Exercises: Atmospheric and hydrospheric dynamics

Wind and ocean currents get their energy from the Sun. Using an everyday example (air moving when a radiator is turned on, or water in a heated pot), explain what happens to air or water when heated and how this movement gives rise to winds or currents.

Order the following steps in the formation of a sea breeze during the day: the cool air over the sea moves toward the coast, forming the breeze; the Sun heats the land faster than the sea; the air over the land warms up and rises; higher up, the air moves toward the sea and descends over it.

Explain in your own words what wind is and where the energy that sets it in motion comes from.

Define what an ocean current is and cite a well-known example, stating whether it is warm or cold.

Match each concept with its definition: wind, sea breeze, and ocean current, with movement of large masses of water in the ocean; movement of air on a local scale between the sea and the coast; movement of air caused by the uneven heating of the surface.

On a summer day, the sand on the beach burns your feet, but the seawater is much cooler. Relate this fact to the formation of the sea breeze.

State whether these statements are true or false and correct the false ones: ocean currents move enormous masses of water; seawater heats up faster than land; at night the breeze blows from the land toward the sea.

The water cycle and winds are connected. Explain where the energy that evaporates seawater comes from, and what role winds play in transporting water vapor from the ocean to the interior of continents.

Two locations situated at the same latitude, one on the coast and another inland, have different climates: the coastal town has milder winters and cooler summers. Explain why, taking into account that seawater heats up and cools down more slowly than land.

During the night, the breeze on the coast blows from the land toward the sea, the opposite of during the day. Explain why the direction of the breeze reverses.

Old sailing ships took advantage of the trade winds to cross the ocean. Explain what the trade winds are and where they get their energy from.

Ocean currents are said to be like conveyor belts transporting heat. Explain what effect a cold current has on the climate of the coast it borders and compare it with that of a warm current.

Waves form through the friction of the wind on the water's surface. Explain this connection between the atmosphere and the hydrosphere and cite another phenomenon in which both layers interact.

Very hot summer afternoons often end in storms. Relate this fact to the rise of warm, humid air and its cooling at altitude.

London (United Kingdom) and Calgary (Canada) are located at virtually the same latitude (around 51° N). However, the average January temperature in London is 5.5 °C (with very rare snowfall), while in Calgary it is -7.5 °C (with continuous snow for months).

1. a) Justify this marked climatic difference by analyzing how general atmospheric circulation and surface ocean currents interact in the North Atlantic.
2. b) A model predicts that global warming will trigger accelerated melting in Greenland, pouring huge volumes of freshwater into the ocean. Predict and justify what effect this input would have on ocean density, the North Atlantic thermohaline circulation (AMOC), and winter temperatures in northwestern Europe.

Along a stretch of coast with limestone cliffs, a city council plans to build a large concrete sea wall at the base of the cliff to stop wave action, claiming that this single project will completely stop cliff retreat.

1. a) Critically evaluate this claim: justify why it is insufficient by analyzing the weathering and erosion processes that the atmosphere (precipitation, wind, and thermal changes) and the continental hydrosphere (runoff and infiltration) will continue to exert on the upper and middle sections of the cliff.
2. b) Predict what medium-term consequences the installation of the sea wall will have on the adjacent beach, relating coastal transport and sedimentation dynamics.

Look at the temperature data for three locations situated at the same latitude (43° N) and at a similar altitude:

• Location 1: Average temp. in January: 9.2 °C; Average temp. in August: 21.1 °C.

• Location 2: Average temp. in January: 2.5 °C; Average temp. in August: 28.0 °C.

• Location 3: Average temp. in January: 12.0 °C; Average temp. in August: 17.5 °C.

1. a) Calculate the thermal amplitude (temperature range) of each one and deduce, with reasoned arguments, which corresponds to a small oceanic island, which to a continental coastal city, and which to the interior of a large continental landmass.
2. b) A classmate claims that seawater warms the coast in summer and cools it in winter. Refute their claim by explaining the thermal property of water (specific heat capacity) that turns the hydrosphere into a thermal regulator for the atmosphere.

On a beach, the wind direction is recorded at 12:00 and at 24:00 over three days: on day 1 it blows from the sea at midday and from the land at midnight; on day 2, the same; on day 3, which is cloudy, there is calm at midday and a land breeze at midnight. Interpret the data, explain the general pattern, and reason why no sea breeze formed on the third day.

During an intense El Niño event, the trade winds blowing westward across the equatorial Pacific weaken or even reverse their direction.

1. a) Predict what immediate consequences this weakening has on the upwelling of deep waters off the coast of Peru, and justify its impact on the marine food webs of the area.
2. b) A student claims that, being a purely oceanic phenomenon in the Pacific, it cannot alter rainfall on land. Refute their claim by explaining how the shift of the warm water mass alters low-pressure zones and convective air currents, causing floods on the arid South American coast and severe droughts in Indonesia.

During firefighting efforts in a large forest fire in a valley, firefighters observe two phenomena:

1. At the base of the fire, intense local winds are generated that blow directly toward the flames, fanning them, even though the general weather forecast indicated calm conditions.

2. High above the fire, a dense vertically developed cloud (pyrocumulus) forms, even producing lightning.

1. a) Physically justify the appearance of these local winds by connecting air temperature with atmospheric pressure and convection currents.
2. b) Explain the dynamic mechanism by which the rising column of warm air and smoke ends up condensing into a storm cloud at higher altitudes.

Imagine a hypothetical planet identical to Earth in size, atmospheric composition, and solar radiation, but that does not rotate on its axis (zero rotation).

1. a) Predict what global atmospheric circulation would be like on that planet: determine how many convective cells would exist in each hemisphere and in what direction surface winds would blow.
2. b) Compare that prediction with the real Earth: justify why on our planet there are three convective cells per hemisphere (Hadley, Ferrel, and Polar) and explain how subsidence (sinking of dry air) in the subtropical high-pressure belts determines the presence of large hot deserts around 30° latitude.

A category 4 hurricane moves across the Atlantic Ocean with winds exceeding 210 km/h. Two events are recorded along its trajectory:

1. Upon making landfall on a warm continental plain, its winds decrease by half in less than 24 hours.

2. Upon drifting back out to sea over a cold ocean current (20 °C), the hurricane ends up dissipating completely instead of re-intensifying.

1. a) An amateur claims that the hurricane weakened on land solely due to crashing into trees and buildings, and that in the cold sea it slowed down because cold water offers more resistance to the air. Refute both ideas by explaining the true thermodynamic mechanism (evaporation and latent heat of condensation) that connects the hydrosphere to the atmosphere in a tropical cyclone.
2. b) Predict and justify what would happen to the frequency and intensity of hurricanes if the average sea surface temperature of the tropical ocean increased by 2.0 °C.