Skip to main content

Terrestrial Ecosystem


A terrestrial ecosystem is a land-based ecological system where biotic components (living organisms) interact with abiotic components (non-living physical and chemical factors).

  • Covers approximately 28–29% of Earth's surface (land area).

  • Organized into large ecological regions called biomes.

  • Distribution is mainly controlled by:

    • Temperature

    • Precipitation

    • Latitude

    • Altitude

 Components

A. Biotic Components

  1. Producers (Autotrophs)

    • Green plants and photosynthetic organisms.

    • Convert solar energy into chemical energy through photosynthesis.

    • Form the primary productivity base.

  2. Consumers (Heterotrophs)

    • Primary consumers (herbivores)

    • Secondary/Tertiary consumers (carnivores, omnivores)

  3. Decomposers (Detritivores & Saprotrophs)

    • Bacteria and fungi.

    • Responsible for nutrient cycling and mineralization.


B. Abiotic Components

  • Soil (edaphic factors)

  • Climate (temperature, precipitation, humidity)

  • Solar radiation

  • Topography

  • Wind patterns

These factors regulate primary productivity, species distribution, and ecosystem functioning.


3. Functional Processes

  • Energy flow (unidirectional)

  • Biogeochemical cycles (carbon, nitrogen, phosphorus cycles)

  • Carbon sequestration

  • Ecological succession

  • Trophic dynamics

Forest Ecosystems

A forest ecosystem is a terrestrial biome characterized by high tree density, vertical stratification, and high biomass.

Classification Basis:

  • Latitude

  • Climate (temperature + rainfall)

  • Vegetation type (leaf morphology)


A. Tropical Forests

Location:

Near the equator (0°–10° latitude).

Climate:

  • High temperature (25–30°C average)

  • Annual rainfall > 200 cm

  • No distinct winter

Key Features:

  • High Net Primary Productivity (NPP)

  • Multi-layered canopy structure:

    • Emergent layer

    • Canopy

    • Understory

    • Forest floor

  • Extremely high species richness and endemism

  • Rapid nutrient cycling but nutrient-poor soils

Ecological Importance:

  • Major global carbon sink

  • High biodiversity reservoir


B. Temperate Forests

Location:

Mid-latitudes (30°–50°).

Climate:

  • Moderate rainfall

  • Distinct seasons

Types:

  1. Deciduous forests

    • Broad-leaved trees

    • Seasonal leaf shedding (adaptation to cold/drought)

  2. Temperate coniferous forests

    • Needle-leaved evergreen trees

Soil:

Relatively fertile compared to tropical forests.


C. Boreal Forest (Taiga)

Location:

High latitudes (50°–70° N).

Climate:

  • Long, severe winters

  • Short growing season

  • Moderate precipitation (mostly snow)

Vegetation:

  • Coniferous species (needle-leaved)

  • Adapted to cold and low evaporation

Ecological Role:

  • Stores large amounts of carbon in biomass and soils

  • Lower species diversity but large geographic extent


Specialized Forest Types

1. Mediterranean Forests

  • Hot, dry summers

  • Sclerophyllous vegetation (thick leaves)

2. Montane Forests

  • Altitudinal zonation

  • Temperature decreases with elevation

3. Mangrove Forests

  • Coastal intertidal zones

  • Salt-tolerant (halophytic) vegetation

  • Shoreline stabilization and storm buffering


2. Grassland Ecosystems

Grasslands are terrestrial ecosystems dominated by grasses and herbaceous vegetation, with insufficient rainfall to support dense forests.

Coverage:

~20% of global land surface.

Climate Control:

  • Moderate to low precipitation

  • Seasonal rainfall

  • Periodic fires and grazing


A. Tropical Grasslands (Savanna)

Features:

  • Wet and dry seasons

  • Scattered trees

  • High grazing pressure

Ecological Traits:

  • Fire-adapted vegetation

  • Large herbivore populations


B. Temperate Grasslands

Climate:

  • Cold winters

  • Hot summers

Soil:

  • Deep, fertile chernozem soils

  • High organic matter

Examples:

  • Prairies

  • Steppes

  • Pampas


C. Montane Grasslands

  • Occur at high altitudes

  • Short growing season

  • Alpine meadows


D. Flooded Grasslands

  • Seasonally inundated

  • High productivity

  • Important wetlands


E. Desert/Xeric Grasslands

  • Transition zones between grassland and desert

  • Sparse vegetation


3. Desert Ecosystems

Deserts are terrestrial ecosystems characterized by extremely low precipitation (<25 cm annually) and high evapotranspiration rates.


Key Characteristics

  • Large diurnal temperature variation

  • Low primary productivity

  • Sandy or rocky soils

  • Low organic matter


Types of Deserts

  1. Hot and dry

  2. Semi-arid

  3. Coastal

  4. Cold deserts


Adaptations

Plants:

  • Xerophytes

  • Succulents

  • Reduced leaf surface area

  • CAM photosynthesis

Animals:

  • Nocturnal behavior

  • Water conservation mechanisms


4. Mountain Ecosystems

Mountain ecosystems are characterized by altitudinal zonation, where climate and vegetation change with elevation.


Key Concepts

  • Environmental lapse rate (temperature decreases with altitude)

  • "Water towers of the world" (source of rivers)

  • High endemism


Zonation

  1. Foothill forests

  2. Montane forests

  3. Subalpine zone

  4. Alpine tundra

  5. Permanent snow


5. Tundra Ecosystems

Tundra is a treeless biome with extremely low temperatures and the presence of permafrost (permanently frozen subsoil).


Types

  1. Arctic tundra (high latitude)

  2. Alpine tundra (high altitude)


Characteristics

  • Short growing season (6–10 weeks)

  • Low precipitation (but low evaporation)

  • Poorly developed soil


Vegetation

  • Mosses

  • Lichens

  • Dwarf shrubs

  • Sedges


Faunal Adaptations

  • Thick fur/insulation

  • Migration

  • Hibernation


Comparative Analysis

FeatureDesertTundraGrasslandForest
Water availabilityVery lowFrozen waterModerate seasonalHigh (varies by type)
BiodiversityLowLow–moderateModerateVery high (tropical)
Soil fertilityPoorPoorHigh (temperate)Variable
TemperatureExtreme heat/coldPersistently coldSeasonalClimate dependent

Ecological Importance of Terrestrial Ecosystems

  1. Carbon sequestration

  2. Oxygen production

  3. Climate regulation

  4. Biodiversity conservation

  5. Soil formation

  6. Water cycle regulation

  7. Provisioning services (food, timber, fiber)


Core Controlling Factors

  • Latitude

  • Altitude

  • Precipitation

  • Temperature

  • Soil type

  • Disturbance regimes (fire, grazing, storms)


Comments

Popular posts from this blog

Regional Geography, Systematic Geography, Idiographic, Nomothetic, Inductive and Deductive Approaches

T wo major ways of studying Geography : the Regional Approach and the Systematic Approach . It also explains the related ideas of idiographic vs. nomothetic and inductive vs. deductive reasoning , especially in the context of the Hartshorne–Schaefer debate . 1. Regional Geography: “All About One” Regional Geography studies one particular region in detail . A region is an area that has some degree of homogeneity (sameness) within its boundary but is also unique or different from other regions . For example, if we study Palakkad District , we may study: Relief and drainage Climate Soil Vegetation Agriculture Population Occupation Economy Culture Political characteristics The purpose is to understand the complete geographical personality of Palakkad and the relationships among its different features. Key concepts Region: A geographical area with identifiable characteristics and boundaries. Homogeneity: Si...

Multispectral and Hyperspectral Imaging Systems

The main idea is how a remote-sensing sensor collects information about an area . A sensor does not simply take an ordinary photograph. It measures the electromagnetic energy reflected or emitted by objects in different wavelength bands . Depending on how many bands are measured and how the sensor collects them, different imaging systems are used. 1. Multispectral vs. Hyperspectral Multispectral imaging (MSI) records information in a limited number of relatively broad, separate spectral bands , such as blue, green, red, near-infrared and shortwave infrared. Hyperspectral imaging (HSI) records information in many narrow and usually contiguous spectral bands . Therefore, it provides a much more detailed spectral signature of each pixel. The resulting dataset is commonly called a hyperspectral data cube (hypercube) because it contains: X-axis → spatial information Y-axis → spatial information Z-axis → wavelength/spectral information Thus, hype...

Discrete Detectors and Scanning mirrors Across the track scanner Whisk broom scanner.

Multispectral Imaging Using Discrete Detectors and Scanning Mirrors (Across-Track Scanner or Whisk Broom Scanner) Multispectral Imaging:  This technique involves capturing images of the Earth's surface using multiple sensors that are sensitive to different wavelengths of electromagnetic radiation.  This allows for the identification of various features and materials based on their spectral signatures. Discrete Detectors:  These are individual sensors that are arranged in a linear or array configuration.  Each detector is responsible for measuring the radiation within a specific wavelength band. Scanning Mirrors:  These are optical components that are used to deflect the incoming radiation onto the discrete detectors.  By moving the mirrors,  the sensor can scan across the scene,  capturing data from different points. Across-Track Scanner or Whisk Broom Scanner:  This refers to the scanning mechanism where the mirror moves perpendicular to the direction of flight.  This allows for t...

Thermal Infrared Remote Sensing

1. Principles Thermal Infrared Remote Sensing is based on the detection of naturally emitted electromagnetic radiation from objects, rather than reflected solar energy. According to Planck's Radiation Law , all objects with a temperature above absolute zero (0 K) emit electromagnetic radiation. For Earth surface features, the peak emission lies in the Thermal Infrared (TIR) region of 3–14 μm of the electromagnetic spectrum. The amount of radiation emitted is primarily a function of surface temperature and emissivity . Sensors measure the radiant energy flux density (W/m²) , which is later converted to surface temperature using Stefan-Boltzmann's Law . 2. Radiation Properties in TIR Emissivity (ε): Ratio of radiation emitted by a surface to that emitted by a perfect blackbody at the same temperature. Natural surfaces like water (ε ≈ 0.98) have high emissivity, while bare soils and metals have lower values. Blackbody: An idealized object th...

Satalite

Landsat → Land resources SPOT → High-resolution mapping IRS → Indian natural-resource mapping ASTER → Geology + thermal + DEM QuickBird → Very high spatial resolution MODIS → Daily global monitoring GOES → Weather monitoring AVHRR → Weather + vegetation + ocean AVIRIS → Hyperspectral imaging Highest spectral resolution: AVIRIS (224 narrow bands) Highest spatial resolution in this list: QuickBird (~0.61 m PAN) Highest temporal frequency: GOES (minutes) Best broad global monitoring: MODIS Indian sensors: IRS-LISS III and LISS IV Hyperspectral: AVIRIS Thermal + multispectral + DEM: ASTER abbreviations MSS – Multispectral Scanner System TM – Thematic Mapper ETM+ – Enhanced Thematic Mapper Plus GOES – Geostationary Operational Environmental Satellite AVHRR – Advanced Very High Resolution Radiometer HRV – High Resolution Visible HRVIR – High Resolution Visible and Infrared HRG – High Resolution Geometric ...