Rain-shadow tendency
Leeward of the mountain
Move the city. Shape the land. Change the wind.
Discover why the weather takes a different turn.
Your city sits behind the mountain. Air rises on the approaching slope, then descends toward the city; warming as it descends can reduce cloud formation.
Leeward of the mountain
Water changes temperature more slowly than land. Airflow and distance affect its reach.
Cold air + relatively warm open water + a downwind city. These ingredients allow snow; they do not guarantee it.
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This is a qualitative teaching model, not live weather, a climate projection, or a forecast. Position and height controls are abstract diagram units. Cloud icons show a mechanism that can favor cloud formation; they do not show measured cloud cover. The diagram is a single cross-section with fixed airflow and no time evolution.
Mountains can lift moist air and favor precipitation on the windward side, while descending air can produce a rain shadow. Near a coast, water can moderate temperature swings, particularly with onshore flow. In the cold scenario, an open lake is assumed warmer than the incoming air; freezing it removes that moisture source. Wind speed, stability, actual temperatures, lake fetch, fronts, storm tracks, and precipitation amounts are not calculated. A mountain between the lake and city marks an interrupted path rather than predicting lake-effect snow beyond it.
Learn more: NWS · airflow over mountains · NWS · lake-effect snow. For observed patterns, try Pattern Finder in In-depth Data Analysis.