Chapter 19 - Non-Frontal Depressions Flashcards

1
Q

Where do cold core lows occur, what do they look like and what do they show as on an isohypes chart?

A

(Polar low) at a polar front depression.

They create a marked lows higher up in isohypse charts

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2
Q

Where do warm core lows occur, what do they look like and how can they be seen on isohypes charts?

A

(thermal low), in TRS

It is dependant on the difference in pressures around the core.

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3
Q

Where do warm core highs occur, what do they look like and how can they be seen on isohypes charts?

A

Sub tropical anti-cyclones.

They create marked high zones on isohypes charts

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4
Q

Where do cold core highs occur, what do they look like and how can they be seen on isohypes charts?

A

In Canada and Syberia in winter.

It is dependant on the pressures around the core, but they may not be seen at all.

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5
Q

What is a cold pool, what kind of weather is to be expected and how does it show on surface pressure charts?

A

A cold pool is a pool of cold air left over when a polar jet stream meanders and then reconnects with itself.

Thunderstorms and hail showers can be expected.

It depends on the pressures aroud the cold pool but it my not show on a surface pressure chart.

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6
Q

What are easterly waves/african easterly waves and what can they result in?

A

They are troughs of low pressure created by the convergance of warm dry air flowing off the SW coast of Africa and warm moist air flowing off the Atlantic.

This causes massive uplift which can lead to TRSs.

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7
Q

What is required for a TRS to form?

A

Ocean temperatures above 26degC (in summer or autumn)

CF so usually 10-20 lat.

A trigger (ITCZ or easterly waves)

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8
Q

What are the 4 stages of a TRS, what are their classifications during each and when do they terminate?

A

Formative stage - tropical depression

Immature stage - tropical storm

Mature stage - TRS

Decaying stage.

They can terminate at any stage if conditions do not favour development.

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9
Q

What are the characteristics of the formative stage of a TRS?

A

Condensation divergence aloft causes surface pressure to deepen below 1000mb

Winds are up to 34kts

Eye forms

Classidied as tropical depression

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10
Q

What are the characteristics of the immature stage of a TRS?

A

Central pressure is less than 1000mb

Wind speed is 34k-63kts

Surface pressure continues to fall

Classified as tropical storm.

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11
Q

What are the characteristics of the mature stage of a TRS?

A

Hurrican force winds - 64+kts

Up to 200nm from centre

In NH gales and bad weather extend further on the right of the path.

Classified as TRS

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12
Q

What are the characteristics of the decaying stage of a TRS?

A

Surface pressure starts to rise

Affected area reduces in size

Dissipates over land

Moves to higher latitudes.

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13
Q

Why is the weather on the right side of a TRS in the NH worse than in the left?

A

The wind speed adds with the travelling speed to create even stronger winds.

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14
Q

What is the designation of a TRS in the Caribean & Eastern Pacific?

A

A Hurricane

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15
Q

What is the designation of a TRS in the South China sea & Western North Pacific?

A

A Typhoon

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16
Q

What is the designation of a TRS in the Indian ocean & West Pacific (SH)?

A

A Cyclone

17
Q

What is the role of a Regional Speciality Meteorological Centre/Tropical Cyclone Warning Centre?

A

To provide advisories & bullitins with up to date first level basic meteorological information on all tropical cyclones, hurricanes and typhoons in their region of responsibility and collectively everywhere in the world.

18
Q

What part of the world suffers the most TRSs?

A

The NW Pacific.