Principal data and analysis code from Riihelä et al (2021): Antarctic sea ice loss drives cryospheric radiative feedback strengthening in recent years, submitted to Nature Geoscience, 2021

This entry contains the principal data of the associated publication - the annual global mean radiative feedbacks resulting from surface albedo changes over both polar regions (poleward of 50 degrees latitude). Data are available based on CLARA-A2.1 surface albedo data record combined with two radia...

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Bibliographic Details
Main Authors: Riihelä, Aku, Bright, Ryan M., Anttila, Kati
Format: Article in Journal/Newspaper
Language:unknown
Published: https://b2share.eudat.eu 2021
Subjects:
3.3 → Natural sciences → Earth sciences
cryospheric radiative feedback
climate feedbacks
surface albedo
radiative kernel applications
Antarctic
Riihelä
Antarc*
Sea ice
Online Access:https://dx.doi.org/10.23728/fmi-b2share.3a345c1121cf41f781ba237b8fddf294
https://fmi.b2share.csc.fi/records/3a345c1121cf41f781ba237b8fddf294
Description
Summary:This entry contains the principal data of the associated publication - the annual global mean radiative feedbacks resulting from surface albedo changes over both polar regions (poleward of 50 degrees latitude). Data are available based on CLARA-A2.1 surface albedo data record combined with two radiative kernels; CloudSat-CALIPSO (CC) and CERES-based albedo change kernel (CACK). Upper and lower limits of estimated radiative feedback uncertainty envelopes are provided in the data file. The entry also provides the principal python codes used in the study. These codes are provided as-is.

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