Robert Tardif

TL;DR: In this article, the authors summarized past achievements related to the understanding of fog formation, development and decay, and in this respect, the analysis of observations and the development of forecasting models and remote sensing methods are discussed in detail.

TL;DR: In this article, the authors use linear, univariate forward models (PSMs) that map climate variables to proxy measurements by fitting proxy data to 2m air temperature from gridded instrumental temperature data; the linear PSMs are then used to predict proxy values from the prior estimate.

TL;DR: In this paper, the authors investigated the character of fog in a region centered on New York City, New York using 20 years of historical data and used hourly surface observations to identify fog events at 17 locations under the influence of various physiographic features, such as landwater contrasts, land surface character (urban, suburban, and rural), and terrain.

TL;DR: In this paper, a proxy-constrained, full-field reanalysis of surface temperature change spanning the Last Glacial Maximum to present at 200-year resolution is presented.

TL;DR: The Last Millennium Reanalysis (LMR) as discussed by the authors utilizes an ensemble methodology to assimilate paleoclimate data for the production of annually resolved climate field reconstructions of the Common Era.