence climate changes on a global scale is the albedo decrease, associated with a temperature increase and a snow cover decrease, mainly in the polar areas, where the remote sensing data are essential because there is much difficulty access to obtain measurements in situ. Therefore, evaluations of satellite measurements are essential.
The daily MOD10A1 snow product provides daily measurements of albedo. Version 6 is currently available. In Antarctica, and more specifically on Livingston Island (South Shetland Archipelago), where one of the Spanish Antarctic bases is located, the daily snow albedo product of MODIS (MOD10A1) has been evaluated using version 5 data (Calleja et al. 2019). However, several authors have recommended updating the analyses based on version 6 data (Box et al. 2012, Casey et al. 2017), as they are more accurate.
In this work, we have analyzed the albedo behavior using MOD10A1 version 6 data between 2006 and 2015 and we have seen an increasing trend of albedo. Version 5 showed an increase of 0.07 per decade. However, version 6 data show less variability (0.04 per decade), and its results are closer to those obtained in the measurements in situ (0.03 per decade). In addition, the results obtained allow us to affirm that the MOD10A1 daily albedo product (v. 6) can be used to determine the albedo in the study area.
References:
Box, J. E., Fettweis, X., Stroeve, J. C., Tedesco, M., Hall, D. K., & Steffen, K. (2012). Greenland ice sheet albedo feedback: thermodynamics and atmospheric drivers. The Cryosphere, 6(4), 821-839.
Calleja, J. F., Corbea-Pérez, A., Fernández, S., Recondo, C., Peón, J., & de Pablo, M. Á. (2019). Snow Albedo Seasonality and Trend from MODIS Sensor and Ground Data at Johnsons Glacier, Livingston Island, Maritime Antarctica. Sensors, 19(16), 3569.
Casey, K. A., Polashenski, C. M., Chen, J., & Tedesco, M. (2017). Impact of MODIS sensor calibration updates on Greenland Ice Sheet surface reflectance and albedo trends. The Cryosphere, 11(4), 1781-1795.
How to cite: Corbea-Pérez, A., Fernández-Calleja, J., Recondo, C., and Fernández, S.: Evaluation the MOD10A1 daily snow albedo product (v. 6) on Livingston Island, Antarctica, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7530, https://doi.org/10.5194/egusphere-egu2020-7530, 2020.
