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Clement Guilloteau
,
Efi Foufoula-Georgiou
,
Pierre Kirstetter
,
Jackson Tan
, and
George J. Huffman

. 3 , right column). Two-dimensional space–time PSDs are commonly used in climate and Earth science to analyze the propagation of atmospheric and oceanic waves along longitudes ( Wheeler and Kiladis 1999 ; Lin et al. 2006 ; Orbe et al. 2020 ). The left half of the PSD (negative wavelengths) corresponds to eastward propagating waves and the right half (positive wavelengths) corresponds to westward propagating waves. The two-dimensional space–time PSD shows the energy of the eastward and westward

Open access
Andrea Camplani
,
Daniele Casella
,
Paolo Sanò
, and
Giulia Panegrossi

://pmm.nasa.gov/sites/default/files/document_files/CSATGPM_COIN_ATBD.pdf . Walker , A. E. , and B. E. Goodison , 1993 : Discrimination of a wet snow cover using passive microwave satellite data . Ann. Glaciol. , 17 , 307 – 311 , https://doi.org/10.3189/S026030550001301X . 10.3189/S026030550001301X Wang , D. , and Coauthors , 2017 : Surface emissivity at microwaves to millimeter waves over polar regions: Parameterization and evaluation with aircraft experiments . J. Atmos. Oceanic Technol. , 34 , 1039 – 1059 , https://doi.org/10.1175/JTECH-D-16-0188.1 . 10

Open access