CCEA A-Level Geography 3910
Processes That Shape Fluvial Environments
Human Interaction in Fluvial Environments
Global Biomes
Small-Scale Ecosystems
The Processes That Shape Our Weather and Climate
Weather in the British Isles
Global Weather Issues
Population Data
Population Change
Population and Resources
Settlement Change and the Rural-Urban Fringe
Planning in Rural Environments
Urban Challenges in MEDC and LEDC Cities
Measuring Development
Reducing the Development Gap
Emerging Markets
Data Collection
Data Processing
Fieldwork Skills and Techniques
Planning and Recording an Investigation
Plate Tectonics: Theory, Margins and LandformsTectonics
Volcanic Activity and Its ManagementTectonics
Seismic Activity and Its ManagementTectonics
Locations and Climates of the Major Tropical BiomesTropical
Management and Sustainability in Arid and Semi-Arid Tropical EcosystemsTropical
Management and Sustainability in the Tropical Forest EnvironmentTropical
Coastal Processes and FeaturesCoastal
Regional Coastlines: Submergence, Emergence and Rising Sea LevelCoastal
Coastal Management and SustainabilityCoastal
Natural Climate Change: Evidence, Causes and the Arrival of the HoloceneClimate
Lowland Glacial LandscapesClimate
Current Global Climate Change: Human Causes and ImpactsClimate
Managing Global Climate ChangeClimate
Cultural Groups, Social Inequality and LandscapeCultural
MigrationCultural
The Geographies of CyberspaceCultural
Sustainable Development in SettlementsPlanning
Urban Design, Planning and Management for SustainabilityPlanning
Traffic and TransportPlanning
Defining EthnicityEthnic
Processes That Create and Maintain Ethnic DiversityEthnic
Ethnic ConflictEthnic
The Changing Nature of TourismTourism
Challenges and Management of Mass TourismTourism
Ecotourism: Opportunities, Challenges and RegulationTourism
Decision Making in Geography
Data Collection
Synoptic charts and remotely sensed data
- 3 things to know
- Unit AS 3
Overview
Synoptic chart, remote sensing and limitations of relying on remotely sensed data in an investigation.
What you need to know
Answer each one before you reveal it.
What are isobars, and in what units is pressure given on a synoptic chart?
What does the spacing of isobars tell you, and why?
Questions from this subtopic
Each one with the model answer underneath.
- 1
What is a synoptic chart, and what does it show?
Model answer
A synoptic chart, or surface pressure chart, is a map showing the state of the atmosphere over a wide area at a single moment. It shows atmospheric pressure at sea level as a pattern of isobars, the positions and types of fronts, the centres of high and low pressure, and often station circles giving wind speed and direction, temperature and cloud cover at individual observing sites. It is the standard tool for identifying which weather system is affecting an area and what weather will follow.
- 2
What are isobars, and in what units is pressure given on a synoptic chart?
Model answer
Isobars are isolines joining all points of equal atmospheric pressure reduced to sea level. Pressure is given in millibars, equivalent to hectopascals, and isobars are normally drawn at intervals of four millibars. Average sea-level pressure is around 1013 millibars, so values well below that indicate a depression and values well above it an anticyclone.
- 3
What does the spacing of isobars tell you, and why?
Model answer
Closely spaced isobars mean a steep pressure gradient - a large pressure change over a short distance - which produces strong winds, so tightly packed isobars around a depression indicate gales. Widely spaced isobars mean a gentle pressure gradient and therefore light winds or calm conditions, which is typical of an anticyclone. Wind speed is read from the isobar spacing, not from the pressure value itself.
- 4
How are the three types of front shown on a synoptic chart, and what does each represent?
Model answer
A warm front is drawn as a line with semicircles on the leading side, and marks warm air advancing over and rising above cooler air ahead of it. A cold front is drawn as a line with triangles, and marks cold air undercutting and forcing up the warm air ahead of it. An occluded front is drawn with alternating semicircles and triangles on the same side, and forms where the faster-moving cold front has caught up with the warm front and lifted the warm air clear of the ground. The symbols are placed on the side towards which the front is moving.
- 5
How do you recognise a depression on a synoptic chart, and what weather sequence does it bring?
Model answer
A depression appears as a centre of low pressure marked L, with roughly circular isobars whose values fall towards the centre, usually closely spaced, and commonly with a warm front and a cold front trailing from it. As it passes, the weather typically runs in sequence: falling pressure with high cloud thickening and steady rain as the warm front arrives; then a milder, cloudy sector with drizzle behind it; then a sharp band of heavy showery rain and a temperature drop at the cold front; followed by rising pressure, brighter conditions and scattered showers in the cold air behind.
- 6
How do you recognise an anticyclone on a synoptic chart, and what weather does it bring?
Model answer
An anticyclone appears as a centre of high pressure marked H, with widely spaced isobars whose values rise towards the centre and no fronts within it. The gentle pressure gradient gives light winds, and descending air suppresses cloud formation, so conditions are settled and dry. In summer that means hot sunny days with a risk of haze or thunderstorms after prolonged heating; in winter the clear skies allow rapid night-time heat loss, giving frost, fog and cold, still days.
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