Land use change suppresses precipitation

Size: px
Start display at page:

Download "Land use change suppresses precipitation"

Transcription

1 Land use change suppresses precipitation W. Junkermann, 1 J. Hacker, 2 T. Lyons 3 and Udaysankar Nair 4 FZK, IMK-IFU, Garmisch- Partenkirchen, Germany 1 Airborne Research Australia, Flinders University, Adelaide, Australia 2 Murdoch University, Perth, Australia 3 National Space Science Technology Center, Huntsville, Alabama, USA 4

2 Outline Background Experimental setup Results Summary

3 RAINFALL Bates et al. Climatic Change, 89, 28, RUNOFF DROUGHT IN WESTERN AUSTRALIAN WHEAT BELT FORSCHUNGSZENTRUM KARLSRUHE IMK-IFU

4 Precipitation change distribution -clouds over natural vegetation + - IOCI, 22

5 The BUFEX experiment 12/26, 8/27 airborne investigations in a natural laboratory comparing meteorology and aerosols 2 seasons homogeneous landscape <- 1 km 4 km -> > 8 km Lake King Airstrip ~25 km ->

6 Background Experimental setup Results Summary

7 AUSTRALIA BUFEX CAMPAGNE, 26/27

8 AUSTRALIA BUFEX CAMPAGNE, 26/27 GRIMM SMPS, nm 2 min GRIMM 1.18, 3 nm 15 um 6 sec TSI 31 > 1 nm 2 sec FSSP um 1 sec Meteorology (temp, dewpoint) and radiation parameters (radiation balance, albedo)

9 Background Experimental setup Results Summary

10 PARTICLES > 1 nm (red) ALTITUDE [m] WEST ~ NUMBER OF PARTICLES TSI CPC COUNTS PBL 4 km NO nm-size PARTICLES OVER THE FOREST!!! VERTICAL MIXED UP TO PBL ALTITUDE [m] EAST PBL 1 2 NUMBER OF PARTICLES

11 PARTICLES > 1 nm (red) km NO nm SIZE PARTICLES OVER THE FOREST!!! SIZE DISTRIBUTIONS (dn/dln(dp) [/cm 3 ] WEST ultrafines Channel [nm] (dn/dln(dp) [/cm 3 ] EAST Channel [nm]

12 PARTICLES > 1 nm (red) (dn/dln(dp) [/cm 3 ] Channel [nm] 4 km - INDEPENDENT FROM SEASON -NO DEPENDENCE ON VEGETATION ON AGRICULTURE (dn/dln(dp) [/cm 3 ] SIZE DISTRIBUTIONS OVER THE AGRICULTURE Channel [nm]

13 SOURCE REGIONS FOR NUCLEATION- PARTICLES SUMMER WINTER

14 a (dn/dln(dp) [/cm 3 ] c (dn/dln(dp) [/cm 3 ] Number Size Distribution 11: New particle production Channel [nm] Number Size Distribution 14: aged new particles CCN Channel [nm] Particle Diameter (nm) b (dn/dln(dp) [/cm 3 ] d Number Size Distribution 1 : 6: 12: 18: 24: east / morning + afternoon Channel [nm] LAKE STUBBS

15 NUCLEATION AEROSOL EFFECT ON PRECIPITATION -> HIGHER DROPLET NUMBER AND REDUCTION OF DROPLET SIZES DUE TO ENHANCED CCN (FLETCHER, 1962, Lohmann and Feichter, 25.) ALTITUDE [m a.s.l.] E W E HORIZONTAL W CCN [/cm3] PARTICLES > 1 nm [/cm3] CCN as particles > 5 nm

16 CLOUDS OVER BOTH AREAS, CLOUDS OVER BOTH AREAS, Experimental proof

17 NUMBER OF DROPLETS [/cm3] a WEST NUMBER OF DROPLETS LIQUID WATER CONTENT EAST :45 4:15 4:45 5:15 5:45 UTC UTC diff 8 h LWC [g/m3] METEOROLOGIC DIFFERENCES

18 NUMBER OF DROPLETS [/cm3] CCN 4/cm3 WEST Number of droplets per size bin WEST NUMBER OF DROPLETS LIQUID WATER CONTENT EAST Droplet size (diameter) [um] EAST UTC diff 8 h CCN 28/cm3 LWC [g/m3]

19 Parameter Temperature (air) [ o C] Pressure [hpa] Dewpoint [ o C] West (agriculture) East (natural vegetation) ground cloud base ground cloud base Water [g/m3] CCN Cloud droplets [/cm3] ~ 4 ~ Average diameter [um] Liquid water content [g/m3].1.15 Note the difference of water vapor converted into LWC

20 Background Experimental setup Results > Landuse change Summary

21 SOURCE REGIONS FOR NUCLEATION- PARTICLES SUMMER WINTER

22 DIFFERENCES BETWEEN THE LAKES? MOIST DRY High GROUNDWATER TABLE low ~ 2 m > 2 m

23 DIFFERENCES BETWEEN THE LAKES? MOIST DRY High GROUNDWATER TABLE low ~ 2 m DEFORESTATION > 2 m

24 SUMMARY Enhanced ultrafine particle numbers over agriculture Nucleation source not related to vegetation Salt lake chemistry / emissions, most probably halogen (iodine?) chemistry Enhanced CCN numbers affect cloud microphysics Modification of cloud microphysics can explain the observed precipitation patterns

25 Long term experiment, natural laboratory Deforestation >rising ground water table (GWT) ->GWT close to surface ~ 197 ->wet chemistry in salt lakes ->increased number of CCN -> ->reduction of precipitation

26 Acknowledgement Admiral James Stirling Settlers who helped clearing the forest National Science Foundation grant ATM and Australian Research Council's Discovery funding scheme (project DP664515) One of the aircraft was donated by the late Ms. Joyce Schultz

27 Thank you for your attention 1827

28

29 NUMBER OF DROPLETS [/cm3] ALTITUDE [m a.s.l.] NUMBER OF DROPLETS LIQUID WATER CONTENT :45 4:15 4:45 5:15 5:45 UTC UTC diff 8 h a DEWPOINT WEST b c d 3 6 CCN [/cm3] EAST DROPLETS [/cm3] LWC [g/m3] CLOUD BASE EAST WEST

CLIMATE. UNIT TWO March 2019

CLIMATE. UNIT TWO March 2019 CLIMATE UNIT TWO March 2019 OUTCOME 9.2.1Demonstrate an understanding of the basic features of Canada s landscape and climate. identify and locate major climatic regions of Canada explain the characteristics

More information

Satellite analysis of aerosol indirect effect on stratocumulus clouds over South-East Atlantic

Satellite analysis of aerosol indirect effect on stratocumulus clouds over South-East Atlantic 1/23 Remote sensing of atmospheric aerosol, clouds and aerosol-cloud interactions. Bremen, 16-19 December 2013 Satellite analysis of aerosol indirect effect on stratocumulus clouds over South-East Atlantic

More information

Implications of Sulfate Aerosols on Clouds, Precipitation and Hydrological Cycle

Implications of Sulfate Aerosols on Clouds, Precipitation and Hydrological Cycle Implications of Sulfate Aerosols on Clouds, Precipitation and Hydrological Cycle Source: Sulfate aerosols are produced by chemical reactions in the atmosphere from gaseous precursors (with the exception

More information

UNIT 12: THE HYDROLOGIC CYCLE

UNIT 12: THE HYDROLOGIC CYCLE UNIT 12: THE HYDROLOGIC CYCLE After Unit 12 you should be able to: o Effectively use the charts Average Chemical Composition of Earth s Crust, Hydrosphere and Troposphere, Selected Properties of Earth

More information

Ultrafine particles over Eastern Australia: an airborne survey

Ultrafine particles over Eastern Australia: an airborne survey Tellus B: Chemical and Physical Meteorology ISSN: (Print) 1600-0889 (Online) Journal homepage: https://www.tandfonline.com/loi/zelb20 Ultrafine particles over Eastern Australia: an airborne survey Wolfgang

More information

1., annual precipitation is greater than annual evapotranspiration. a. On the ocean *b. On the continents

1., annual precipitation is greater than annual evapotranspiration. a. On the ocean *b. On the continents CHAPTER 6 HUMIDITY, SATURATION, AND STABILITY MULTIPLE CHOICE QUESTIONS 1., annual precipitation is greater than annual evapotranspiration. a. On the ocean *b. On the continents 2., annual precipitation

More information

Climate 1: The Climate System

Climate 1: The Climate System Climate 1: The Climate System Prof. Franco Prodi Institute of Atmospheric Sciences and Climate National Research Council Via P. Gobetti, 101 40129 BOLOGNA SIF, School of Energy, Varenna, July 2014 CLIMATE

More information

Preliminary Observations of Cloud and Precipitation Characteristics in the Brisbane, Australia Region

Preliminary Observations of Cloud and Precipitation Characteristics in the Brisbane, Australia Region Preliminary Observations of Cloud and Precipitation Characteristics in the Brisbane, Australia Region Sarah Tessendorf April 23, 2008 R. Bruintjes,, J. Wilson, R. Roberts, E. Brandes,, P. May, J. Peter,

More information

Potential impacts of aerosol and dust pollution acting as cloud nucleating aerosol on water resources in the Colorado River Basin

Potential impacts of aerosol and dust pollution acting as cloud nucleating aerosol on water resources in the Colorado River Basin Potential impacts of aerosol and dust pollution acting as cloud nucleating aerosol on water resources in the Colorado River Basin Vandana Jha, W. R. Cotton, and G. G. Carrio Colorado State University,

More information

3. The map below shows an eastern portion of North America. Points A and B represent locations on the eastern shoreline.

3. The map below shows an eastern portion of North America. Points A and B represent locations on the eastern shoreline. 1. Most tornadoes in the Northern Hemisphere are best described as violently rotating columns of air surrounded by A) clockwise surface winds moving toward the columns B) clockwise surface winds moving

More information

Introduction. Effect of aerosols on precipitation: - challenging problem - no agreement between the results (quantitative and qualitative)

Introduction. Effect of aerosols on precipitation: - challenging problem - no agreement between the results (quantitative and qualitative) Introduction Atmospheric aerosols affect the cloud mycrophysical structure & formation (observations, numerical studies) An increase of the aerosol particles: - increases CCN concentrations - decreases

More information

DANO, Burkina Faso. Instruments Data set Status Highlights. Norbert Kalthoff and Juliane Schwendike. Institut für Meteorologie und Klimaforschung

DANO, Burkina Faso. Instruments Data set Status Highlights. Norbert Kalthoff and Juliane Schwendike. Institut für Meteorologie und Klimaforschung DANO, Burkina Faso Instruments Data set Status Highlights by Norbert Kalthoff and Juliane Schwendike Dano (super-)site in Burkina Faso Dreyer Foundation Dano Dano Bontioli Measurements at Bontioli site

More information

Background and History

Background and History p1 Background and History What is the Indian Ocean Climate Initiative? The Indian Ocean Climate Initiative (IOCI) is a strategic program of research and information transfer to support government decision-making.

More information

AEROSOL-CLOUD INTERACTIONS AND PRECIPITATION IN A GLOBAL SCALE. SAHEL Conference April 2007 CILSS Ouagadougou, Burkina Faso

AEROSOL-CLOUD INTERACTIONS AND PRECIPITATION IN A GLOBAL SCALE. SAHEL Conference April 2007 CILSS Ouagadougou, Burkina Faso AEROSOL-CLOUD INTERACTIONS AND PRECIPITATION IN A GLOBAL SCALE SAHEL Conference 2007 2-6 April 2007 CILSS Ouagadougou, Burkina Faso The aerosol/precipitation connection Aerosol environment has changed

More information

Long-term Trends and Spatio-temporal Variations in Atmospheric Aerosols at UFS (TP I/02)

Long-term Trends and Spatio-temporal Variations in Atmospheric Aerosols at UFS (TP I/02) Long-term Trends and Spatio-temporal Variations in Atmospheric Aerosols at UFS (TP I/02) Jia Sun 1, Markus Hermann 1, Ludiwg Ries 2, Wolfram Birmili 2 and Alfred Wiedensohler 1 1 Leibniz Institute for

More information

The Climatology of Clouds using surface observations. S.G. Warren and C.J. Hahn Encyclopedia of Atmospheric Sciences.

The Climatology of Clouds using surface observations. S.G. Warren and C.J. Hahn Encyclopedia of Atmospheric Sciences. The Climatology of Clouds using surface observations S.G. Warren and C.J. Hahn Encyclopedia of Atmospheric Sciences Gill-Ran Jeong Cloud Climatology The time-averaged geographical distribution of cloud

More information

Climate and the Atmosphere

Climate and the Atmosphere Climate and Biomes Climate Objectives: Understand how weather is affected by: 1. Variations in the amount of incoming solar radiation 2. The earth s annual path around the sun 3. The earth s daily rotation

More information

Land Surface Sea Ice Land Ice. (from Our Changing Planet)

Land Surface Sea Ice Land Ice. (from Our Changing Planet) Lecture 5: Land Surface and Cryosphere (Outline) Land Surface Sea Ice Land Ice (from Our Changing Planet) Earth s s Climate System Solar forcing Atmosphere Ocean Land Solid Earth Energy, Water, and Biochemistry

More information

Earth s Climate System. Surface Albedo. Climate Roles of Land Surface. Lecture 5: Land Surface and Cryosphere (Outline) Land Surface Sea Ice Land Ice

Earth s Climate System. Surface Albedo. Climate Roles of Land Surface. Lecture 5: Land Surface and Cryosphere (Outline) Land Surface Sea Ice Land Ice Lecture 5: Land Surface and Cryosphere (Outline) Earth s Climate System Solar forcing Land Surface Sea Ice Land Ice Atmosphere Ocean Land Solid Earth Energy, Water, and Biochemistry Cycles (from Our Changing

More information

Final Exam: Monday March 17 3:00-6:00 pm (here in Center 113) Slides from Review Sessions are posted on course website:

Final Exam: Monday March 17 3:00-6:00 pm (here in Center 113) Slides from Review Sessions are posted on course website: Final Exam: Monday March 17 3:00-6:00 pm (here in Center 113) 35% of total grade Format will be all multiple choice (~70 questions) Final exam will cover entire course - material since 2 nd midterm weighted

More information

Mountain Snowpacks, Climate Change and the Silver Solution

Mountain Snowpacks, Climate Change and the Silver Solution Mountain Snowpacks, Climate Change and the Silver Solution Climate Change Seminar Series University of Nevada Las Vegas 11 July 2012 Arlen Huggins Desert Research Institute Reno, Nevada Climate, snow and

More information

ENTRAINMENT-MIXING IN SHALLOW CUMULUS AND THE ONSET OF PRECIPITATION

ENTRAINMENT-MIXING IN SHALLOW CUMULUS AND THE ONSET OF PRECIPITATION ENTRAINMENT-MIXING IN SHALLOW CUMULUS AND THE ONSET OF PRECIPITATION Frédéric Burnet & Jean-Louis Brenguier Météo-France CNRM-GAME Experimental and Instrumental Research Group Objectives What are the controling

More information

Assimilation of satellite derived soil moisture for weather forecasting

Assimilation of satellite derived soil moisture for weather forecasting Assimilation of satellite derived soil moisture for weather forecasting www.cawcr.gov.au Imtiaz Dharssi and Peter Steinle February 2011 SMOS/SMAP workshop, Monash University Summary In preparation of the

More information

Day Microphysics RGB Nephanalysis in daytime. Meteorological Satellite Center, JMA

Day Microphysics RGB Nephanalysis in daytime. Meteorological Satellite Center, JMA Day Microphysics RGB Nephanalysis in daytime Meteorological Satellite Center, JMA What s Day Microphysics RGB? R : B04 (N1 0.86) Range : 0~100 [%] Gamma : 1.0 G : B07(I4 3.9) (Solar component) Range :

More information

Climate also has a large influence on how local ecosystems have evolved and how we interact with them.

Climate also has a large influence on how local ecosystems have evolved and how we interact with them. The Mississippi River in a Changing Climate By Paul Lehman, P.Eng., General Manager Mississippi Valley Conservation (This article originally appeared in the Mississippi Lakes Association s 212 Mississippi

More information

Light Up Your World Adapted from Reflecting on Reflectivity,

Light Up Your World Adapted from Reflecting on Reflectivity, Climate Change I m Supposed To Know What That Is? Light Up Your World Adapted from Reflecting on Reflectivity, http://www.climatechangenorth.ca Overview: Students often confuse global warming and the depletion

More information

Direct radiative forcing due to aerosols in Asia during March 2002

Direct radiative forcing due to aerosols in Asia during March 2002 Direct radiative forcing due to aerosols in Asia during March 2002 Soon-Ung Park, Jae-In Jeong* Center for Atmospheric and Environmental Modeling *School of Earth and Environmental Sciences, Seoul National

More information

High resolution rainfall projections for the Greater Sydney Region

High resolution rainfall projections for the Greater Sydney Region 20th International Congress on Modelling and Simulation, Adelaide, Australia, 1 6 December 2013 www.mssanz.org.au/modsim2013 High resolution rainfall projections for the Greater Sydney Region F. Ji a,

More information

Fully coupled aerosol-radiationinteraction

Fully coupled aerosol-radiationinteraction Forschungszentrum Karlsruhe in der Helmholtz-Gemeinschaft Fully coupled aerosol-radiationinteraction with LM-ART D. Bäumer, B. Vogel, H. Vogel, T. Stanelle, R. Rinke, M. Bangert, Ch. Kottmeier Langen,

More information

Aerosol Effects on Water and Ice Clouds

Aerosol Effects on Water and Ice Clouds Aerosol Effects on Water and Ice Clouds Ulrike Lohmann Department of Physics and Atmospheric Science, Dalhousie University, Halifax, N. S., Canada Contributions from Johann Feichter, Johannes Hendricks,

More information

Lecture Ch. 6. Condensed (Liquid) Water. Cloud in a Jar Demonstration. How does saturation occur? Saturation of Moist Air. Saturation of Moist Air

Lecture Ch. 6. Condensed (Liquid) Water. Cloud in a Jar Demonstration. How does saturation occur? Saturation of Moist Air. Saturation of Moist Air Lecture Ch. 6 Saturation of moist air Relationship between humidity and dewpoint Clausius-Clapeyron equation Dewpoint Temperature Depression Isobaric cooling Moist adiabatic ascent of air Equivalent temperature

More information

Aerosols AP sizes AP types Sources Sinks Amount and lifetime Aerosol radiative effects. Aerosols. Trude Storelvmo Aerosols 1 / 21

Aerosols AP sizes AP types Sources Sinks Amount and lifetime Aerosol radiative effects. Aerosols. Trude Storelvmo Aerosols 1 / 21 Aerosols Trude Storelvmo Aerosols 1 / 21 Aerosols: Definition Definition of an aerosol: disperse system with air as carrier gas and a solid or liquid or a mixture of both as disperse phases. Aerosol particles

More information

Projeto Temático FAPESP 2013/ Climate Ecosystems Atmospheric Composition

Projeto Temático FAPESP 2013/ Climate Ecosystems Atmospheric Composition Projeto Temático FAPESP 2013/05014-0 Climate Ecosystems Atmospheric Composition GoAmazon2014/15 Experiment Manaus is a city of 2 million people surrounded by just forest in a radius of 1.500 Km. UNIQUE

More information

LABORATORY EXPERIMENTS OF MIXED- PHASE CLOUD FORMATION

LABORATORY EXPERIMENTS OF MIXED- PHASE CLOUD FORMATION LABORATORY EXPERIMENTS OF MIXED- PHASE CLOUD FORMATION Takuya Tajiri 1*, Katsuya Yamashita 1, Masataka Murakami 1, Narihiro Orikasa 1, Atsushi Saito 1, Tomohiro Nagai 1, Tetsu Sakai 1, and Hiroshi Ishimoto

More information

Welcome to ATMS 111 Global Warming.

Welcome to ATMS 111 Global Warming. Welcome to ATMS 111 Global Warming http://www.atmos.washington.edu/2010q1/111 http://cgz.e2bn.net/e2bn/leas/c99/schools/cgz/accounts/staff/rchambers/geobytes/gcse/case%20studies/causes_of_flooding_in_bangladesh.jpg

More information

Satellite measurements of CCN and cloud properties at the cloudy boundary layer: The Holy Grail is it achievable?

Satellite measurements of CCN and cloud properties at the cloudy boundary layer: The Holy Grail is it achievable? Satellite measurements of CCN and cloud properties at the cloudy boundary layer: The Holy Grail is it achievable? C 1 Daniel Rosenfeld, The Hebrew University of Jerusalem E -85 D C -89-93 E -85 D C -93-89

More information

Thermal / Solar. When air is warmed it... Rises. Solar Energy. Evaporation. Condensation Forms Clouds

Thermal / Solar. When air is warmed it... Rises. Solar Energy. Evaporation. Condensation Forms Clouds Thermal / Solar Light from the Sun is transformed into what type of energy when it hits Earth's surface? Rises When air is warmed it... Solar Energy Water moves through the water cycle using what type

More information

Exam 2: Cloud Physics April 16, 2008 Physical Meteorology Questions 1-10 are worth 5 points each. Questions are worth 10 points each.

Exam 2: Cloud Physics April 16, 2008 Physical Meteorology Questions 1-10 are worth 5 points each. Questions are worth 10 points each. Exam : Cloud Physics April, 8 Physical Meteorology 344 Name Questions - are worth 5 points each. Questions -5 are worth points each.. Rank the concentrations of the following from lowest () to highest

More information

p = ρrt p = ρr d = T( q v ) dp dz = ρg

p = ρrt p = ρr d = T( q v ) dp dz = ρg Chapter 1: Properties of the Atmosphere What are the major chemical components of the atmosphere? Atmospheric Layers and their major characteristics: Troposphere, Stratosphere Mesosphere, Thermosphere

More information

Weather Notes. Chapter 16, 17, & 18

Weather Notes. Chapter 16, 17, & 18 Weather Notes Chapter 16, 17, & 18 Weather Weather is the condition of the Earth s atmosphere at a particular place and time Weather It is the movement of energy through the atmosphere Energy comes from

More information

Can dust cause droughts?

Can dust cause droughts? Can dust cause droughts? Dust and sea surface temperature forcing of the 1930 s Dust bowl Cook et al., GRL 2008 Impact of desert dust radiative forcing on Sahel precipitation: Radiative Importance of dust

More information

Modelling aerosol-cloud interations in GCMs

Modelling aerosol-cloud interations in GCMs Modelling aerosol-cloud interations in GCMs Ulrike Lohmann ETH Zurich Institute for Atmospheric and Climate Science Reading, 13.11.2006 Acknowledgements: Sylvaine Ferrachat, Corinna Hoose, Erich Roeckner,

More information

Weather is the of the Earth s atmosphere at a place and time. It is the movement of through the atmosphere o Energy comes from the

Weather is the of the Earth s atmosphere at a place and time. It is the movement of through the atmosphere o Energy comes from the Weather Notes Weather Weather is the of the Earth s atmosphere at a place and time It is the movement of through the atmosphere o Energy comes from the The sun is the force that weather The sun s energy

More information

Week: Dates: 3/2 3/20 Unit: Climate

Week: Dates: 3/2 3/20 Unit: Climate clementaged.weebly.com Name: EVEN Period: Week: 28 30 Dates: 3/2 3/20 Unit: Climate Monday Tuesday Wednesday Thursday Friday 2 O 3 E *Vocabulary *Water in the Atmosphere and Clouds Notes *Cloud Drawings

More information

MICROPHYSICAL AND PRECIPITATION FORMATION PROCESSES AND RADAR SIGNATURES

MICROPHYSICAL AND PRECIPITATION FORMATION PROCESSES AND RADAR SIGNATURES MICROPHYSICAL AND PRECIPITATION FORMATION PROCESSES AND RADAR SIGNATURES 4 TH International Workshop on Weather Modification 3 rd Workshop on Cloud Physics 21-22 October 2010 Daegu, Korea Projects Current

More information

Name Date Class. well as the inland, found near the Tropics. 4. In the, or the regions near the Equator, you may find a lush

Name Date Class. well as the inland, found near the Tropics. 4. In the, or the regions near the Equator, you may find a lush WATER, CLIMATE, AND VEGETATION Vocabulary Activity DIRECTIONS: Fill in the Blanks Select a term from below to complete each of the following sentences. CHAPTER 1. The constant movement of water, a process

More information

YMC FOR CLIMATE CHANGE AND AIR QUALITY (CCAQ) CENTER of BMKG

YMC FOR CLIMATE CHANGE AND AIR QUALITY (CCAQ) CENTER of BMKG Contribution of CENTER for CLIMATE CHANGE and AIR QUALITY (CCAQ) OF BMKG in the Prepared by Dr. Dodo Gunawan Director FIRST INTERNATIONAL SCIENCE AND PLANNING WORKSHOP ON YMC, SINGAPORE 27-30 JANUARY 2015

More information

The Sensitivity of Global Nucleation, CCN and Climate to SO2 and Criegee-Intermediate Chemistry

The Sensitivity of Global Nucleation, CCN and Climate to SO2 and Criegee-Intermediate Chemistry The Sensitivity of Global Nucleation, CCN and Climate to SO2 and Criegee-Intermediate Chemistry Jeff Pierce, Mat Evans, Cat Scott, Steve D'Andrea, Delphine Farmer, Erik Swietlicki and Dom Spracklen Pierce,

More information

GEOGRAPHY EYA NOTES. Weather. atmosphere. Weather and climate

GEOGRAPHY EYA NOTES. Weather. atmosphere. Weather and climate GEOGRAPHY EYA NOTES Weather and climate Weather The condition of the atmosphere at a specific place over a relatively short period of time Climate The atmospheric conditions of a specific place over a

More information

Studying 2006 dry and 2007 wet events using surface observations and NCEP Reanalysis

Studying 2006 dry and 2007 wet events using surface observations and NCEP Reanalysis Studying 2006 dry and 2007 wet events using surface observations and NCEP Reanalysis Xiquan Dong, Baike Xi, and Aaron Kennedy University of North Dakota 1 Objectives 1. How do seasonal cycles of observed

More information

Meteorology. Chapter 15 Worksheet 1

Meteorology. Chapter 15 Worksheet 1 Chapter 15 Worksheet 1 Meteorology Name: Circle the letter that corresponds to the correct answer 1) The Tropic of Cancer and the Arctic Circle are examples of locations determined by: a) measuring systems.

More information

Working Group Initiation of Convection

Working Group Initiation of Convection Working Group Initiation of Convection Ulrich Corsmeier Institut für Meteorologie und Klimaforschung (IMK) Forschungszentrum Karlsruhe/Universität Karlsruhe 2 nd COPS Workshop June 27 June 28, 2005 University

More information

Confidence levels and error bars for continuous detection of mixing layer heights by ceilometer

Confidence levels and error bars for continuous detection of mixing layer heights by ceilometer Confidence levels and error bars for continuous detection of mixing layer heights by ceilometer Christoph Münkel, Vaisala GmbH, Hamburg, Germany Klaus Schäfer, KIT IMK-IFU, Garmisch-Partenkirchen, Germany

More information

2018 Science Olympiad: Badger Invitational Meteorology Exam. Team Name: Team Motto:

2018 Science Olympiad: Badger Invitational Meteorology Exam. Team Name: Team Motto: 2018 Science Olympiad: Badger Invitational Meteorology Exam Team Name: Team Motto: This exam has 50 questions of various formats, plus 3 tie-breakers. Good luck! 1. On a globally-averaged basis, which

More information

TROPICAL-EXTRATROPICAL INTERACTIONS

TROPICAL-EXTRATROPICAL INTERACTIONS Notes of the tutorial lectures for the Natural Sciences part by Alice Grimm Fourth lecture TROPICAL-EXTRATROPICAL INTERACTIONS Anomalous tropical SST Anomalous convection Anomalous latent heat source Anomalous

More information

Page 1. Name:

Page 1. Name: Name: 1) As the difference between the dewpoint temperature and the air temperature decreases, the probability of precipitation increases remains the same decreases 2) Which statement best explains why

More information

INVESTIGATION FOR A POSSIBLE INFLUENCE OF IOANNINA AND METSOVO LAKES (EPIRUS, NW GREECE), ON PRECIPITATION, DURING THE WARM PERIOD OF THE YEAR

INVESTIGATION FOR A POSSIBLE INFLUENCE OF IOANNINA AND METSOVO LAKES (EPIRUS, NW GREECE), ON PRECIPITATION, DURING THE WARM PERIOD OF THE YEAR Proceedings of the 13 th International Conference of Environmental Science and Technology Athens, Greece, 5-7 September 2013 INVESTIGATION FOR A POSSIBLE INFLUENCE OF IOANNINA AND METSOVO LAKES (EPIRUS,

More information

1. Base your answer to the following question on the weather map below, which shows a weather system that is affecting part of the United States.

1. Base your answer to the following question on the weather map below, which shows a weather system that is affecting part of the United States. 1. Base your answer to the following question on the weather map below, which shows a weather system that is affecting part of the United States. Which sequence of events forms the clouds associated with

More information

Addressing Diurnal Temperature Biases in the WRF Model

Addressing Diurnal Temperature Biases in the WRF Model Addressing Diurnal Temperature Biases in the WRF Model Jeffrey Massey University of Utah Collaborators: Jim Steenburgh, Jason Knievel, Sebastian Hoch, Josh Hacker Long term 2-m temperature verification

More information

Water Balance in the Murray-Darling Basin and the recent drought as modelled with WRF

Water Balance in the Murray-Darling Basin and the recent drought as modelled with WRF 18 th World IMACS / MODSIM Congress, Cairns, Australia 13-17 July 2009 http://mssanz.org.au/modsim09 Water Balance in the Murray-Darling Basin and the recent drought as modelled with WRF Evans, J.P. Climate

More information

Impacts of aerosols in the CORDEX-Europe domain using the regional aerosol-climate model REMO-HAM

Impacts of aerosols in the CORDEX-Europe domain using the regional aerosol-climate model REMO-HAM Impacts of aerosols in the CORDEX-Europe domain using the regional aerosol-climate model REMO-HAM Armelle Reca C. Remedio (1), Claas Teichmann (1,2), Joni-Pekka Pietikäinen (3), Natalia Sudarchikova (1),

More information

Impacts of Climate on the Corn Belt

Impacts of Climate on the Corn Belt Impacts of Climate on the Corn Belt Great Lakes Crop Summit 2015 2015 Evelyn Browning Garriss Conclusions Climate change is not linear. It ebbs and flows. Recent polar volcano eruptions created a cool

More information

Convection-Resolving Model Simulations: Process-Based Comparison of LM Results with Observations

Convection-Resolving Model Simulations: Process-Based Comparison of LM Results with Observations Convection-Resolving Model Simulations: Process-Based Comparison of LM Results with Observations Jörg Trentmann, Britta Wecker, Marcus Paulat, Heini Wernli, Ulrich Corsmeier, Jan Handwerker Goal Improve

More information

Remote sensing of meteorological conditions at airports for air quality issues

Remote sensing of meteorological conditions at airports for air quality issues Remote sensing of meteorological conditions at airports for air quality issues Stefan Emeis, Klaus Schäfer Institute for Meteorology and Climate Research Atmospheric Environmental Research (IMK-IFU) Forschungszentrum

More information

Airborne observations of the effect of a cold front on the aerosol particle size distribution and new particle formation

Airborne observations of the effect of a cold front on the aerosol particle size distribution and new particle formation Quarterly Journal of the Royal Meteorological Society Q. J. R. Meteorol. Soc. 136: 944 961, April 21 Part B Airborne observations of the effect of a cold front on the aerosol particle size distribution

More information

Factors That Affect Climate

Factors That Affect Climate Factors That Affect Climate Factors That Affect Climate Latitude As latitude (horizontal lines) increases, the intensity of solar energy decreases. The tropical zone is between the tropic of Cancer and

More information

IARA - GoAmazon 2014

IARA - GoAmazon 2014 IARA - GoAmazon 2014 Activities related to Aerosol, Cloud, Precipitation, and Radiation Interactions and Dynamics of Convective Cloud Systems (ACRIDICON) and CHUVA Project Luiz.Machado@cptec.inpe.br CHUVA

More information

Wind and turbulence structure in the boundary layer around an isolated mountain: airborne measurements during the MATERHORN field study

Wind and turbulence structure in the boundary layer around an isolated mountain: airborne measurements during the MATERHORN field study Wind and turbulence structure in the boundary layer around an isolated mountain: airborne measurements during the MATERHORN field study Stephan F.J. De Wekker 1, G.D. Emmitt 2, S. Greco 2, K. Godwin 2,

More information

Tropical Montane Cloud Forests: Importance and Challenges in a Changing Environment

Tropical Montane Cloud Forests: Importance and Challenges in a Changing Environment Tropical Montane Cloud Forests: Importance and Challenges in a Changing Environment Daniel E. Comarazamy and Jorge E. González The NOAA-CREST Center & Department of Mechanical Engineering, City College

More information

Code Proposed Standards Code Current Standards ESS1A The Universe and Its Stars Describe the presence of the Sun, Moon, and stars in the sky over time

Code Proposed Standards Code Current Standards ESS1A The Universe and Its Stars Describe the presence of the Sun, Moon, and stars in the sky over time Kindergarten Earth Science Code Proposed Standards Code Current Standards ESS1A The Universe and Its Stars Describe the presence of the Sun, Moon, and stars in the sky over time 6.1.A.K.a. Observe and

More information

LESSON 2. Speeding in Space. Literacy Article 2A. Name. Date

LESSON 2. Speeding in Space. Literacy Article 2A. Name. Date Literacy Article 2A Name Date LESSON 2 Speeding in Space The solar system is composed of many things. It includes our star, the Sun, the planets and their moons, comets, and asteroids. All of these objects

More information

School Name Team # International Academy East Meteorology Test Graphs, Pictures, and Diagrams Diagram #1

School Name Team # International Academy East Meteorology Test Graphs, Pictures, and Diagrams Diagram #1 School Name Team # International Academy East Meteorology Test Graphs, Pictures, and Diagrams Diagram #1 Use the map above, and the locations marked A-F, to answer the following questions. 1. The center

More information

Name the surface winds that blow between 0 and 30. GEO 101, February 25, 2014 Monsoon Global circulation aloft El Niño Atmospheric water

Name the surface winds that blow between 0 and 30. GEO 101, February 25, 2014 Monsoon Global circulation aloft El Niño Atmospheric water GEO 101, February 25, 2014 Monsoon Global circulation aloft El Niño Atmospheric water Name the surface winds that blow between 0 and 30 What is the atmospheric pressure at 0? What is the atmospheric pressure

More information

Polar Weather Prediction

Polar Weather Prediction Polar Weather Prediction David H. Bromwich Session V YOPP Modelling Component Tuesday 14 July 2015 A special thanks to the following contributors: Kevin W. Manning, Jordan G. Powers, Keith M. Hines, Dan

More information

ERAD Enhancement of precipitation by liquid carbon dioxide seeding. Proceedings of ERAD (2002): c Copernicus GmbH 2002

ERAD Enhancement of precipitation by liquid carbon dioxide seeding. Proceedings of ERAD (2002): c Copernicus GmbH 2002 Proceedings of ERAD (2002): 150 154 c Copernicus GmbH 2002 ERAD 2002 Enhancement of precipitation by liquid carbon dioxide seeding K. Nishiyama 1, K. Wakimizu 2, Y. Suzuki 2, H. Yoshikoshi 2, and N. Fukuta

More information

Development of an ensemble-based volcanic ash dispersion model for operations at Darwin VAAC

Development of an ensemble-based volcanic ash dispersion model for operations at Darwin VAAC Development of an ensemble-based volcanic ash dispersion model for operations at Darwin VAAC Rodney Potts Bureau of Meteorology Australia [C Lucas, R Dare, M Manickam, A Wain, M Zidikheri, A Bear-Crozier]

More information

Real case simulations using spectral bin cloud microphysics: Remarks on precedence research and future activity

Real case simulations using spectral bin cloud microphysics: Remarks on precedence research and future activity Real case simulations using spectral bin cloud microphysics: Remarks on precedence research and future activity Takamichi Iguchi 1,2 (takamichi.iguchi@nasa.gov) 1 Earth System Science Interdisciplinary

More information

ESCI 344 Tropical Meteorology Lesson 7 Temperature, Clouds, and Rain

ESCI 344 Tropical Meteorology Lesson 7 Temperature, Clouds, and Rain ESCI 344 Tropical Meteorology Lesson 7 Temperature, Clouds, and Rain References: Forecaster s Guide to Tropical Meteorology (updated), Ramage Tropical Climatology, McGregor and Nieuwolt Climate and Weather

More information

The role of dust on cloud-precipitation cycle

The role of dust on cloud-precipitation cycle UNIVERSITY OF ATHENS SCHOOL OF PHYSICS, DIVISION OF ENVIRONMENT AND METEOROLOGY ATMOSPHERIC MODELING AND WEATHER FORECASTING GROUP The role of dust on cloud-precipitation cycle Stavros Solomos, George

More information

The reviewer s comments are presented in italics, followed by our responses. We thank the reviewer for his comments.

The reviewer s comments are presented in italics, followed by our responses. We thank the reviewer for his comments. Anonymous Referee #1 The reviewer s comments are presented in italics, followed by our responses. We thank the reviewer for his comments. The authors describe cloud microphysical measurements made at Storm

More information

1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures?

1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures? CHAPTER 17 1 What Is Climate? SECTION Climate BEFORE YOU READ After you read this section, you should be able to answer these questions: What is climate? What factors affect climate? How do climates differ

More information

ATMOSPHERIC CIRCULATION AND WIND

ATMOSPHERIC CIRCULATION AND WIND ATMOSPHERIC CIRCULATION AND WIND The source of water for precipitation is the moisture laden air masses that circulate through the atmosphere. Atmospheric circulation is affected by the location on the

More information

NATIONAL HYDROPOWER ASSOCIATION MEETING. December 3, 2008 Birmingham Alabama. Roger McNeil Service Hydrologist NWS Birmingham Alabama

NATIONAL HYDROPOWER ASSOCIATION MEETING. December 3, 2008 Birmingham Alabama. Roger McNeil Service Hydrologist NWS Birmingham Alabama NATIONAL HYDROPOWER ASSOCIATION MEETING December 3, 2008 Birmingham Alabama Roger McNeil Service Hydrologist NWS Birmingham Alabama There are three commonly described types of Drought: Meteorological drought

More information

Weather. Describing Weather

Weather. Describing Weather CHAPTER 13 Weather LESSON 1 Describing Weather What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column if you agree with the

More information

Chapter 2 Planet Earth

Chapter 2 Planet Earth Chapter 2 Planet Earth Section Notes Earth and the Sun s Energy Water on Earth The Land Close-up The Water Cycle World Almanac Major Eruptions in the Ring of Fire Quick Facts Chapter 2 Visual Summary Video

More information

The PRECIS Regional Climate Model

The PRECIS Regional Climate Model The PRECIS Regional Climate Model General overview (1) The regional climate model (RCM) within PRECIS is a model of the atmosphere and land surface, of limited area and high resolution and locatable over

More information

Weather. Describing Weather

Weather. Describing Weather Weather Describing Weather What is weather? Weather is the atmospheric conditions, along with short-term changes, of a certain place at a certain time. Have you ever been caught in a rainstorm on what

More information

The Atmospheric Chemistry and Physics of Ammonia

The Atmospheric Chemistry and Physics of Ammonia The Atmospheric Chemistry and Physics of Ammonia Russell Dickerson Dept. Meteorology, The University of Maryland Presented at the National Atmospheric Deposition Program Ammonia Workshop October 23, 2003

More information

InSAR atmospheric effects over volcanoes - atmospheric modelling and persistent scatterer techniques

InSAR atmospheric effects over volcanoes - atmospheric modelling and persistent scatterer techniques InSAR atmospheric effects over volcanoes - atmospheric modelling and persistent scatterer techniques Rachel Holley 1,2, Geoff Wadge 1, Min Zhu 1, Ian James 3, Peter Clark 4 Changgui Wang 4 1. Environmental

More information

The Role of the Land Surface in Fog Modelling Simulations with COSMO-FOG

The Role of the Land Surface in Fog Modelling Simulations with COSMO-FOG COSMO-USER SEMINAR Langen, 2009 The Role of the Land Surface in Fog Modelling Simulations with COSMO-FOG Isabel Alberts, Matthieu Masbou and Andreas Bott Meteorological Institute University of Bonn, ialberts@uni-bonn.de

More information

P1.34 MULTISEASONALVALIDATION OF GOES-BASED INSOLATION ESTIMATES. Jason A. Otkin*, Martha C. Anderson*, and John R. Mecikalski #

P1.34 MULTISEASONALVALIDATION OF GOES-BASED INSOLATION ESTIMATES. Jason A. Otkin*, Martha C. Anderson*, and John R. Mecikalski # P1.34 MULTISEASONALVALIDATION OF GOES-BASED INSOLATION ESTIMATES Jason A. Otkin*, Martha C. Anderson*, and John R. Mecikalski # *Cooperative Institute for Meteorological Satellite Studies, University of

More information

Arizona Cloud Seeding Efforts: A Salt River Project Perspective. James Walter SRP Surface Water Resources CPWAC/CPWP Joint Meeting March 30, 2018

Arizona Cloud Seeding Efforts: A Salt River Project Perspective. James Walter SRP Surface Water Resources CPWAC/CPWP Joint Meeting March 30, 2018 Arizona Cloud Seeding Efforts: A Salt River Project Perspective James Walter SRP Surface Water Resources Importance of Winter Precipitation Winter Cloud Seeding 101 Early Cloud Seeding Projects Questions

More information

Climate Classification

Climate Classification Chapter 15: World Climates The Atmosphere: An Introduction to Meteorology, 12 th Lutgens Tarbuck Lectures by: Heather Gallacher, Cleveland State University Climate Classification Köppen classification:

More information

Arizona Drought Monitoring Sensitivity and Verification Analyses Project Results and Future Directions

Arizona Drought Monitoring Sensitivity and Verification Analyses Project Results and Future Directions Arizona Drought Monitoring Sensitivity and Verification Analyses Project Results and Future Directions A Water Sustainability Institute, Technology and Research Initiative Fund Project Christopher L. Castro,

More information

Tropical Moist Rainforest

Tropical Moist Rainforest Tropical or Lowlatitude Climates: Controlled by equatorial tropical air masses Tropical Moist Rainforest Rainfall is heavy in all months - more than 250 cm. (100 in.). Common temperatures of 27 C (80 F)

More information

Climate outlook, longer term assessment and regional implications. What s Ahead for Agriculture: How to Keep One of Our Key Industries Sustainable

Climate outlook, longer term assessment and regional implications. What s Ahead for Agriculture: How to Keep One of Our Key Industries Sustainable Climate outlook, longer term assessment and regional implications What s Ahead for Agriculture: How to Keep One of Our Key Industries Sustainable Bureau of Meteorology presented by Dr Jeff Sabburg Business

More information

Collision and Coalescence 3/3/2010. ATS 351 Lab 7 Precipitation. Droplet Growth by Collision and Coalescence. March 7, 2006

Collision and Coalescence 3/3/2010. ATS 351 Lab 7 Precipitation. Droplet Growth by Collision and Coalescence. March 7, 2006 ATS 351 Lab 7 Precipitation March 7, 2006 Droplet Growth by Collision and Coalescence Growth by condensation alone takes too long ( 15 C -) Occurs in clouds with tops warmer than 5 F Greater the speed

More information

The hydrologic service area (HSA) for this office covers Central Kentucky and South Central Indiana.

The hydrologic service area (HSA) for this office covers Central Kentucky and South Central Indiana. January 2012 February 13, 2012 An X inside this box indicates that no flooding occurred within this hydrologic service area. January 2012 continued the string of wet months this winter. Rainfall was generally

More information

Impact of new particle formation on the concentrations of aerosols and cloud condensation nuclei around Beijing

Impact of new particle formation on the concentrations of aerosols and cloud condensation nuclei around Beijing ! JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116, D19208, doi:10.1029/2011jd016025, 2011!! Impact of new particle formation on the concentrations of aerosols and cloud condensation nuclei around Beijing H.

More information

Interdecadal variation in rainfall patterns in South West of Western Australia

Interdecadal variation in rainfall patterns in South West of Western Australia Interdecadal variation in rainfall patterns in South West of Western Australia Priya 1 and Bofu Yu 2 1 PhD Candidate, Australian Rivers Institute and School of Engineering, Griffith University, Brisbane,

More information