Historical Nansen Cast Temperature Profiles and the Ocean Heat Content 1 Change since 19 th Century 2

Improved Global Ocean Heat Content Estimation by Modeling Vertical Spatio-Temporal Dependence

Estimating ocean heat content (OHC) with reliable uncertainties is critical for understanding and monitoring the evolution of Earth's climate, as the ocean has stored most of the energy accumulated in the climate system due to Earth Energy Imbalance. Here, we use Argo profiling float data from 2004-2022 to map OHC. As...

Observations of seawater temperature and salinity as the main source of information on large-scale ocean currents

Abstract A. S. Sarkisyan developed a diagnostic method in the 1960s, based on the inclusion of annual mean temperature and salinity fields in circulation models, which made it possible to simulate climatic currents in the World Ocean and a number of other marine basins. As observations of seawater temperature and salin...

Marine Heatwaves and NAO-Related Ocean–Atmosphere Variability in the North Atlantic

Increasing greenhouse gas concentrations are placing severe pressure on the Earth system, particularly on the ocean, which plays a vital role in carbon and heat uptake, and overall climate regulation. Consequently, the ocean is experiencing an accelerated warming, leading to an increase in the occurrence of extreme sea...

The Vertical Structure of the Temperature Field and the Spatial Distribution of the Dispersion of Temperature Fluctuations in the Global Ocean on Synoptic Scales

Orographic Quantitative Precipitation Forecast Sensitivity to the Choice of Microphysics Parameterization during a U.S.West Coast Atmospheric River Event

The Center for Western Weather and Water Extremes provides high-resolution forecasts of Atmospheric Rivers (ARs) along the U.S. West Coast. Using a 34-year reforecast dataset, we assess the sensitivity of orographic quantitative precipitation forecasts (QPF) associated with ARs to bulk microphysics parameterization (...

Regions of extremes of decadal surface temperature trends in 1900-1970

Surface layer temperature changes occur on various time scales: interannual, decadal, secular. Decades and longer periods are the most important time scales for studying gradual changes in mean hydrometeorological values. This paper is dedicated to assessing the spatial distribution of decadal trends in mean annual sur...