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insolation only simulation  (Kemper GmbH)
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Kemper GmbH insolation only simulation
Spectral comparisons of EAM proxy records with global ice volume, greenhouse gases, and <t>insolation.</t> Local δ 18 O sw , a record for which the effects of temperature and seawater δ 18 O have been removed, compared to a global CH 4 , b global CO 2 , and c global ice volume. δ 18 O cave , a record for which the effects of temperature and seawater δ 18 O have not been removed, compared to d local summer and e high-latitude summer-insolation forcing. Labeled lines denote primary orbital frequencies (frequency = 1/period in ky)
Insolation Only Simulation, supplied by Kemper GmbH, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/insolation+only+simulation/pmc06105601-217-10-27?v=Kemper+GmbH
Average 90 stars, based on 1 article reviews
insolation only simulation - by Bioz Stars, 2026-08
90/100 stars
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Spectral comparisons of EAM proxy records with global ice volume, greenhouse gases, and insolation. Local δ 18 O sw , a record for which the effects of temperature and seawater δ 18 O have been removed, compared to a global CH 4 , b global CO 2 , and c global ice volume. δ 18 O cave , a record for which the effects of temperature and seawater δ 18 O have not been removed, compared to d local summer and e high-latitude summer-insolation forcing. Labeled lines denote primary orbital frequencies (frequency = 1/period in ky)

Journal: Nature Communications

Article Title: Precession-band variance missing from East Asian monsoon runoff

doi: 10.1038/s41467-018-05814-0

Figure Lengend Snippet: Spectral comparisons of EAM proxy records with global ice volume, greenhouse gases, and insolation. Local δ 18 O sw , a record for which the effects of temperature and seawater δ 18 O have been removed, compared to a global CH 4 , b global CO 2 , and c global ice volume. δ 18 O cave , a record for which the effects of temperature and seawater δ 18 O have not been removed, compared to d local summer and e high-latitude summer-insolation forcing. Labeled lines denote primary orbital frequencies (frequency = 1/period in ky)

Article Snippet: The experiment consisted of three separate simulations, beginning with an insolation only simulation, followed by addition of greenhouse gasses, followed by addition of ice-volume and sea level (Fox-Kemper et al., manuscript in preparation).

Techniques: Labeling