Add to ORKGThe sparse observational network over the Arctic region makes severe storms such as polar lows (PLs)...
Four basic types of synoptic-scale conditions describe the atmospheric structure and variability obs...
Polar lows (PLs) are intense mesoscale weather systems that often cause severe storm winds in the No...
Polar lows are intense meso-α-scale cyclones that develop over the oceans poleward of the main baroc...
Polar lows are intense meso-α-scale cyclones that develop over the oceans poleward of the main baroc...
Polar lows are intense meso- a -scale cyclones that develop over the oceans poleward of the main b...
Polar lows are subsynoptic-scale cyclones that develop poleward of the main polar front over the oce...
Polar lows are subsynoptic-scale cyclones that develop poleward of the main polar front over the oce...
Polar lows are small, but extreme cyclones that develop in marine polar air mass. They feature one o...
Conditions for polar low development are not clearly understood. Polar lows were identified using hi...
Conditions for polar low development are not clearly understood. Polar lows were identified using hi...
Conditions for polar low development are not clearly understood. Polar lows were identified using hi...
In East Asia, a strong winter monsoon and high baroclinicity cause enhanced cyclone activity, which ...
The 11th Symposium on Polar Science/Ordinary sessions: [OM] Polar Meteorology and Glaciology, Poster...
Here we present an objective global climatology of polar lows. In order to obtain objective detectio...
The sparse observational network over the Arctic region makes severe storms such as polar lows (PLs)...
Four basic types of synoptic-scale conditions describe the atmospheric structure and variability obs...
Polar lows (PLs) are intense mesoscale weather systems that often cause severe storm winds in the No...
Polar lows are intense meso-α-scale cyclones that develop over the oceans poleward of the main baroc...
Polar lows are intense meso-α-scale cyclones that develop over the oceans poleward of the main baroc...
Polar lows are intense meso- a -scale cyclones that develop over the oceans poleward of the main b...
Polar lows are subsynoptic-scale cyclones that develop poleward of the main polar front over the oce...
Polar lows are subsynoptic-scale cyclones that develop poleward of the main polar front over the oce...
Polar lows are small, but extreme cyclones that develop in marine polar air mass. They feature one o...
Conditions for polar low development are not clearly understood. Polar lows were identified using hi...
Conditions for polar low development are not clearly understood. Polar lows were identified using hi...
Conditions for polar low development are not clearly understood. Polar lows were identified using hi...
In East Asia, a strong winter monsoon and high baroclinicity cause enhanced cyclone activity, which ...
The 11th Symposium on Polar Science/Ordinary sessions: [OM] Polar Meteorology and Glaciology, Poster...
Here we present an objective global climatology of polar lows. In order to obtain objective detectio...
The sparse observational network over the Arctic region makes severe storms such as polar lows (PLs)...
Four basic types of synoptic-scale conditions describe the atmospheric structure and variability obs...
Polar lows (PLs) are intense mesoscale weather systems that often cause severe storm winds in the No...