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Climatic geomorphology is a field that studies how climate influences the formation and evolution of landforms. It defines distinct "morphoclimatic zones" across the globe where specific relief-forming processes are dominant due to climate.12

Key aspects include:
* Climate's Role: In regions without significant tectonic activity, climate is the primary driver of landform development. This is particularly evident in areas that have experienced repeated climate changes, leading to polygenetic landform associations.34
* Morphogenetic Areas: These are regions where a particular set of landforms is generated under a specific climate. As climates shift, these morphogenetic areas can move, leaving behind relict landforms from previous environments.2
* Process Variation: Different climates (humid, arid, glacial) utilize distinct geomorphic agents like running water, wind, and ice, shaping landforms in unique ways. For example, tropical regions with dense vegetation and deep weathering profiles exhibit different fluvial activity compared to savanna regions with seasonal rainfall and higher erosion rates.541

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