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The Role of Convective Intensity in Modulating the Earth's Radiative Balance (Data)

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NIAID Data Ecosystem2026-05-02 收录
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https://zenodo.org/record/14796434
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README for datasets used in Pilewskie and L'Ecuyer, 2025, "The Role of Convective Intensity in Modulating the Earth's Radiative Balance", Journal of Climate tropicsCO_v2_06to16_110624.csv: Contains tropical oceanic Convective Objects (COs) and their properties identified using CloudSat and CALIPSO observations Conditions for COs that are stored: Convective fraction (number of convective precipitation profiles / number of all precipitation profiles in CO) > 0.2 Freezing level > 2 km relative Center of Gravity (rCoG) - Freezing level > 1 km Mean latitude and longitude of CO is located where the product between the convective core length and rCoG is the largest anvil_cod_iwp_cre_06to16_040424.csv: CloudSat 2B-FLXHR-LIDAR shortwave (SW) cloud optical depth (COD) summed over convective object anvils only profiles Top-of-atmosphere SW, longwave (LW), and net cloud radiative effects (CREs) of each convective object anvil profile Three files containing the number of CloudSat overpasses within 8 degree x 2 degree grid boxes separated daytime-only ('Day'), nighttime-only ('Night'), and combined day and night ('Day_and_Night'): CSat_overpasses_8x2_Day_06to11.csv CSat_overpasses_8x2_Night_06to11.csv CSat_overpasses_8x2_Day_and_Night_06to11.csv
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2025-02-03
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