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Andrew A. Lacis
Researcher at Goddard Institute for Space Studies
Publications - 166
Citations - 29249
Andrew A. Lacis is an academic researcher from Goddard Institute for Space Studies. The author has contributed to research in topics: Climate model & Climate change. The author has an hindex of 73, co-authored 161 publications receiving 27563 citations. Previous affiliations of Andrew A. Lacis include Goddard Space Flight Center & Computer Sciences Corporation.
Papers
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Global Climate Data and Models: A Reconciliation
TL;DR: In their Perspective, Hansen et al. as mentioned in this paper discuss a correction to the satellite data published by Wentz and Schabel in Nature that may have profound implications for discussions of climate change, and conclude that the question now is not whether global warming exists, but what should be done about it.
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Application of spectral analysis techniques in the intercomparison of aerosol data. Part II: Using maximum covariance analysis to effectively compare spatiotemporal variability of satellite and AERONET measured aerosol optical depth
TL;DR: In this article, the authors introduce Maximum Covariance Analysis (MCA), also known as Singular Value Decomposition analysis, as an effective way to compare correlated aerosol spatial and temporal patterns between satellite measurements and AERONET data.
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Assessing Goddard Institute for Space Studies ModelE aerosol climatology using satellite and ground‐based measurements: A comparison study
Li Liu,Li Liu,Andrew A. Lacis,Barbara E. Carlson,Michael I. Mishchenko,Brian Cairns,Brian Cairns +6 more
TL;DR: In this article, Schmidt et al. evaluate the aerosol climatology used in the GISS ModelE by characterizing and comparing the geographic distribution and seasonal variability of aerosol optical depth (AOD) and particle size via Angstrom exponent (A) against available satellite and ground-based measurements, i.e., MODIS, MISR, POLDER, AVHRR and AERONET data.
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Fast atmosphere‐ocean model runs with large changes in CO2
TL;DR: In this article, the authors used a modified coupled atmosphere-ocean model, whose stability was improved so that the model would accommodate large radiative forcings yet be fast enough to reach rapid equilibrium.
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GCM simulations of volcanic aerosol forcing. I - Climate changes induced by steady-state perturbations
TL;DR: In this paper, the response of the climate system to a temporally and spatially constant amount of volcanic particles is simulated using a general circulation model (GCM) and the optical depth of the aerosols is chosen so as to produce approximately the same amount of forcing as results from doubling the present CO2 content of the atmosphere and from the boundary conditions associated with the peak of the last ice age.