A strudel (plural: strudel) is a vertical hole in sea ice through which downward jet-like, buoyancy-driven drainage of flood water is thought to occur.
 This feature is less than a few tens of meters in size and typically occurs within 30 km from a river mouth, in the sea ice expanse that is fastened to the coastline (known as "fast ice").
 Once the water that flooded the ice has completely drained off the ice surface, strudel become recognizable by a radial pattern of feeder channels that lead to the hole.
 They are elongated and irregularly spaced, with the larger ones up to several kilometers apart.
 Their distribution tends to be controlled by weak areas in the ice — in places, they line up along fractures or refrozen extensional cracks.
 The ice sheet where they occur may be 2 m in thickness, at water depths (below the ice) in the order of a few meters.
A laminectomy is a surgical procedure that removes a portion of the vertebral bone called the lamina.
 The back muscles are pushed aside rather than cut and the parts of the vertebra adjacent to the lamina are left intact.
 Recovery typically occurs within a few days.
Cyclone Qendresa (also known as Medicane Qendresa) was one of the most intense Mediterranean tropical-like cyclones on record, which struck Malta and the Italian island of Sicily in 2014.
 The storm formed on 5 November and rapidly intensified on 7 November, due to a cold-core low aloft.
 Qendresa directly hit Malta in the afternoon and then crossed the eastern coast of Sicily on 8 November.
 Later, the cyclone weakened significantly and dissipated over Crete on 11 November.
Athetoid cerebral palsy or dyskinetic cerebral palsy (sometimes abbreviated ADCP) is a type of cerebral palsy primarily associated with damage, like other forms of CP, to the basal ganglia in the form of lesions that occur during brain development due to bilirubin encephalopathy and hypoxic-ischemic brain injury.
 Unlike spastic or ataxic cerebral palsies, ADCP is characterized by both hypertonia and hypotonia, due to the affected individual's inability to control muscle tone.
 Clinical diagnosis of ADCP typically occurs within 18 months of birth and is primarily based upon motor function and neuroimaging techniques.
 While there are no cures for ADCP, some drug therapies as well as speech, occupational therapy, and physical therapy have shown capacity for treating the symptoms.
Mediterranean tropical-like cyclones, sometimes referred to as Mediterranean hurricanes or medicanes, are rare meteorological phenomena observed in the Mediterranean Sea.
 Due to the dry nature of the Mediterranean region, formation of tropical cyclones is infrequent, with only 99 recorded tropical-like storms between 1948 and 2011.
 No agency, however, is officially responsible for monitoring the formation and development of medicanes.
 Tropical cyclogenesis typically occurs within two separate regions of the sea.
 The first region, encompassing areas of the western Mediterranean, is more conducive for development than the other, the Ionian Sea to the east.
 The rough mountainous geography of the region raises additional difficulties despite being favorable for the development of severe weather and convective activity in general, and only with abnormal meteorological circumstances can medicanes form.
 Numerous studies have been conducted on the impact of global warming on Mediterranean tropical cyclone formation, generally concluding that fewer yet more intense storms would form.
The 1948 Pacific typhoon season is an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean.
 The season runs throughout 1948, though most tropical cyclones typically develop between May and October.
 The scope of this article is limited to the Pacific Ocean to the north of the equator between 100°E and 180th meridian.
 Within the northwestern Pacific Ocean, there are two separate agencies that assign names to tropical cyclones which can often result in a cyclone having two names.
 The Japan Meteorological Agency  will name a tropical cyclone should it be judged to have 10-minute sustained wind speeds of at least 65 km/h (40 mph) anywhere in the basin, whilst the Philippine Atmospheric, Geophysical and Astronomical Services Administration  assigns names to tropical cyclones which move into or form as a tropical depression in their area of responsibility located between 135°E and 115°E and between 5°N–25°N regardless of whether or not a tropical cyclone has already been given a name by the JMA.
 Tropical depressions that are monitored by the United States' Joint Typhoon Warning Center  are given a number with a "W" suffix.
Cyclone Hudah was a powerful and destructive tropical cyclone that affected Southeast Africa in April 2000.
 It was the last in a series of three cyclones that impacted Madagascar during the year.
 Hudah first developed as a disturbance embedded within the monsoon trough on March 22, within the Australian region cyclone basin.
 Moving westward as the result of a strong subtropical ridge to its south, the storm quickly intensified, and reached Category 2 cyclone intensity on March 25 before entering the Southwest Indian cyclone basin.
 For various reasons that remain unknown, the cyclone was only designated a name by the time it had crossed into the area of responsibility of the Regional Specialized Meteorological Center in Réunion.
 Nonetheless, Météo-France (MFR) assigned the name "Hudah" to the cyclone.
 An eye formed, and the storm intensified into a tropical cyclone on March 27 well to the southeast of Diego Garcia.
 On April 1, the MFR upgraded it to a very intense tropical cyclone, estimating peak 10 minute winds of 225 km/h (140 mph).
 By contrast, the Joint Typhoon Warning Center (JTWC) estimated 1 minute winds of 235 km/h (145 mph).
 Cyclone Hudah maintained peak winds until making landfall just southeast of Antalaha, Madagascar on April 2.
 It weakened greatly over land, but re-attained tropical cyclone status on April 5 after moving over the Mozambique Channel.
 Hudah reached 10 minute winds of 160 km/h (100 mph) by the time it made landfall on Mozambique near Pebane, Mozambique, on April 8, and dissipated by the next day.
The 1949 Pacific typhoon season is an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean.
 The season runs throughout 1949, though most tropical cyclones typically develop between May and October.
 The scope of this article is limited to the Pacific Ocean to the north of the equator between 100°E and 180th meridian.
 Within the northwestern Pacific Ocean, there are two separate agencies that assign names to tropical cyclones which can often result in a cyclone having two names.
 The Japan Meteorological Agency  will name a tropical cyclone should it be judged to have 10-minute sustained wind speeds of at least 65 km/h (40 mph) anywhere in the basin, whilst the Philippine Atmospheric, Geophysical and Astronomical Services Administration  assigns names to tropical cyclones which move into or form as a tropical depression in their area of responsibility located between 135°E and 115°E and between 5°N–25°N regardless of whether or not a tropical cyclone has already been given a name by the JMA.
 Tropical depressions that are monitored by the United States' Joint Typhoon Warning Center  are given a number with a "W" suffix.
In meteorology (and climatology), a mesonet, portmanteau of mesoscale network, is a network of (typically) automated weather and environmental monitoring stations designed to observe mesoscale meteorological phenomena.
 Dry lines, squall lines, and sea breezes are examples of phenomena that can be observed by mesonets.
 Due to the space and time scales associated with mesoscale phenomena, weather stations comprising a mesonet will be spaced closer together and report more frequently than synoptic scale observing networks, such as ASOS.
 The term mesonet refers to the collective group of these weather stations, and are typically owned and operated by a common entity.
 Mesonets usually record in situ surface weather observations but some involve other observation platforms, particularly vertical profiles of the planetary boundary layer (PBL).
A food allergy is an abnormal immune response to food.
 The signs and symptoms may range from mild to severe.
 They may include itchiness, swelling of the tongue, vomiting, diarrhea, hives, trouble breathing, or low blood pressure.
 This typically occurs within minutes to several hours of exposure.
 When the symptoms are severe, it is known as anaphylaxis.
 Food intolerance and food poisoning are separate conditions.

Question: Cyclone Qendresa was one of the most intense meteorological phenomena that typically occurs within two separate what?
Answer: regions of the sea