Here is the situation in the Northern Hemisphere:The following is a post from a popular meteorologist (who pushes global warming) noting the cold recorded today anomalies in South America and Australia:

And from a different map projection:

Because of map distortions, that makes the area of the equator look smaller than it really is, it is not straightforward to say what the overall balance is of heat vs cold. A guess is that it looks like the anomaly is on the warm side, at least in the Northern Hemisphere. If that is so, the air can hold more humidity. When the air then is carried north, it cools down, the relative humidity goes up and water vapour condenses to give rise to precipitation in the form of mostly rain or snow. Is that the reason why:
Greenland keeps adding
One location, where the precipitation has been on the plus side since September 1st, is Greenland, as seen in the latest map of the surface mass balance: Surface Conditions: Polar Portal

For Antarctica, I could not find a similar model. The advantage of Greenland is its smaller size, which facilitates surveys. There was however a study, published in 2017 by Elizabeth R. Thomas et al, that based on a number of ice cores modelled the development of the surface mass balance of the Antarctic ice sheet over the last 1000 years. It may have been mentioned already, but I could not find it, so here is the abstract:
Coming back to the Northern Hemisphere, the Sea Ice is still thereRegional Antarctic snow accumulation over the past 1000 years
DOI:10.5194/cp-13-1491-2017
- November 2017
- Climate of the Past 13(11):1491-1513
Here we present Antarctic snow accumulation variability at the regional scale over the past 1000 years. A total of 79 ice core snow accumulation records were gathered and assigned to seven geographical regions, separating the high-accumulation coastal zones below 2000 m of elevation from the dry central Antarctic Plateau. The regional composites of annual snow accumulation were evaluated against modelled surface mass balance (SMB) from RACMO2.3p2 and precipitation from ERA-Interim reanalysis. With the exception of the Weddell Sea coast, the low-elevation composites capture the regional precipitation and SMB variability as defined by the models. The central Antarctic sites lack coherency and either do not represent regional precipitation or indicate the model inability to capture relevant precipitation processes in the cold, dry central plateau. Our results show that SMB for the total Antarctic Ice Sheet (including ice shelves) has increased at a rate of 7 ± 0.13 Gt decade⁻¹ since 1800 AD, representing a net reduction in sea level of ∼ 0.02 mm decade⁻¹ since 1800 and ∼ 0.04 mm decade⁻¹ since 1900 AD. The largest contribution is from the Antarctic Peninsula (∼ 75 %) where the annual average SMB during the most recent decade (2001–2010) is 123 ± 44 Gt yr⁻¹ higher than the annual average during the first decade of the 19th century. Only four ice core records cover the full 1000 years, and they suggest a decrease in snow accumulation during this period. However, our study emphasizes the importance of low-elevation coastal zones, which have been under-represented in previous investigations of temporal snow accumulation.
Sea Ice Thickness and Volume: Polar Portal

Sea Ice Extent: Polar Portal

Checking up on the Northern Sea Route, there has been little news since May, after trade between Russia and the West became more difficult. But judging from the map, if there is 1,5-2 meter ice in the eastern area above Siberia, already now, it might not have been as easy a year as many of the previous years.