A soil associated with the hot and wet tropics is typically characterized by high levels of weathering, leaching, and organic matter accumulation. These soils are often acidic, nutrient-poor, and prone to erosion due to the high levels of rainfall and warm temperatures in tropical regions.
A soil associated with the hot and wet tropics is typically highly weathered and nutrient-poor. The combination of high temperatures and heavy rainfall leads to rapid decomposition of organic matter and leaching of nutrients, resulting in laterite or oxisol soils that are low in fertility. Agricultural practices in these regions often require careful management to maintain soil health and productivity.
Very hot and wet weather is called "muggy" or "humid." This type of weather often feels uncomfortable and can be associated with high levels of moisture in the air.
A soil from a warm, wet place would likely be more leached of minerals and organic matter due to higher rainfall and microbial activity. In contrast, a soil from a hot, dry place would likely have higher concentrations of minerals and organic matter due to minimal leaching and slower decomposition rates. The warm wet soil would likely be more acidic and have less defined soil horizons compared to the hot dry soil which may be more alkaline and have clearer soil horizons.
Wet soil is commonly referred to as damp or moist soil.
In hot wet climates, heavy rainfall and high temperatures cause rapid weathering and leaching of nutrients from the soil. This leaching process results in the depletion of essential nutrients in the soil, making it thin and poor in fertility. The high levels of moisture can also lead to soil erosion, further contributing to its poor quality.
A soil associated with the hot and wet tropics is typically highly weathered and nutrient-poor. The combination of high temperatures and heavy rainfall leads to rapid decomposition of organic matter and leaching of nutrients, resulting in laterite or oxisol soils that are low in fertility. Agricultural practices in these regions often require careful management to maintain soil health and productivity.
Wet soil and mildly hot tempatures
tropics
Wet. Hot and wet climates allow for the fastest weathering.
u probably mean WET tropics... look that up instead
a hot biome would be irregularly warm warm would mean cool so its not a desert biome either a forest grassland or savana more of a humid place
because it is located in the tropics
the tropics and the amazon rainforest
Very hot and wet weather is called "muggy" or "humid." This type of weather often feels uncomfortable and can be associated with high levels of moisture in the air.
Mangroves can not grow in any desert, hot or cold. They love to 'have wet feet' and can only survive where the soil is wet.
oxisols
A soil from a warm, wet place would likely be more leached of minerals and organic matter due to higher rainfall and microbial activity. In contrast, a soil from a hot, dry place would likely have higher concentrations of minerals and organic matter due to minimal leaching and slower decomposition rates. The warm wet soil would likely be more acidic and have less defined soil horizons compared to the hot dry soil which may be more alkaline and have clearer soil horizons.