Atmospheric and Surface Contributions to Planetary Albedo
By A. Donohoe, D. Battisti. 2011
171 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/daaa8afaf5305e94b48fd2c5fdbee4edb315b444
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- David Ferreira
- John Marshall
- Jun Yang
- Gwenaël Boué
- David McGee
- D. Fabrycky
- Dorian S. Abbot
- A. Donohoe
In Global and Planetary Change
- David Ferreira
- John Marshall
- David McGee
- Jun Yang
- Gwenaël Boué
- D. Fabrycky
- Dorian S. Abbot
- A. Donohoe
Citations in the corpus
- STRONG DEPENDENCE OF THE INNER EDGE OF THE HABITABLE ZONE ON PLANETARY ROTATION RATE (2014, background): “Cloud reflection of solar radiation is responsible for most of the planetary albedo on modern Earth (Donohoe & Battisti 2011), and clouds also significantly increase Earth’s greenhouse effect by absorbing terrestrial infrared emis- Correspondence: abbot@uchicago.edu sion (Harrison et al. 1990).”
- The ocean’s role in setting the mean position of the Inter-Tropical Convergence Zone (2013, methodology): “We can gain insight into the role of cloud and surface reflection in setting the hemispheric contrast of absorbed shortwave radiation by partitioning the planetary albedo between surface and atmospheric reflection via the method of Donohoe and Battisti (2011).”