Current methods for quantification of differences between scRNA-seq datasets collected in multiple conditions focus on discrete regions of the transcriptional state space such as clusters of cells. He
The Soil Moisture Active Passive (SMAP) mission has greatly contributed to the use of remote sensing technologies for observing the Earth’s land surface and estimating geophysical parame-ters that inf
LPC coefficient of the histograms, each column is a vector of 300 elements, which contain the LPC coefficients of calculated from the YUV, 100 histograms for each colour histogram.
Remote sensing technologies, such as radiometry radar or synthetic-aperture radar (SAR) provide satellite ob- servations with different spatio-temporal resolutions. Some of these observations can be c