UNR and DRI Weather Comparison Jan 2010

Slides:

Advertisements

Similar presentations

Factors that Affect Climate

Advertisements

High Pressure or Anticyclones

Urban Heat Island Effect (城市熱島效應)

Weather Vocabulary Words Meteorologist Weather Temperature Wind Front Anemometer Precipitation Cloud coverage Weather Map.

Chapter 12: Air Pollution A brief history of air pollution A brief history of air pollution Types and sources of air pollutants Types and sources of air.

Air Masses and Weather Fronts. The study of weather is meteorology Someone who studies weather is called a meteorologist.

Transport of Air Pollutants

Vertical Air Motion. Air Parcels Ascend/Descend Adiabatically Expansional CoolingCompressional heating.

Weather Cloud Formation May 19, Adiabatic Temperature Changes When air is allowed to expand, it cools, and when its is compressed, it warms. Do.

Climate Change. LOOKING AHEAD UNIT D Climate Change CHAPTER 9 Earth’s Climate: Out of Balance CHAPTER 8 Earth’s Climate System and Natural Changes CHAPTER.

Visibility ATC Chapter 5.

4-4.3 Compare daily and seasonal changes in weather conditions (including wind speed and direction, precipitation, and temperature) and patterns.

Air Masses and Fronts Weather. How Do Air Masses Affect Weather? Weather maps show that cities across a large region share the same weather and they also.

Chapter 1 The Atmosphere.

Air Pressure: The weight of the air in the atmosphere pressing down. At sea level the air pressure is mb (millibars) = 1 atmosphere 1 atmosphere.

Lapse Rates and Stability of the Atmosphere

Warm Up 3/14 Which gas is most important for understanding atmospheric processes? a. water vapor c. carbon dioxide b. oxygen d. ozone What is true.

Air Pollution Potential and Fire Weather Forecasting Anthony R. Lupo Atms Sci 4310 / 7310 Lab 9.

Air Masses and Weather Fronts Study Guide Notes. The study of weather is meteorology Someone who studies weather is called a meteorologist.

Air Quality CH 15 Prentice Hall p CH 15 Prentice Hall p At ppt.

Breezes and Fronts Jeopardy.  At Night What time of day do land breezes occur?

Chapter 11 Section 2 State of Atmosphere. Temperature vs. Heat Temperature: measures the movement of molecules  Faster = Warmer  Slower = Colder  Measured.

Objectives Review Vocabulary

Weather Data and Climate Weather changes from day to day… Climate does not change!

Today’s Weather. What causes the weather? 4F53-B998-E6D91AE43323&blnFromSearch=1&productcode=US.

Properties of the Atmosphere

CLOUDS. What are clouds?

Weather The amount that air presses on the earth is called… Air pressure.

Introduction #2 B The Earth’s Atmosphere. The thickness of our Atmosphere.

_____ The lifting condensation level is the level at which, if an air parcel is forced to lift to it, it will keep going

Twenty Questions What do you know about the weather?

Composition/Characterstics of the Atmosphere 80% Nitrogen, 20% Oxygen- treated as a perfect gas Lower atmosphere extends up to  50 km. Lower atmosphere.

Ecology: Abiotic Factors. Ecology: Abiotic Factors Unit Concept: Everything is connected to the non-living environment.

Group#4 Homework ATMS 411 Sebastian White, Kelsey Anderson, Maritza Andicoechea, Saleh Alzahrani.

Atmospheric Stability, Clouds and Lapse Rates. Hot Air Rises or

Inversions. Usually temperature decreases with height by approximately 5.5 C per km But with high pressure, clear or near clear skies, and light winds,

Atmospheric Stability The resistance of the atmosphere to vertical motion. Stable air resists vertical motion Unstable air encourages vertical motion.

Weather in Atlantic Canada Chapter 3. Condensation Occurs when moist air rises and cools, forming clouds. Air rises because of being warmed from below.

Temperature Rainfall Wind WEATHER AND CLIMATE. Relevance of Weather.

Air Masses and Fronts D 68-73

Atmospheric Stability and Air Masses

Lecture 5 reading assignm: A&K finish Ch 3, Ch 4. Hartmann 3.8, 3.9, 3.10, 3.12 Lapse rate, change in T with height Atmospheric water: quantifying water.

STATE OF THE ATMOSPHERE Advanced Earth Science. Temperature vs. Heat  NOT THE SAME THING!!  Temperature measures how fast or slow molecules move around.

A Major Component of Earth’s Weather. The Hydrologic Cycle Water can exist as a solid, liquid, or gas on Earth. The movement of water from different reservoirs.

Whether it’s cold or whether it’s hot, we shall have weather whether or not!

Weather Symbols and Station Models. Why do we use Symbols? Less space Universal language Why do we use station models Gives us a small picture of weather.

Energy Notes 4.

Monday’s lesson (At the end the lesson you will be able to…) Describe the changes in temperature with height through the lower layers of the atmosphere.

Presented by Supervisor Vinay Pratap Singh Prof. Krishan Kumar

Precipitation Presentation

Lesson 1 Task 1 Can you draw a fully labelled diagram to show the ‘day model’ of radiation balance in the earth’s energy budget in 5 minutes on these.

Cloud Formation.

DO NOW Pick up notes and Review #20. Turn in any completed work.

Weather in Atlantic Canada

Section 2: Properties of the Atmosphere

Layers of the Atmosphere

Structure of the Atmosphere

ATOC 4720: class 14 Saturated-adiabatic and pseudoadiabatic processes

Weather and Weather Factors

Section 2: Properties of the Atmosphere

Location, Location, Location

The Meteorology Leading up to and on Measurement Day

Atmospheric Stability

Homework Sunday, April 28, 2019 Finish Gizmo - Clouds

New CoHA Product Access Page & Representativeness Analysis

Climates of Western Canada: Factors Affecting Temperature

Do Now (10 min) Write in the title: “Weather: Temperature” Write in the objective: “Objective: Explain four factors that affect temperature, and demonstrate.

At 1 1.2ppt Air Quality W&C Chapter 1.2 Pages

Presentation transcript:

UNR and DRI Weather Comparison Jan 2010 Why temperature? DRI is about 143.3 meters above UNR. Adiabatic lapse rate 9.8 C/km, UNR is warmer by 1.4 C ???

UNR and UNR Farm

UNR Weather Station Location tractor

Schematic of a Weather Station see http://www.cemp.dri.edu/cemp/recent/

Air Temperature at DRI and UNR in Jan 2010 UNR is warmer at mid day, but DRI is warmer at night.

(DRI - UNR) + 1.4 C = 0 ???? Monster Inversions!! No Wind!

Air Pollution Consequence of Stagnation and Inversion: Total Particle Mass Concentration (PM 2.5 um) Summer Wild Fire Mexico City Reno

And the Black Carbon Particle Mass Concentration Mexico City ventilates better than Reno. This woodsmoke was mostly not Black Carbon.

Close with Diffraction from Cloud Droplets Using the Moon as a Light Source: 27 Jan 10