This document discusses the different types of biomes including hot and dry deserts, semi-arid deserts, and coastal deserts. It provides details on the climate, temperature, soil, rainfall, vegetation, and animals commonly found in each desert type. Deserts cover about one fifth of the Earth's surface and occur where annual rainfall is less than 50 cm. They experience daily temperature extremes, low humidity, shallow rocky soils with good drainage, and specialized plants and animals adapted to the harsh conditions.
desert ecosystem
Deserts and semi arid lands are extremely specialised and sensitive ecosystems that are easily destroyed by human activities. The plants and animals that inhabit these dry areas can live only in this ecosystem.
Desert ecosystem, is usually believed to be barren, but this fragile ecosystem supports numerous amazing living creatures, known for their adaptability.
Deserts alone covers about seventh of the land surface. We normally call deserts as “sand seas or oceans of sands”. Most of the major desert areas like as the Sahara, the Arabian, the Kalahari, and the Deserts of Australia all lie between 10 and 30 degrees north or south of the equator. Deserts are dry ecosystems comprising a substantial part of the globe
Effect of Precipatation on Distribution of Plants.pptxCHZaryabAli
Useful for the students who wants to study this topic & enhances the knowledge for a specific topic.
PRECIPITATION:
is any product of the condensation of atmospheric water that falls under gravity from clouds.
The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates". Thus, fog and mist are not precipitation but suspensions, because the water vapor does not condense sufficiently to precipitate.
Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air.
REASON FOR CHANGE IN PRECIPITATION:There are many reasons for changes in precipitation. The leading cause is a change in temperature. Many scientists believe an increase in temperature could lead to a more intense water cycle. The rates of evaporation from soils and water, as well as transpiration from plants, could increase. The amount of precipitation could also increase. Predicted changes in the water cycle differ according to the region of the planet being examined. Many scientists believe rates of evaporation will be greater than precipitation in the middle latitudes such as the United States. This could result in drier summers in these regions. Of course, predicted changes in the water cycle also differ according to the climate.EFFECT OF PRECIPITATION ON PLANTS:Precipitation, especially rain, has a dramatic effect on plants distribution. All plants need at least some water to survive, therefore rain (being the most effective means of watering) is important to agriculture. While a regular rain pattern is usually vital to healthy plants, too much or too little rainfall can be harmful, even devastating to crops. Drought can kill crops and increase erosion, while overly wet weather can cause harmful fungus growth. Plants need varying amounts of rainfall to survive. For example, certain cacti require small amounts of water, while tropical plants may need up to hundreds of inches of rain per year to survive.In areas with wet and dry seasons, soil nutrients diminish and erosion increases during the wet season.
DISTRIBUTION OF PLANTS IN DIFFERENT BIOMES:The geographical distribution (and productivity) of the plants in the various biomes is controlled primarily by the climatic variables precipitation and temperature. There are 8 major terrestrial biomes >Tropical Rain Forest >Tropical Savanna > Deserts >Grass Lands > Chaparral > Temperate Deciduous Forests > Temperate Boreal Forests > Artic And Alpine TundraEach biome plants have different adaptation to survive in that environment.
Tundra means marshy plain. The geographical distribution of the tundra biome is largely poleward of 60° North latitude.
The tundra biome is characterized by an absence of trees, the presence of dwarf plants
Introduction to Philosophy of the Human Person
Human Person
Human Living
Human Freedom
Intersubjectivity of the Human Person
Human Person in his/her environment
Human Person in the Society
Human Person as Oriented towards their Impending death
Students, digital devices and success - Andreas Schleicher - 27 May 2024..pptxEduSkills OECD
Andreas Schleicher presents at the OECD webinar ‘Digital devices in schools: detrimental distraction or secret to success?’ on 27 May 2024. The presentation was based on findings from PISA 2022 results and the webinar helped launch the PISA in Focus ‘Managing screen time: How to protect and equip students against distraction’ https://www.oecd-ilibrary.org/education/managing-screen-time_7c225af4-en and the OECD Education Policy Perspective ‘Students, digital devices and success’ can be found here - https://oe.cd/il/5yV
The Roman Empire A Historical Colossus.pdfkaushalkr1407
The Roman Empire, a vast and enduring power, stands as one of history's most remarkable civilizations, leaving an indelible imprint on the world. It emerged from the Roman Republic, transitioning into an imperial powerhouse under the leadership of Augustus Caesar in 27 BCE. This transformation marked the beginning of an era defined by unprecedented territorial expansion, architectural marvels, and profound cultural influence.
The empire's roots lie in the city of Rome, founded, according to legend, by Romulus in 753 BCE. Over centuries, Rome evolved from a small settlement to a formidable republic, characterized by a complex political system with elected officials and checks on power. However, internal strife, class conflicts, and military ambitions paved the way for the end of the Republic. Julius Caesar’s dictatorship and subsequent assassination in 44 BCE created a power vacuum, leading to a civil war. Octavian, later Augustus, emerged victorious, heralding the Roman Empire’s birth.
Under Augustus, the empire experienced the Pax Romana, a 200-year period of relative peace and stability. Augustus reformed the military, established efficient administrative systems, and initiated grand construction projects. The empire's borders expanded, encompassing territories from Britain to Egypt and from Spain to the Euphrates. Roman legions, renowned for their discipline and engineering prowess, secured and maintained these vast territories, building roads, fortifications, and cities that facilitated control and integration.
The Roman Empire’s society was hierarchical, with a rigid class system. At the top were the patricians, wealthy elites who held significant political power. Below them were the plebeians, free citizens with limited political influence, and the vast numbers of slaves who formed the backbone of the economy. The family unit was central, governed by the paterfamilias, the male head who held absolute authority.
Culturally, the Romans were eclectic, absorbing and adapting elements from the civilizations they encountered, particularly the Greeks. Roman art, literature, and philosophy reflected this synthesis, creating a rich cultural tapestry. Latin, the Roman language, became the lingua franca of the Western world, influencing numerous modern languages.
Roman architecture and engineering achievements were monumental. They perfected the arch, vault, and dome, constructing enduring structures like the Colosseum, Pantheon, and aqueducts. These engineering marvels not only showcased Roman ingenuity but also served practical purposes, from public entertainment to water supply.
How to Create Map Views in the Odoo 17 ERPCeline George
The map views are useful for providing a geographical representation of data. They allow users to visualize and analyze the data in a more intuitive manner.
2024.06.01 Introducing a competency framework for languag learning materials ...Sandy Millin
http://sandymillin.wordpress.com/iateflwebinar2024
Published classroom materials form the basis of syllabuses, drive teacher professional development, and have a potentially huge influence on learners, teachers and education systems. All teachers also create their own materials, whether a few sentences on a blackboard, a highly-structured fully-realised online course, or anything in between. Despite this, the knowledge and skills needed to create effective language learning materials are rarely part of teacher training, and are mostly learnt by trial and error.
Knowledge and skills frameworks, generally called competency frameworks, for ELT teachers, trainers and managers have existed for a few years now. However, until I created one for my MA dissertation, there wasn’t one drawing together what we need to know and do to be able to effectively produce language learning materials.
This webinar will introduce you to my framework, highlighting the key competencies I identified from my research. It will also show how anybody involved in language teaching (any language, not just English!), teacher training, managing schools or developing language learning materials can benefit from using the framework.
We all have good and bad thoughts from time to time and situation to situation. We are bombarded daily with spiraling thoughts(both negative and positive) creating all-consuming feel , making us difficult to manage with associated suffering. Good thoughts are like our Mob Signal (Positive thought) amidst noise(negative thought) in the atmosphere. Negative thoughts like noise outweigh positive thoughts. These thoughts often create unwanted confusion, trouble, stress and frustration in our mind as well as chaos in our physical world. Negative thoughts are also known as “distorted thinking”.
This is a presentation by Dada Robert in a Your Skill Boost masterclass organised by the Excellence Foundation for South Sudan (EFSS) on Saturday, the 25th and Sunday, the 26th of May 2024.
He discussed the concept of quality improvement, emphasizing its applicability to various aspects of life, including personal, project, and program improvements. He defined quality as doing the right thing at the right time in the right way to achieve the best possible results and discussed the concept of the "gap" between what we know and what we do, and how this gap represents the areas we need to improve. He explained the scientific approach to quality improvement, which involves systematic performance analysis, testing and learning, and implementing change ideas. He also highlighted the importance of client focus and a team approach to quality improvement.
3. • Deserts cover about one fifth of the Earth's
surface and occur where rainfall is less than
50 cm/year. Although most deserts, such as
the Sahara of North Africa and the deserts of
the south-western U.S., Mexico, and
Australia, occur at low latitudes, another
kind of desert, cold deserts, occur in the
basin and range area of Utah and Nevada and
in parts of western Asia.
4. Most deserts have a considerable amount
of specialized vegetation, as well as
specialized vertebrate animals.
Disturbances are common in the form of
occasional fires or cold weather, and
sudden, infrequent, but intense rains that
cause flooding.
5. • There are major types of deserts:
• Hot and dry
• Semiarid
• Coastal
6. HOT AND DRY DESERT
Temperatures exhibit daily extremes because the atmosphere
contains little humidity to block the Sun's rays.
Rainfall is usually very low and/or concentrated in short
bursts between long rainless periods
Soils are course-textured, shallow, rocky or gravely with good
drainage and have no subsurface water. They are coarse
because there is less chemical weathering.
Canopy in most deserts is very rare. Plants are mainly ground-
hugging shrubs and short woody trees.
The animals include small nocturnal (active at night)
carnivores. The dominant animals are burrowers and kangaroo
rats. There are also insects, arachnids, reptiles and birds. The
animals stay inactive in protected hideaways during the hot
day and come out to forage at dusk, dawn or at night, when
the desert is cooler.
7. SEMI ARID DESERT
The summers are moderately long and dry, and like hot
deserts, the winters normally bring low concentrations of
rainfall. Summer temperatures usually average between 21-
27° C. It normally does not go above 38° C and evening
temperatures are cool, at around 10° C.
The soil can range from sandy and fine-textured to loose
rock fragments, gravel or sand.
The spiny nature of many plants in semiarid deserts
provides protection in a hazardous environment. The large
numbers of spines shade the surface enough to significantly
reduce transpiration.
Naturally, many animals find protection in underground
burrows where they are insulated from both heat and
aridity.
8. COASTAL DESERT
The cool winters of coastal deserts are followed by
moderately long, warm summers.
The average rainfall measures 8-13 cm in many areas.
The soil is fine-textured with a moderate salt content. It
is fairly porous with good drainage. Some plants have
extensive root systems close to the surface where they
can take advantage of any rain showers.
The plants are widely scattered.
Some animals have specialized adaptations for dealing
with the desert heat and lack of water. Some toads seal
themselves in burrows with gelatinous secretions and
remain inactive for eight or nine months until a heavy
rain occurs. Amphibians that pass through larval stages
have accelerated life cycles, which improves their chances
of reaching maturity before the waters evaporate
9. CLIMATE
Too Dry
Disturbances are common in the
form of occasional fires or cold
weather, and sudden, infrequent,
but intense rains that cause
flooding.
10. TEMPERATURE
Hot desert climates feature hot, typically
exceptionally hot, periods of the year. In
many locations featuring a hot desert
climate, maximum temperatures of over
40 °C (104 °F) aren't uncommon in
summer and can even soar to over 45 °C
(113 °F) in the hottest regions.
11. SOIL
Soils often have abundant
nutrients because they need
only water to become very
productive and have little or no
organic matter.
Little to no topsoil due to high
winds mineral not deep in soil.
12. RAINFALL
rainfall is less than 50 cm/year.
VEGETATION
Most deserts have a considerable
amount of specialized vegetation
15. Adaptation
Animal Adaptation
• Get water from food
• Thick outer coat
• Burrow during day
• Large ears
• Small animals less surface area
Plant Adaptation
• Spines
• Succulents
• Thick waxy cuticle
• Shallow broad roots
16. Samples
Sand dunes in Death Valley National
Monument, California.
Sahara Desert, North Africa
Gobi Desert, Mongolia / N.E China Chihuahuan Desert, Mexico
17. The Master Minds:
Braza,John Arbel
Carandan, Archibald
Medrano, Mary Rosalynd
Mendoza, Jhinzen Khallil
Roxas, Anna Marie