Climate ppt.pptx
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Climate is defined as the statistics of weather over long periods of time, measured by assessing patterns of temperature, humidity, atmospheric pressure, wind, precipitation, and other meteorological variables in a given region over many years. It differs from weather, which describes atmospheric conditions over shorter periods ranging from a day to a few weeks. Factors that affect climate include latitude, altitude, distance from large bodies of water, topography, and ocean currents.
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Isotope geochemistry can be used for geochronology, understanding solar system and continent evolution, tracing the history of life, unraveling climate history, and determining the origin of mineral and energy resources. The history of isotope geochemistry began with the discovery of radioactivity and production of the first radiometric age for the Earth. Isotopes have differing numbers of neutrons. Nuclear stability depends on the balance of nuclear forces. Radioactive decay follows exponential laws. Isotope ratios are altered by geological processes and can be used to study earth systems. Stable and radioactive isotopes are produced via stellar nucleosynthesis during the lives of stars and their deaths as supernovae.
firemeup.pptx
The document discusses fire hazards and prevention. It defines the elements of the fire triangle as fuel, heat, and oxygen. It identifies various causes of fires such as matches, electrical faults, arson, open flames, fireworks, and static electricity. It provides examples of fuel sources like wood, grass, and kerosene. The document also discusses preventing fires at home through safe practices and what to do in the event of a fire, such as calling emergency services. Safety measures and standard fire safety procedures are emphasized.
RV.pptx
Volcanic eruptions can produce several hazardous events such as pyroclastic flows, lava flows, lahars, ash falls, and noxious gas emissions. Pyroclastic flows are among the most dangerous as they can travel far at high speeds while still hot, burying and burning everything in their path as seen at Pompeii. Lava flows are generally less explosive but can still destroy infrastructure in their path. Lahars, or volcanic mudflows, are deadly as they can flow rapidly while carrying large debris. Volcano monitoring helps observe seismic activity, deformation, and gas outputs to detect signs of impending eruptions and warn of potential hazards.
chap01.ppt
This PowerPoint presentation discusses the process of identifying and correcting hazards. It defines a hazard and explains that the goal of hazard identification is to precisely identify potential harm to workers, equipment, and the environment. The presentation outlines several methods for identifying hazards, such as reviewing injury records, inspecting new processes, and complying with regulations. It also describes how to develop an action plan to address identified hazards through corrective measures, assigned responsibilities, and target dates. Additionally, the presentation explains how to perform a job safety analysis (JSA) by selecting a job, breaking it into steps, identifying potential hazards, and developing solutions.
judiciary.pptx
The Philippine judicial system blends elements of civil law from Spanish influence and common law from American influence. It has a hierarchical structure consisting of lower courts, regional trial courts, appellate courts, specialized courts, and the Supreme Court. In recent decades, reforms have aimed to improve judicial qualifications, independence, accountability, and efficiency. However, issues remain regarding political influence, lack of resources, and case backlogs.
EPPG.pptx
The document traces the evolution of politics and governance in the Philippines from pre-historic times to the present. It discusses the early barangay system ruled by datus, the centralized government established under Spanish colonial rule headed by a governor-general, the revolutionary governments that formed in opposition to Spanish rule led by Aguinaldo, the American colonial period when civil and military governments were established, the creation of the Commonwealth government in 1935 in preparation for independence, the Japanese occupation during World War 2, and provides a list of the 16 presidents of the Philippines since independence.
mitigation.pptx
This document discusses disaster mitigation strategies. It begins by defining disaster management and outlining its objectives. It then distinguishes between structural and non-structural mitigation measures. Structural mitigation involves construction projects to reduce disaster impacts, and includes selecting safe building sites, orienting structures properly, ensuring stability, and building cyclone shelters. Non-structural mitigation seeks to modify human behavior through land use regulations, hazard zoning, and education. The document provides several examples of both structural and non-structural mitigation techniques used in India to reduce disaster risks.
vulnerability in disaster.pptx
This document defines vulnerability and discusses it from different perspectives. Vulnerability refers to the susceptibility of individuals, communities, or systems to harm from hazards. It is determined by physical, social, economic, and environmental factors that influence the ability to prepare for, respond to, and recover from disasters. The document outlines four main types of vulnerability: physical, economic, social, and environmental. Understanding vulnerability is important for assessing disaster risk. Approaches to reducing vulnerability include building codes, insurance, economic diversity, awareness raising, and preparedness measures.
Earthquakes (10).ppt
Logarithmic scales are useful for measuring large ranges of values because they compress large spreads into more even spaces. They align with human perception in fields like sound measurement, where equal ratios in frequency correspond to equal changes in pitch. The Richter scale and Modified Mercalli scale are used to describe earthquake magnitudes and intensities. The Richter scale quantifies seismic energy based on amplitude readings, while the Mercalli scale qualitatively rates observed effects on people and structures on a 12-point scale.
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+
53.13485
−
27.82088
with a host spectroscopic redshift of
2.903
±
0.007
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�
(
�
−
�
)
∼
0.9
) despite a host galaxy with low-extinction and has a high Ca II velocity (
19
,
000
±
2
,
000
km/s) compared to the general population of SNe Ia. While these characteristics are consistent with some Ca-rich SNe Ia, particularly SN 2016hnk, SN 2023adsy is intrinsically brighter than the low-
�
Ca-rich population. Although such an object is too red for any low-
�
cosmological sample, we apply a fiducial standardization approach to SN 2023adsy and find that the SN 2023adsy luminosity distance measurement is in excellent agreement (
≲
1
�
) with
Λ
CDM. Therefore unlike low-
�
Ca-rich SNe Ia, SN 2023adsy is standardizable and gives no indication that SN Ia standardized luminosities change significantly with redshift. A larger sample of distant SNe Ia is required to determine if SN Ia population characteristics at high-
�
truly diverge from their low-
�
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Climate ppt.pptx
- 1. WEATHER is the atmospheric conditions, including the temperature, wind, snow, rain, or anything else happening outside OVER A SHORT PERIOD OF TIME OR FROM DAY TO DAY
- 2. CLIMATE IS THE STATISTICS OF WEATHER OVER LONG PERIODS OF TIME. IT IS MEASURED BY ASSESSING THE PATTERNS OF VARIATION IN TEMPERATURE, HUMIDITY, ATMOSPHERIC PRESSURE, WIND, PRECIPITATION, ATMOSPHERIC PARTICLE COUNT AND OTHER METEOROLOGICAL VARIABLES IN A GIVEN REGION OVER LONG PERIODS OF TIME.
- 3. What are the factors that affect climate?
- 4. 1. LATITUDE How latitude affects climate?
- 6. 2. ALTITUDE How does altitude affects climate?
- 7. Mt. Kilimanjaro is located in Africa and found near the equator. It stands 5895m above sea level. The peak of this mountain is covered by ice.
- 9. The air temperature decreases as the altitude increases. For every 1000 m, there is a drop of 6.50C. At higher elevations, there is less air. The air molecules are farther apart, thus making the air less dense. Lighter air cannot absorb much heat, making air temperature lower. Ultimately, the decrease in air temperature is due to the decrease in air pressure.
- 10. 3. DISTANCE FROM BODIES OF WATER.
- 12. 4. TOPOGRAPHY.