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Matias Takala

Researcher at Finnish Meteorological Institute

Publications -  55
Citations -  1422

Matias Takala is an academic researcher from Finnish Meteorological Institute. The author has contributed to research in topics: Snow & Snowmelt. The author has an hindex of 13, co-authored 52 publications receiving 1009 citations.

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Estimating northern hemisphere snow water equivalent for climate research through assimilation of space-borne radiometer data and ground-based measurements

TL;DR: In this paper, an algorithm assimilating synoptic weather station data on snow depth with satellite passive microwave radiometer data is applied to produce a 30-year-long time-series of seasonal snow water equivalent (SWE) for the northern hemisphere.
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Patterns and trends of Northern Hemisphere snow mass from 1980 to 2018.

TL;DR: Applying a bias correction to a state-of-the-art dataset covering non-alpine regions of the Northern Hemisphere and to three other datasets yields a more constrained quantification of snow mass in March from 1980 to 2018, enabling a better estimation of the role of seasonalSnow mass in Earth's energy, water and carbon budgets.
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Artificial neural network-based techniques for the retrieval of SWE and snow depth from SSM/I data

TL;DR: In this article, the retrieval of snow water equivalent (SWE) and snow depth is performed by inverting Special Sensor Microwave Imager (SSM/I) brightness temperatures at 19 and 37 GHz using artificial neural network ANN-based techniques.
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Detection of Snowmelt Using Spaceborne Microwave Radiometer Data in Eurasia From 1979 to 2007

TL;DR: The novelty here is the demonstration and validation of estimates for a large continental scale (for areas dominated by boreal forests) using extensive reference data sets for a nearly 30-year period.
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Early snowmelt significantly enhances boreal springtime carbon uptake

TL;DR: A proxy indicator for spring recovery from in situ flux data on CO2 exchange and recent satellite snowmelt products is developed and a relation between spring recovery and carbon uptake is established to assess changes in springtime carbon exchange showing a major advance in the CO2 sink.