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Analysis of Climate Factors: Precipitation, Temperature, and Aridity

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Analysis of Precipitation

Total Precipitation

  • Very abundant: +1000 mm (mountain climate)
  • Abundant: +800 mm (oceanic climate)
  • Short: 800-300 mm (continentalized coastal Mediterranean climate)
  • Very low: <300 mm (sub-desert steppe climate)
  • Extremely low: <150 mm (desert climate)

Distribution of Rainfall

  • Regular: No dry month with rainfall < 30 mm (oceanic climate)
  • Fairly regular: Maximum of 2 dry months (oceanic climate transitioning towards continental Mediterranean)
  • Irregular: More than 2 dry months (Mediterranean climate), +7 dry months (dry sub-desert or steppe Mediterranean climate)

Noteworthy points:

  • Seasons with more abundant precipitation
  • Months with less or no rainfall (dry months)

Analysis of Temperature

Average Annual Temperature and Thermal

... Continue reading "Analysis of Climate Factors: Precipitation, Temperature, and Aridity" »

Understanding the Composition and Structure of the Atmosphere

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Composition of the Atmosphere: The atmosphere is the envelope of the land held around our planet by gravity. It is composed of a set of gases and other gaseous elements in suspension. The atmosphere's presence avoids large oscillations of temperature on the Earth's surface, as solar radiation decreases during the day and prevents excessive heat loss at night. In the absence of the atmosphere, temperatures could reach over 95°C during the day and drop to -180°C overnight. The atmosphere contains the necessary components for organisms to perform their vital processes.


Origin and Balance of the Atmosphere: Gases in the atmosphere originated from the rocks of the Earth approximately 4.6 billion years ago, when the Earth's materials were in a semi-... Continue reading "Understanding the Composition and Structure of the Atmosphere" »

Earth Systems, Planetary Habitability, and Environmental Change

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Conditions for a Habitable Planet

  • Suitable Temperature: Must allow metabolic processes to function.
  • Tectonic Activity: Volcanic eruptions and magmatic intrusions bring essential elements for life to the surface.
  • Presence of Liquid Water.
  • Radiation Protection: Shielding against high-frequency photochemical radiation (e.g., magnetosphere, ionosphere, ozone layer).

Earth Systems and Human Interactions

System Components

  • Nature: Biosphere, Atmosphere, Geosphere, Hydrosphere.
  • Society: Population, Lifestyles, Science, Technology, Culture.
  • Economy: Agriculture, Industry, Transport, Housing.

Inter-System Exchanges

  • Nature to Society (NS): Provides air, water, energy, protection.
  • Society to Nature (SN): Generates waste, causes impacts.
  • Nature to Economy (NE): Provides
... Continue reading "Earth Systems, Planetary Habitability, and Environmental Change" »

Mesozoic and Cenozoic Eras: Evolution, Climate, and Fossils

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Mesozoic Era (250-65 Ma)

No geological evolution. Towards the end of the Paleozoic and Mesozoic, all continents of the Earth united to form Pangea. The distribution of land and sea undergoes major changes during this era, during which continents separate.

Life in the Mesozoic

In the Mesozoic, a major diversification of marine fauna, especially molluscs and echinoderms, occurred due to the fracturing of Pangea. Reptiles experienced significant diversification, colonizing air, aquatic, and terrestrial environments (dinosaurs).

Types of Dinosaurs:

  • Teropods: Carnivorous with short front legs equipped with strong claws and enormous teeth.
  • Sauropods: Large quadrupedal herbivores with very long necks and tails, and columnar legs.
  • Ornithopods: Bipedal herbivores.
... Continue reading "Mesozoic and Cenozoic Eras: Evolution, Climate, and Fossils" »

Geography and Climate of Andalusia: Rivers, Climate Variations, and Environmental Issues

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THE WATER OR RIVERS:

The route of the rivers is determined by the relief. The characteristic differentiated sides are the Atlantic side and Mediterranean.

Atlantic:

Here are the longest rivers. This vertiente pertenece the longest river and the mighty of the region Guadalquivur along with its main tributary, the Genil basin is regulated by Gualdalkibir numbers embalses. Other rivers of the red side are the Guadalete, Odiel, and Barbate.

Mediterranean:

Is composed of rivers that pour their waters into the Mediterranean Sea. These rivers are born on the mountain rivers Penibética neighborhoods so they are small and short with irregular flow. Some of these rivers remain dry most of the year. Among Andalusian Mediterranean rivers can stand the walking... Continue reading "Geography and Climate of Andalusia: Rivers, Climate Variations, and Environmental Issues" »

Ethics and Morality: Principles of Human Conduct

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Understanding Ethics: Core Concepts and Distinctions

Etymology and Definition of Ethics

Ethics is a concept derived from the Greek word "ethos," which means 'custom,' 'character,' 'habit,' or 'disposition.' Its etymology is similar to that of 'morality.'

Ethics vs. Morality: Key Differences

While 'ethics' and 'morality' are often used interchangeably, many scholars establish a primary distinction. Ethics is the philosophical discipline that studies morality, forming a core part of moral philosophy.

Ethics is the discipline that studies how human actions should be to be considered morally good. It examines how we ought to act to live a morally upright life and explores various systems where human happiness is often considered the ultimate goal.

The

... Continue reading "Ethics and Morality: Principles of Human Conduct" »

Earth's Ancient Eras: Precambrian and Paleozoic Transformations

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Precambrian Eon (4.55 Billion to 541 Million Years Ago)

The Precambrian Eon encompasses Earth's earliest and longest period, from its formation to the dawn of complex life.

Archean Eon (4.0 to 2.5 Billion Years Ago)

Rocks from the Archean Eon constitute only about 3% of Earth's exposed surface, yet they hold crucial clues to our planet's infancy.

Geological Evolution

In the beginning, Earth was a vast ocean of magma, which gradually cooled, leading to the formation of the lithosphere.

Atmosphere Formation

The atmosphere formed from the degassing of the planet, with a composition very similar to primitive volcanic emanations: slightly reductive, virtually without oxygen, and rich in water vapor.

Hydrosphere Development

The hydrosphere formed from the... Continue reading "Earth's Ancient Eras: Precambrian and Paleozoic Transformations" »

Ancient Theaters, Amphitheaters, and Circuses: A Comparative Study

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Ancient Theaters, Amphitheaters, and Circuses

Participate in this topic by adding -nt- (1a and 2a) or -ent- (3a and 4a). Laudo to Laudants-NTIS, NTIS-time 2 timens, Capio-3 capients capientis, audio 4-audients audientis. // participant Amans, NTIS puerum-lover Pueri lovers, Puelles amantibus; etc. ...// cancertat may be involved or absolute (in ablative). // Translation (was, were, they came ... they saw ... what is ....)// Decumanus (EO) Cards (NS) //

The Greek Theatre was divided into three distinct sections:

  • The stands where spectators were sitting.
  • The orchestra, a circular space where the chorus sang and danced.
  • The stage, a platform for actors and a building that served as a backdrop, storage, and dressing rooms (scaena).

The Romans followed... Continue reading "Ancient Theaters, Amphitheaters, and Circuses: A Comparative Study" »

Late Medieval Spain: Political and Economic Transformations

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The First Nuclei of Resistance

United Astur-Leones

In 718, Don Pelayo was elected king. In 722, the victory of Covadonga was achieved.

United Pamplona

Around the 9th century, Sancho I strengthened the new kingdom, extending it southward. His dynasty established the County of Aragon in 970.

County of Aragon

In the central Pyrenees, the counties of Aragon, Ribagorza, and Sobrarbe were formed. From 970, it was linked to Pamplona.

Catalan Counties

Located in the eastern Pyrenees, these counties were related to the Carolingian monarchy in the 8th and 9th centuries.

Main Stages of the Reconquest

8th-10th Centuries

Christian advances were limited to occupying nearly empty territories, such as the Duero basin and the northern Ebro.

11th and First Half of the 12th

... Continue reading "Late Medieval Spain: Political and Economic Transformations" »

Understanding the Greenhouse Effect, Climate Change, and Carbon Cycle

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The greenhouse effect is a natural process that warms the Earth's surface. Here's a breakdown:

  1. Solar radiation received: 100%.
  2. 30% is reflected by the atmosphere and the Earth's surface.
  3. 19% is absorbed by clouds and other atmospheric components.
  4. 51% is absorbed by the land surface, which then heats up.
  5. The heated surface emits infrared radiation.
  6. Some of this infrared radiation is absorbed by greenhouse gases and re-emitted back to the surface.
  7. The remaining infrared radiation passes through the atmosphere and dissipates into outer space.

Reconstructing Past Climates

Ice core records help reconstruct past climates:

  1. Air bubbles trapped in ice: Ice accumulated in layers, particularly in Antarctica, contains small air bubbles. These bubbles reveal the
... Continue reading "Understanding the Greenhouse Effect, Climate Change, and Carbon Cycle" »