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The sensitivity of stratiform midlatitude orographic precipitation to global mean temperature is investigated through numerical simulations. As a step toward understanding the relative influence of thermodynamic and dynamical processes on orographic precipitation, simple idealizations of Earth’s major north–south mountain chains are considered. The individual terrain elements occupy four islands equally spaced around the Northern Hemisphere of a planet otherwise covered by ocean. Although these mountains have very little influence on the sensitivity of the zonally averaged precipitation to changes in global mean surface temperature, the precipitation on the windward slopes of the ridges is highly sensitive to such changes. When the ridges run between 40° and 60°N, the windward-slope hydrological sensitivity exceeds the Clausius–Clapeyron scaling of about 7% K−1 over the northern half of the barrier, leading to substantial precipitation changes. The annual accumulated orographic precipitation is mo...

The Response of Orographic Precipitation over Idealized Midlatitude Mountains Due to Global Increases in CO2