High moisture confluence in Japan Sea polar air mass convergence zone captured by hourly radiosonde launches from a ship.

Some of the heaviest snowfalls in urban areas in the world occur in Japan, particularly in regions that face the Japan Sea. Many heavy snowfalls are produced by a Japan Sea polar air mass convergence zone (JPCZ), which is an atmospheric river-like cloud zone that forms when Siberian cold air flows over the warm Japan Sea. Quantifying how the air-sea interaction strengthens the JPCZ is key to snowfall prediction. However, until our observations with hourly meteorological balloon launches from a training vessel in 2022, no simultaneous air-sea observations targeting the JPCZ had been conducted. Our observations showed that wind direction shifted drastically by about 90 degrees from the surface to an altitude of about 3.5 km within a narrow horizontal range of about 15 km, indicating airflow convergence from the surroundings. Maximum temperature difference between surface air (3 °C) and water was 11 °C near the JPCZ centre with 17 m s-1 wind speed. Large amounts of heat, 718 W m-2, was thus gained from the warm sea. Water vapour was also concentrated by the horizontal convergence, which caused heavy snow, equivalent to 100 cm of snowfall in 7 h. The surrounding sea greatly affects moisture formation within the JPCZ.

Author Correction: Warm hole in Pacific Arctic sea ice cover forced mid-latitude Northern Hemisphere cooling during 2017-18.

An amendment to this paper has been published and can be accessed via a link at the top of the paper.

Warm hole in Pacific Arctic sea ice cover forced mid-latitude Northern Hemisphere cooling during 2017-18.

In North America and Asia, extreme cold weather characterized the winter of 2017-18. At the same time, the Pacific, the Bering Sea, and the Atlantic Arctic regions experienced anomalously low sea ice extent in the early winter. The jet stream dividing cold Arctic air from warm air deviated from normal zonal patterns northward into the ice-free areas north of the Bering Strait. Large southward jet stream pathways formed over Asia and America, allowing cold air to spread into Asia and the southern areas of North America. We hypothesise that the late autumn Bering Strait sea-ice anomaly and Pacific atmospheric rivers were partially responsible for the cold winter. We used data analyses and numerical experiments to test this hypothesis. We propose a positive feedback mechanism between the sea ice anomaly and atmospheric river activity, with anomalous south winds toward the sea ice anomaly potentially leading to more warm water injected by the wind-driven current through the Bering Strait. Our findings suggest that Poleward propagation of the atmospheric rivers made upper air warm, leading to their upgliding, which further heated the overlying air, causing poleward jet meanders. As a part of this response the jet stream meandered southward over Asia and North America, resulting in cold intrusions. We speculate that the positive feedback mechanism observed during the 2017-18 winter could recur in future years when the sea-ice reduction in the Pacific Arctic interacts with enhanced atmospheric river activity.

Poleward upgliding Siberian atmospheric rivers over sea ice heat up Arctic upper air.

We carried out upper air measurements with radiosondes during the summer over the Arctic Ocean from an icebreaker moving poleward from an ice-free region, through the ice edge, and into a region of thick ice. Rapid warming of the Arctic is a significant environmental issue that occurs not only at the surface but also throughout the troposphere. In addition to the widely accepted mechanisms responsible for the increase of tropospheric warming during the summer over the Arctic, we showed a new potential contributing process to the increase, based on our direct observations and supporting numerical simulations and statistical analyses using a long-term reanalysis dataset. We refer to this new process as "Siberian Atmospheric Rivers (SARs)". Poleward upglides of SARs over cold air domes overlying sea ice provide the upper atmosphere with extra heat via condensation of water vapour. This heating drives increased buoyancy and further strengthens the ascent and heating of the mid-troposphere. This process requires the combination of SARs and sea ice as a land-ocean-atmosphere system, the implication being that large-scale heat and moisture transport from the lower latitudes can remotely amplify the warming of the Arctic troposphere in the summer.

Nucleolin Acts as a Scavenger Receptor for Acetylated Low-Density Lipoprotein on Macrophages.

Although macrophage phagocytoses modified low-density lipoprotein (LDL), excessive accumulation of modified LDL induces macrophage foam cell formation, which is a feature of atherosclerotic plaque. Thus, the identification of scavenger receptor for modified LDL will provide better understanding of an atherosclerotic event. We recently showed that nucleolin expressed on macrophages acts as a scavenger receptor for various endogenous discarded products. Here, we investigated whether or not nucleolin is involved in the uptake of acetylated LDL (AcLDL). In contrast to normal LDL, AcLDL directly bound to immobilized nucleolin. AcLDL exhibited a higher affinity for macrophages than normal LDL. This binding of AcLDL was inhibited by anti-nucleolin antibody and antineoplastic guanine-rich oligonucleotide (AGRO), a nucleolin-specific oligonucleotide aptamer. In addition, AcLDL exhibited a higher affinity for HEK cells transfected with nucleolin than those without. Further, intracellular accumulation of AcLDL was also inhibited by anti-nucleolin antibody. The results of this study suggest that nucleolin expressed on macrophages is a receptor for AcLDL.

Macrophage recognition of toxic advanced glycosylation end products through the macrophage surface-receptor nucleolin.

Advanced glycosylation end-products (AGEs) are non-enzymatically glycosylated proteins that play an important role in several diseases and aging processes, including angiopathy, renal failure, diabetic complications, and some neurodegenerative diseases. In particular, glyceraldehyde (GCA)- and glycolaldehyde (GOA)-derived AGEs are deemed toxic AGEs, due to their cytotoxicity. Recently, the shuttling-protein nucleolin has been shown to possess scavenger receptor-activity. Here, we investigated whether or not macrophages recognize toxic AGEs through nucleolin receptors expressed on their surface. Free amino acid groups and arginine residues found in bovine serum albumin (BSA) were time-dependently modified by incubation with GCA and GOA. In addition, average molecular size was increased by incubation with GCA and GOA. While GCA-treated BSA (GCA-BSA) and GOA-treated BSA (GOA-BSA) were recognized by thioglycollate-elicited mouse peritoneal macrophages in proportion to their respective aldehyde-modification ratios, aldehyde-untreated control-BSA was not. Surface plasmon-resonance analysis revealed that nucleolin strongly associated with GCA-BSA and GOA-BSA, but not with control-BSA. Further, pretreating macrophages with anti-nucleolin antibody, but not control-Immunoglobulin G, inhibited recognition of GCA-BSA and GOA-BSA by macrophages. Additionally, AGRO, a nucleolin-specific oligonucleotide aptamer, inhibited recognition of GCA-BSA and GOA-BSA. Moreover, nucleolin-transfected HEK293 cells recognized more GCA-BSA and GOA-BSA than control HEK cells did. Binding of nucleolin and GCA-BSA/GOA-BSA was also blocked by anti-nucleolin antibody at molecular level. These results indicate that nucleolin is a receptor that allows macrophages to recognize toxic AGEs.