period 7 group 2
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This document discusses different types of precipitation including rain, snow, sleet, and hail. Rain falls as water droplets, snow is frozen water vapor forming snowflakes, sleet forms when rain passes through freezing air, and hail consists of pellets of ice.
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Precipitation and clouds
Precipitation can take several forms as water falls from clouds including rain, drizzle, sleet, hail and snow which are distinguished by the size and state of the falling water droplets. Clouds form when water vapor cools and condenses in the atmosphere, with the main cloud types being cumulus, stratus and cirrus clouds.
Lesson different forms of water
Groundwater is found underground in soil and rock cracks, while evaporation turns water into vapor due to heat. Condensation is when vapor turns back into liquid, and precipitation occurs when water is released from clouds as rain, snow or hail. Other forms of water include humidity in the air, snow as ice crystals, hail as ice and snow balls, dew as drops on surfaces at night, fog as low clouds reducing visibility, and frost as ice crystals on surfaces below freezing.
Clouds2
Clouds are made of tiny water or ice droplets formed through the water cycle of evaporation, condensation, and precipitation. There are four main types of clouds: cirrus, which are the highest and feathery white clouds; stratus, which are low gray blanket-like clouds; cumulus, which are puffy white clouds in the middle sky that change shape; and cumulonimbus, which are tall, dark, and fluffy clouds that can cause thunderstorms.
Educ373 Inquiry Project #3 & #4
Clouds are large collections of tiny water droplets or ice crystals that are light enough to float in the air. Clouds form when warm air rises and cools, causing water vapor to condense onto particles. Clouds appear white because they reflect all colors of light equally. Thicker clouds or those with other clouds blocking light above look gray. Clouds move with wind currents and are categorized by height, composition, and appearance into high, mid, low, and vertically developed clouds as well as miscellaneous types like contrails and mammatus clouds.
5aprno
1) When air is compressed or expands, it causes changes in temperature - compression warms air while expansion cools it.
2) Mountains cause air to rise and cool, which can lead to cloud formation and precipitation on the windward side, while the air is dry on the leeward side having lost most moisture.
3) When warm and cold air masses meet, they form fronts where the denser cold air acts as a barrier to the rising warm air, which can produce storms along the front.
Clouds
Clouds are made of tiny water or ice droplets that form from water vapor condensing in the sky. There are four main types of clouds: cirrus clouds are the highest and have a feathery appearance; stratus clouds are low and gray; cumulus clouds are puffy and change shape; and cumulonimbus clouds can span all levels and produce thunderstorms.
How are clouds formed
Clouds are formed when warm air rises and expands, causing water vapor to condense around tiny particles like dust. Billions of these tiny water droplets together form visible clouds. Clouds appear white because the water droplets scatter all the colors of light equally. Clouds turn gray when they are thick enough that light cannot pass through or when other clouds block light from above, casting shadows. Clouds float because the air and water droplets inside are warmer than the surrounding air, causing them to rise.
Ch 16 1 Water In Atmosphere
Humidity refers to the amount of water vapor in the air, measured as a percentage. Dew point is the temperature at which water vapor condenses to liquid or solid form, causing clouds to form. Different types of precipitation, like rain, snow, or hail occur when water droplets in clouds become too large for the clouds to support and fall to the earth's surface. There are three main types of clouds - cirrus, cumulus, and stratus - which form at different levels in the atmosphere and under varying weather conditions.
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Precipitation and clouds
Precipitation can take several forms as water falls from clouds including rain, drizzle, sleet, hail and snow which are distinguished by the size and state of the falling water droplets. Clouds form when water vapor cools and condenses in the atmosphere, with the main cloud types being cumulus, stratus and cirrus clouds.
Lesson different forms of water
Groundwater is found underground in soil and rock cracks, while evaporation turns water into vapor due to heat. Condensation is when vapor turns back into liquid, and precipitation occurs when water is released from clouds as rain, snow or hail. Other forms of water include humidity in the air, snow as ice crystals, hail as ice and snow balls, dew as drops on surfaces at night, fog as low clouds reducing visibility, and frost as ice crystals on surfaces below freezing.
Clouds2
Clouds are made of tiny water or ice droplets formed through the water cycle of evaporation, condensation, and precipitation. There are four main types of clouds: cirrus, which are the highest and feathery white clouds; stratus, which are low gray blanket-like clouds; cumulus, which are puffy white clouds in the middle sky that change shape; and cumulonimbus, which are tall, dark, and fluffy clouds that can cause thunderstorms.
Educ373 Inquiry Project #3 & #4
Clouds are large collections of tiny water droplets or ice crystals that are light enough to float in the air. Clouds form when warm air rises and cools, causing water vapor to condense onto particles. Clouds appear white because they reflect all colors of light equally. Thicker clouds or those with other clouds blocking light above look gray. Clouds move with wind currents and are categorized by height, composition, and appearance into high, mid, low, and vertically developed clouds as well as miscellaneous types like contrails and mammatus clouds.
5aprno
1) When air is compressed or expands, it causes changes in temperature - compression warms air while expansion cools it.
2) Mountains cause air to rise and cool, which can lead to cloud formation and precipitation on the windward side, while the air is dry on the leeward side having lost most moisture.
3) When warm and cold air masses meet, they form fronts where the denser cold air acts as a barrier to the rising warm air, which can produce storms along the front.
Clouds
Clouds are made of tiny water or ice droplets that form from water vapor condensing in the sky. There are four main types of clouds: cirrus clouds are the highest and have a feathery appearance; stratus clouds are low and gray; cumulus clouds are puffy and change shape; and cumulonimbus clouds can span all levels and produce thunderstorms.
How are clouds formed
Clouds are formed when warm air rises and expands, causing water vapor to condense around tiny particles like dust. Billions of these tiny water droplets together form visible clouds. Clouds appear white because the water droplets scatter all the colors of light equally. Clouds turn gray when they are thick enough that light cannot pass through or when other clouds block light from above, casting shadows. Clouds float because the air and water droplets inside are warmer than the surrounding air, causing them to rise.
Ch 16 1 Water In Atmosphere
Humidity refers to the amount of water vapor in the air, measured as a percentage. Dew point is the temperature at which water vapor condenses to liquid or solid form, causing clouds to form. Different types of precipitation, like rain, snow, or hail occur when water droplets in clouds become too large for the clouds to support and fall to the earth's surface. There are three main types of clouds - cirrus, cumulus, and stratus - which form at different levels in the atmosphere and under varying weather conditions.
period 7 group 5
Station models are symbolic illustrations used by meteorologists to plot multiple weather elements in a small space on weather maps. They allow analysis of patterns in air pressure, temperature, wind, cloud cover, and precipitation. Station models use internationally-accepted coding conventions to represent key weather data like temperature, dew point, wind, and precipitation. Weather maps display analysis of meteorological data to show features like fronts, temperature gradients, wind speed, and pressure patterns.
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Weather observations can be made by checking a thermometer, looking at cloud cover, and measuring wind speed. Meteorologists study weather data from tools like satellites and radar to create maps and improve forecasting of conditions like tornadoes and snow storms, which helps people prepare for dangerous weather and decide when to evacuate.
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A document discusses different types of weather fronts, mentioning warm fronts and cold fronts. It provides a brief overview of warm fronts and cold fronts without going into detail about their characteristics or how they form. The document is high-level and does not delve into explanations about these atmospheric phenomena.
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Humidity refers to the amount of water vapor in the air. The warmer the air temperature, the more water vapor it can hold before reaching saturation. Cooler air temperatures cause water vapor molecules to slow down and condense together, forming liquid water droplets through the process of condensation. Relative humidity measures the current water vapor content compared to the maximum amount possible at a specific temperature before saturation is reached.
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The document discusses key weather factors such as air temperature, wind, and humidity. It explains that air temperature is a measure of molecular motion, with higher temperatures indicating more rapid movement. It also describes how wind is caused by differences in air pressure from warm and cool air masses, and can be measured with an anemometer. Finally, it defines relative humidity as the amount of water vapor in the air compared to the maximum possible at a given temperature, with dew point referring to the temperature when air reaches saturation.
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Weather refers to the current atmospheric conditions including air pressure, wind, temperature and moisture. The sun provides energy that evaporates water, causing weather phenomena like snow, rain, hurricanes and hail. Atmospheric pressure is measured in hectopascals at sea level using precise instruments, and air moves from high to low pressure areas causing wind. Temperature reflects the energy of atmospheric particle motion, and moisture makes things slightly wet or damp.
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Cirrostratus clouds are very high clouds that can indicate either fair weather or an approaching storm. Altostratus clouds form at middle levels and can let sunlight pass through if not too thick. Fog forms at low levels when air reaches its dew point near the ground.
Period 3 Group 1
Weather refers to the current atmospheric conditions including air pressure, wind, temperature and moisture. The sun provides energy that evaporates water, causing weather phenomena like snow, rain, hurricanes and hail. Atmospheric pressure is measured in hectopascals at sea level using precise instruments, and air moves from high to low pressure areas causing wind. Temperature reflects the energy of atmospheric particle motion, and moisture makes things slightly wet or damp.
period 3 group 3
Cirrostratus clouds are very high clouds that can indicate either fair weather or an approaching storm. Altostratus clouds form at middle levels and can let sunlight pass through if not too thick. Fog forms at low levels when air cools to its dew point near the ground.
period 3 group 1
The document discusses how temperature affects air molecules and wind. When temperatures are lower, air molecules move more slowly, making it feel cooler. Temperature is a property of matter, as heat flows from hot to cool areas. Wind is caused by differences in air density as warmer, less dense air rises and cooler, denser air sinks, creating air movement in specific directions that can be measured with a wind vane or anemometer.
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The document discusses the water cycle, which is also known as the hydrologic cycle. It has no starting or ending point. The cycle includes evaporation where water in bodies of water is heated by the sun and turns to vapor, condensation where water vapor in the air cools and condenses to form clouds, and precipitation where clouds become too full and release water in forms such as rain, snow, hail, and snowflakes. Tables and examples of different types of precipitation are also included.
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Clouds form when warm air rises, expands, and cools, causing water vapor to condense into droplets that make up clouds. Clouds are classified by their shape and height, with some bringing rain or snow while others appear wispy on sunny days.
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Cold fronts occur when cold air cuts under warm air, forming cumulonimbus clouds that can cause thunderstorms or tornadoes. Warm fronts happen as warmer air advances over colder air. Occluded fronts include three air masses where colder air forces warm air upward. Stationary fronts remain stationary, causing light winds and precipitation.
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This document discusses 3 different air masses with varying temperatures that interact. A colder air mass forces warmer air upwards, blocking the warm air from reaching the surface. The 3 air masses mentioned are colder air, cool air, and warmer air that interact in some way.
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Relative humidity is a measure of the amount of water vapor in the air compared to the amount needed for saturation at a specific temperature. Dew point is the temperature at which air becomes saturated and condensation forms. Dew point is a better measure of moisture content because relative humidity can decrease as temperature increases even if dew point remains the same. Fog is likely when the air temperature and dew point temperature are the same, as cooling air to the dew point causes saturation because cooler air has less energy to overcome liquid bonds between water molecules.
Period 8 group 1
Weather is affected by factors like air pressure, wind, temperature, and moisture in the air. The sun provides energy that evaporates water into the atmosphere, where clouds form and later fall as rain or snow. It also heats the air, affecting local weather conditions. Air temperature influences daily life, as it is a measure of molecular motion - higher temperatures mean molecules move more rapidly, feeling warm, while lower temperatures mean slower motion and feeling cold. The record lowest worldwide temperature was -89.6°C in Antarctica, while the highest recorded anywhere was 162°F in Libya.
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period 7 group 5
Station models are symbolic illustrations used by meteorologists to plot multiple weather elements in a small space on weather maps. They allow analysis of patterns in air pressure, temperature, wind, cloud cover, and precipitation. Station models use internationally-accepted coding conventions to represent key weather data like temperature, dew point, wind, and precipitation. Weather maps display analysis of meteorological data to show features like fronts, temperature gradients, wind speed, and pressure patterns.
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period 7 group 6
A document discusses different types of weather fronts, mentioning warm fronts and cold fronts. It provides a brief overview of warm fronts and cold fronts without going into detail about their characteristics or how they form. The document is high-level and does not delve into explanations about these atmospheric phenomena.
period 7 group 1
Humidity refers to the amount of water vapor in the air. The warmer the air temperature, the more water vapor it can hold before reaching saturation. Cooler air temperatures cause water vapor molecules to slow down and condense together, forming liquid water droplets through the process of condensation. Relative humidity measures the current water vapor content compared to the maximum amount possible at a specific temperature before saturation is reached.
period 4 group 1
The document discusses key weather factors such as air temperature, wind, and humidity. It explains that air temperature is a measure of molecular motion, with higher temperatures indicating more rapid movement. It also describes how wind is caused by differences in air pressure from warm and cool air masses, and can be measured with an anemometer. Finally, it defines relative humidity as the amount of water vapor in the air compared to the maximum possible at a given temperature, with dew point referring to the temperature when air reaches saturation.
Pd 3 Group 1
Weather refers to the current atmospheric conditions including air pressure, wind, temperature and moisture. The sun provides energy that evaporates water, causing weather phenomena like snow, rain, hurricanes and hail. Atmospheric pressure is measured in hectopascals at sea level using precise instruments, and air moves from high to low pressure areas causing wind. Temperature reflects the energy of atmospheric particle motion, and moisture makes things slightly wet or damp.
Pd 3 Group 3
Cirrostratus clouds are very high clouds that can indicate either fair weather or an approaching storm. Altostratus clouds form at middle levels and can let sunlight pass through if not too thick. Fog forms at low levels when air reaches its dew point near the ground.
Period 3 Group 1
Weather refers to the current atmospheric conditions including air pressure, wind, temperature and moisture. The sun provides energy that evaporates water, causing weather phenomena like snow, rain, hurricanes and hail. Atmospheric pressure is measured in hectopascals at sea level using precise instruments, and air moves from high to low pressure areas causing wind. Temperature reflects the energy of atmospheric particle motion, and moisture makes things slightly wet or damp.
period 3 group 3
Cirrostratus clouds are very high clouds that can indicate either fair weather or an approaching storm. Altostratus clouds form at middle levels and can let sunlight pass through if not too thick. Fog forms at low levels when air cools to its dew point near the ground.
period 3 group 1
The document discusses how temperature affects air molecules and wind. When temperatures are lower, air molecules move more slowly, making it feel cooler. Temperature is a property of matter, as heat flows from hot to cool areas. Wind is caused by differences in air density as warmer, less dense air rises and cooler, denser air sinks, creating air movement in specific directions that can be measured with a wind vane or anemometer.
Pd.3 Group 3
The document discusses the water cycle, which is also known as the hydrologic cycle. It has no starting or ending point. The cycle includes evaporation where water in bodies of water is heated by the sun and turns to vapor, condensation where water vapor in the air cools and condenses to form clouds, and precipitation where clouds become too full and release water in forms such as rain, snow, hail, and snowflakes. Tables and examples of different types of precipitation are also included.
per 3 group 66
An isotherm is a line on a weather map connecting points of equal temperature, showing temperature patterns. An isobar is an imaginary line connecting places of equal barometric pressure, which can indicate wind speed and pressure in an area. Isotherms and isobars are lines used on weather maps and charts to depict temperature and pressure conditions.
period 3 group#3
Clouds form when warm air rises, expands, and cools, causing water vapor to condense into droplets that make up clouds. Clouds are classified by their shape and height, with some bringing rain or snow while others appear wispy on sunny days.
period 3 group 6
Meteorologists forecast the likelihood of future weather conditions based on observations of the atmosphere and its phenomena related to weather and climate. Today's weather in Pittsburgh will be reported on by meteorologists using their scientific knowledge of the atmosphere to analyze current conditions and predict future weather.
period 3 group 4
Fronts are boundaries between air masses of different densities, moisture, or temperatures. There are four main types of fronts:
Cold fronts occur when cold air cuts under warm air, forming cumulonimbus clouds that can cause thunderstorms or tornadoes. Warm fronts happen as warmer air advances over colder air. Occluded fronts include three air masses where colder air forces warm air upward. Stationary fronts remain stationary, causing light winds and precipitation.
pd 8 group 3
This document discusses 3 different air masses with varying temperatures that interact. A colder air mass forces warmer air upwards, blocking the warm air from reaching the surface. The 3 air masses mentioned are colder air, cool air, and warmer air that interact in some way.
Period 8 group 4
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Period 8 Group 1
Relative humidity is a measure of the amount of water vapor in the air compared to the amount needed for saturation at a specific temperature. Dew point is the temperature at which air becomes saturated and condensation forms. Dew point is a better measure of moisture content because relative humidity can decrease as temperature increases even if dew point remains the same. Fog is likely when the air temperature and dew point temperature are the same, as cooling air to the dew point causes saturation because cooler air has less energy to overcome liquid bonds between water molecules.
Period 8 group 1
Weather is affected by factors like air pressure, wind, temperature, and moisture in the air. The sun provides energy that evaporates water into the atmosphere, where clouds form and later fall as rain or snow. It also heats the air, affecting local weather conditions. Air temperature influences daily life, as it is a measure of molecular motion - higher temperatures mean molecules move more rapidly, feeling warm, while lower temperatures mean slower motion and feeling cold. The record lowest worldwide temperature was -89.6°C in Antarctica, while the highest recorded anywhere was 162°F in Libya.
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My slides at Nordic Testing Days 6.6.2024
Climate impact / sustainability of software testing discussed on the talk. ICT and testing must carry their part of global responsibility to help with the climat warming. We can minimize the carbon footprint but we can also have a carbon handprint, a positive impact on the climate. Quality characteristics can be added with sustainability, and then measured continuously. Test environments can be used less, and in smaller scale and on demand. Test techniques can be used in optimizing or minimizing number of tests. Test automation can be used to speed up testing.
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Observability Concepts EVERY Developer Should Know -- DeveloperWeek Europe.pdf
Monitoring and observability aren’t traditionally found in software curriculums and many of us cobble this knowledge together from whatever vendor or ecosystem we were first introduced to and whatever is a part of your current company’s observability stack.
While the dev and ops silo continues to crumble….many organizations still relegate monitoring & observability as the purview of ops, infra and SRE teams. This is a mistake - achieving a highly observable system requires collaboration up and down the stack.
I, a former op, would like to extend an invitation to all application developers to join the observability party will share these foundational concepts to build on:
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period 7 group 2
- 7. THE END