Mechanisms for European summer temperature response to solar forcing over the last millennium

from Navarro-González (4), these results have been rein- terpreted and chlorinated compounds could have been the product of the reaction of perchlorates identified by Phoe- nix

In this application the whole population is used for the determination of seasonal patterns and forecast errors, but we recur to stratified sampling to

Because of the time scales associated with PA development, it is unlikely that the time evolution of PA's results from direct anomalous thermal forcing associated

(A and B) Two example behavior sessions: each showing the movement of the animal over time (top two rows, showing running position and running speed) compared with the

The Atlantic Meridional Overturning Circulation (AMOC) shows a significant intensification 5 to 10 years after the eruptions of the period post-1400 A.D., in response to

Multi-decadal to centennial hydro-climate variability and linkage to solar forcing in the Western Mediterranean during the last 1000

Based on the recent remote sensing tools in conjunction with meteorological observations and models, we conclude on the three essential processes that control the O 3 concen-

The damping of LWCRF caused by the increased atmospheric water vapor loading and presence of large amount of high clouds over the Indian region during the summer monsoon season