We observed an unexpected correlation between structural type and the total number of projections studied for a cortical area (comprising projections found to be absent as well as projections found to be present) (ρ = −0.40, p < 0.01).
John Sterman, director of the MIT Sloan Sustainability Initiative, said the new emissions projection study, which he wasn't involved in, was "sound" in its conclusions.
Future projection studies such as those investigating changes in clouds and tropical cyclone activities are also investigated.
The evolution of the rupture speed down-dip from the hypocenter is also constrained by back-projection studies.
We thus conclude with a cautionary note on the inference of frequency-dependent source properties from low-frequency back-projection studies.
These additional source regions extend the area of the earthquake farther south and north than the region that has been imaged by other back-projection studies.
To address this challenge, the present study introduced a novel method to normalize the results from projection studies according to different baseline and projection periods and climate scenarios, thereby facilitating comparison and synthesis.
Motivated by this interesting observation, back-projection studies extended to intermediate frequencies, down to about 0.1 Hz, have suggested that a progressive transition of rupture properties as a function of frequency is observable.
In the highest frequency band (0.5 1 Hz), the artifact is smaller and the beamforming images are roughly consistent with the MUSIC estimates, which explain the overall agreement of high-frequency back-projection studies.
The along-dip frequency dependent slip migration observed in previous back-projection studies is based on the USArray data (Koper et al., 2011a; Mori, 2011; Yao et al., 2011).
