The Southern Ocean has absorbed most of the excess heat associated with anthropogenic greenhouse gas emissions. Since observations are sparse in certain regions and seasons, much our knowledge ocean uptake is based on climate model simulations. However, models still inadequately represent some properties clouds, they have not identified mechanisms by which clouds may affect (SOHU). Here, we use...

Abstract. In this study, we analyse the role of climate change in forest fires that raged through large parts Sweden summer 2018 from a meteorological perspective. This is done by studying Canadian Fire Weather Index (FWI) based on sub-daily data, both reanalysis data sets (ERA-Interim, ERA5, Japanese 55 year Reanalysis, JRA-55, and Modern-Era Retrospective analysis for Research Applications ve...

An abstract is not available for this content so a preview has been provided. As you have access to content, full PDF via the ‘Save PDF’ action button.

An abstract is not available for this content so a preview has been provided. As you have access to content, full PDF via the ‘Save PDF’ action button.

In this paper, Japan Meteorological Agency (JRA-55) reanalysis and observational rainfall datasets from the National Climate Center (NCC) of China, as well satellite Tropical Rainfall Measuring Mission (TRMM), Global Precipitation Climatology Project (GPCP), International Satellite Cloud (ISCCP), are used. The correlation coefficient fast Fourier transform (FFT) low-pass filter also used, in or...

An abstract is not available for this content so a preview has been provided. As you have access to content, full PDF via the ‘Save PDF’ action button.

An abstract is not available for this content so a preview has been provided. As you have access to content, full PDF via the ‘Save PDF’ action button.

An abstract is not available for this content so a preview has been provided. As you have access to content, full PDF via the ‘Save PDF’ action button.

Rises in surface and lower troposphere air temperatures through the 21st century are projected to be especially pronounced over the Arctic Ocean during the cold season. This Arctic amplification is largely driven by loss of the sea ice cover, allowing for strong heat transfers from the ocean to the atmosphere. Consistent with observed reductions in sea ice extent, fields from both the NCEP/NCAR...