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Explore the essential nutrient cycles on Earth, including carbon, nitrogen, phosphorous, sulfur cycles, and learn about atmospheric layers, wind patterns, ocean currents, El Nino, La Nina, and climate impacts. Understand how these processes shape our environment.
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Nutrient Cycles • Carbon Cycle • Based on CO2 cycling from animals to plants during respiration and photosynthesis. • Heavy deposits are stored in wetland soils, oceans, sedimentary rocks. • under right conditions, can become fossil fuels • Released by combustion and volcanic activity. • Returns to the soil from the atmosphere through rainfall • Carbonic Acid + H20 = Rain with a pH of ~5.4
Nutrient Cycles • Nitrogen Cycle • Nitrogen Fixation • Bacteria converts gaseous nitrogen to ammonia • ex: Rhizobium conversion of N to ammonium ions. • Nitrification • Plants absorb ammonium ions as a nutrient. • Passed on to animals. • Used to make vital organic compounds • CHON
Nutrient Cycles • Phosphorous Cycle • Based on phosphate ions (PO43-) usually found in rock formations and ocean sediments. • Released by weathering and volcanic activity. • Plants uptake nutrients and pass them on to animals. • Waste products, animal remains, and runoff return phosphate.
Nutrient Cycles • Sulfur Cycle • Most sulfur found in rocks, minerals, and ocean sediments. • Sulfur enters atmosphere through weathering, sea spray, and volcanic activity (H2S, SO2). • Returns to the earth from the atmosphere in the form of acid rain. • Avg. pH is 4.3
Nutrient Cycles • Hydrologic Cycle (aka) Water Cycle • Evaporation and Transpiration • Condensation and Precipitation • Infiltration and Percolation • Runoff
Atmosphere • Troposphere • inner layer of the atmosphere • physical properties include: • temperature • precipitation • cloud cover • wind direction and speed • these properties (and others) at a given time and place are called the weather. • Stratosphere • second layer of the atmosphere
Winds • Global air circulation patterns are affected by: • uneven heating of the earth’s surface. • seasonal changes. • earth’s rotation. • long-term variations in the amount of solar energy striking the earth. • properties of air and water.
What is the Earth’s tilt? • 23.5º
Winds • Warm Fronts • leading edge of a mass of warm air converging on a mass of cool air • less dense, warm air rises above the cool air • moisture condenses and produces clouds • often the clouds will descend and produce precipitation
Winds • Cold Fronts • leading edge of a mass of cool air converging on a mass of warm air • denser cool air stays toward the ground • produces rapidly moving towering clouds called thunderheads • cold fronts bring high surface winds and thunderstorms but then cooler, clear skies afterward
Pressure • Highs • high pressure air masses that descend towards the earth’s surface • produces fair weather • Lows • low pressure air masses that rises • rising cools and expands the air causing precipitation High Low High Low High Low High
Ocean Currents • Created by same reasons as winds. • Distributes heat, nutrients, and DO. • Upwellings • occurs from constant trade winds • They push surface water out which is replaced by cool, deep water rich in nutrients.
El Nino – Southern Oscillation (ENSO) • Trade winds normally blow warm water off the coast of South America and California (creates upwellings). • When winds fail, weaken, or change direction, the waters warm and stagnate. • Causes less productivity and possibly red tide. • As the Pacific surface temperature becomes warmer, global weather patterns are disrupted • First seen with wetter weather in eastern Pacific.
La Nina • Opposite of El Nino. • Trade winds will increase in strength • Weather patterns are also affected • Opposite effects of El Nino
Climate and Weather • Climate • average long term weather • ~30 years of data • basically determined by average temperature and average precipitation • Winds • create climate • circulate heat, moisture, and nutrients. • also transport bacteria, viruses, pollution and radioactive wastes.
Rain Shadow Effect • AKA: Orographic Uplift • warm air rises and releases moisture on windward side of mountain. • air on leeward side is cooler and dry. • creates a distinctive microclimate on either side of mountain.
Microclimate Factors • Vegetation • affects humidity, winds, and creates shadows. • warmer in winter, cooler in summer. • Cities • buildings, asphalt, and vehicles raise temperatures and create haze and smog.
Plate Boundaries • Convergent • Transform • Divergent
Biomes • Biome • A large, relatively distinct terrestrial region with a similar climate soil, plants, and animals, regardless of where it occurs in the world • Typically determined by: • Climate • especially precipitation • Latitude • distance from the equator • Altitude • elevation above sea level
Tundras • Treeless biome in the far north with harsh, cold winters and extremely short summers • Precipitation • 10–25 cm/yr • Temperature • Short growing season • 50–160 days
Tundras • Nutrient poor soils with little organic material • Permafrost present • Low species richness • Vegetation is mostly grasses & shrubs • Small herbivores • Occasional Arctic fox & wolf • Low primary productivity
Boreal Forests • A region of coniferous forests in the northern hemisphere • Just south of tundra • Growing Season • A little longer than tundra • Precipitation • ~ 50 cm/yr
Boreal Forests • Soils are acidic and mineral poor • Vegetation comprised of drought resistant conifers • Mostly small animals • Some large animals • wolves, bear, moose • Aka: • coniferous forest • evergreen forest • taiga
Temperate Rainforests • Coniferous biome with cool weather, dense fog and high precipitation • Ex: Northwest US • Precipitation • > 127 cm/yr • Heaviest in winter • Temperature • Winters are mild • Summers are cool
Temperate Rainforests • Soils are nutrient-poor, but high in organic material (dropped needles) • Cool temperatures slow decomposition • Dominant Vegetation • Large evergreen trees • Old-growth forest • Variety of cool climate animal life • Very high species richness • Heavily logged
Temperate Deciduous Forests • Forest biome that occurs in temperate areas with a moderate amount of precipitation • Precipitation • 75–150 cm/yr • Temperature • Seasonality • Hot summers and cold winters
Temperate Deciduous Forests • Topsoil is rich in organic material and underlain by clay • Vegetation is primarily deciduous • oak, maple, beech • Animals • deer, bear and small animals • Most of this biome land area has been regenerated after farming & timber harvest
Grasslands • Grasslands with hot summers, cold winters and too little precipitation to support trees • Precipitation • 25–75 cm/yr • 90% of this biome has been lost to farmland
Grasslands • Soil has thick, organic material rich organic horizon • Periodic fires keep the dominant vegetation • Animals • Once covered with bison • no longer true • Smaller animals are still present (ex: prairie dogs)
Grasslands • North America • prairies • South America • pampas • Europe/Asia • steppes • Africa • veld
Chaparrals • Also called a Mediterranean Climate • Ex: Southern California • Ex: Greece • Temperature • Mild, moist winters • Hot, dry summers • Frequent fires • Crown vs. Surface
Chaparrals • Soil is thin and often not fertile • Vegetation • Dense growth of evergreen shrubs • Lush during the growing season • Animals • Mule deer, chipmunks, many species of birds
Deserts • Biome where lack of precipitation limits plant growth • Temperature • Can vary greatly in 24-hr period, as well as yearly (based on location) • Precipitation • < 25 cm/yr
Deserts • Soils low in nutrients and high in salts • Sparse vegetation • cactus and sagebrush • Animals are very small to regulate temperature
Savannas • Tropical grassland with widely scattered trees • Temperature • Varies little throughout the year • Precipitation • Seasons regulated by precipitation, not temperature • 76–150 cm/yr
Savannas • Soil low in nutrients due to leaching • Vegetation • Wide expanses of grass, occasional Acacia trees • Animals • Herds of hoofed animals • Large predators - lions, hyenas, etc.
Tropical Rainforests • Lush, species-rich biome that occurs where climate is warm and moist throughout the year • Precipitation • 200–450 cm/yr • Very productive biome • Most species-rich biome
Tropical Rainforests • Ancient, weathered, nutrient-poor soil • Nutrients tied up in vegetation, not soil • Vegetation • distinct layers • Canopy • Understory • Forest floor • Animals • Most abundant insect, reptiles and amphibians on earth