Datasets for origins of Southern Ocean warm sea surface temperature bias in CMIP6 models

NIAID Data Ecosystem2026-05-01 收录

气候模型偏差

南大洋海温偏差

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https://zenodo.org/record/8219809 数据链接链接失效反馈

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Datasets for origins of Southern Ocean warm sea surface temperature bias in CMIP6 models

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2023-08-08

Data for: Connecting hemispheric asymmetries of planetary albedo and surface temperature

行星反照率不对称性

气候模型偏差

Satellite measurements show that the Northern and Southern hemispheres reflect equal amounts of short-wave radiation (“albedo symmetry”), but no theory exists on if, how, and why the symmetry is estab

NIAID Data Ecosystem90

Contrasting impacts of radiative forcing in the Southern Ocean versus...

气候模型偏差

南大洋辐射强迫

Most current climate models suffer from pronounced cloud and radiation biases in the Southern Ocean (SO) and in the tropics. Using one GFDL climate model, this study...

DASH Search60

DISTENDER Climate Simulations: Statistical Downscaling for CMTo_D1, Vertical level 10m, Global model CanESM5, scenario ssp370 - The Metropolitan City of Turin (CMTo, Italy)

区域气候降尺度

气候模型偏差

Local (high resolution) climate data produced applying statistical downscaling techniques in the EU Project DISTENDER for five case studies. https://distender.eu/the-project . The datasets from the st

Zenodo2025-11-28 更新40

The role of surface shortwave flux correction in reducing climatological temperature biases

气候模型偏差

海表温度模拟优化

Coupled ocean-atmosphere climate models suffer from a number of climatological biases in sea surface temperature (SST) such as the cold tongue bias in the tropical Pacific, and warm biases along easte

Zenodo2019-11-12 更新60

Climate model biases and El Niño Southern Oscillation (ENSO) simulation US CLIVAR Variations

ENSO厄尔尼诺-南方涛动

气候模型偏差

Over the last two decades the representation of ENSO in climate models has significantly improved, as documented by the extensive literature describing ENSO simulations in the Climate Model Intercompa

NOAA Institutional Repository2021-10-26 更新50

Datasets for origins of Southern Ocean warm sea surface temperature bias in CMIP6 models

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