What Oceanic and Atmospheric Patterns Are Predicted for a Newly Discovered Planet?
PLANET W is a newly discovered planet that is similar to Earth. It has oceans, an atmosphere very similar to Earth's, and ice at both poles. Since no astronaut has yet ventured to the planet, we currently only know things we can observe from a distance, specifically the physical geography — the distribution of land, oceans, and sea ice, as well as the larger features on land. To guide future expeditions, you will use the known physical geography to predict the global patterns of wind, ocean currents, and atmosphere-ocean-cryosphere interactions.
Goals of This Exercise:
- Observe the global distribution of continents and oceans on Planet W.
- Create a map showing the predicted geometries of global winds, ocean currents, and major atmospheric features, like the ITCZ and polar front.
- Draw cross sections that portray the global patterns, predicting the locations of warm pools, zones of high and low precipitation, and possible sites for ENSO-type oscillations.
- Use your predictions to propose two habitable sites for the first two landing parties.
Follow the steps below, entering your answers for each step in the appropriate place on the worksheet or online.
- Observe the distribution of continents and oceans on the planet. Note any features that you think will have a major impact on the climate, weather patterns, and other aspects of atmosphere-ocean-cryosphere interactions. Descriptions of some features are on the next page.
- Draw on the worksheet the predicted patterns of atmospheric wind circulation (trade winds, westerlies, etc.), assuming that the patterns are similar to those on Earth.
- Draw on the worksheet the likely paths of ocean currents within the central ocean. Identify the segments of a current that will be a warm current, cold current, or neither.
- Draw on the worksheet the likely locations of warm pools and shade in red any area on land whose climate will be heavily influenced by the presence of this warm pool. Shade in parts of the ocean that are likely to be more saline than others.
- From the pattern of winds and ocean currents, identify which side of a mountain range would have relatively high precipitation and which side would have lower precipitation because it is in a rain shadow. Color in these zones on the worksheet, using blue for mountain flanks with high precipitation and yellow for areas of low precipitation. Note, however, that precipitation patterns along a mountain range can change as it passes from one zone of prevailing winds into another, or if wind directions change from season to season.
Your instructor may also have you complete the following steps. Complete your answers on a sheet of graph paper.
6. Draw four cross sections across the central ocean, extending from one side of the globe to the other. Of these cross sections, draw one in an east-west direction across each of the following zones: (1) between the equator and 30° (N or S); (2) within a zone of westerlies (N or S); and (3) within the south polar zone, south of 60° S. The fourth cross section can be drawn at any location and in any direction, but it should depict some aspect of the oceanic and atmospheric circulation that is not fully captured by the other cross sections. On each cross section, draw the surface wind patterns, zones of rising or sinking air, and possible geometries of a Walker cell or other type of circulation, where appropriate. Be prepared to discuss your observations and interpretations.
7. Draw a north-south cross section through the oceans, showing shallow and deep flows that could link up into a thermohaline conveyor. Describe how this might influence the climate of the entire planet and what might happen if this system stops working.
Some Important Observations About the Planet
- The planet rotates around its axis once every 24 hours in the same direction as Earth. Therefore it has days and nights similar to Earth's. It orbits a sun similar to our own, at about the same distance. Its spin axis is slightly tilted relative to the orbital plane, so it has seasons.
- The planet has well-developed atmospheric currents, with wind patterns similar to those on Earth.
- The oceans are likewise similar to those on Earth. They are predicted to have ocean currents that circulate in patterns similar to those on Earth. The oceans are predicted to have variations in sea-surface temperature, salinity, and therefore density, but no data are available for these aspects.
- The planet has ice and snow near both poles, some on land and some over the ocean.
1. A continent, simply called Polar Continent for now, is over the North Pole, but slightly off to one side. The western part of the continent extends south of 60°, but there are no data about whether this part has ice. There appear to be ice shelves and sea ice surrounding part of the continent.
2. There is a gap between Polar Continent and those continents to the south, providing a relatively land-free zone through which the ocean can circulate. Consider how this gap might influence speeds of winds and ocean currents here.
3. A nearly continuous mountain range runs along the coast of Eastern Continent.
4. There is extensive ice and snow over the South Pole, but the ice is floating on the ocean (there is no land at the pole). The sea ice extends to the Eastern and Western Continents, both of which also have glaciers that flow downhill toward the sea, where they melt.
5. Western Continent does not have significant mountains but, like Eastern Continent, has a curved coastline with large peninsulas that extend out into the ocean and embayments, where the ocean curves into the land.
- What Influences Climates Near the Southern Isthmus of Central America?
- Do Other Oceans Display Oscillations?
- How Does an El Niño Start and Stop?
- Do Impacts of ENSO Reach Beyond the Tropics?
- What Are the Phases of ENSO?
- What Are El Niño and the Southern Oscillation?
- What Connects Equatorial Atmospheric and Oceanic Circulation?
- How Are the Atmosphere, Oceans, and Cryosphere Coupled?
- What Processes Affect Ocean Temperature and Salinity in Tropical and Polar Regions?