Spatial coverage and temporal trends of land-based atmospheric mercury measurements in the Northern and Southern Hemispheres
|
|
- Angelica Phelps
- 5 years ago
- Views:
Transcription
1 Institut für Küstenforschung Zur Anzeige wird der QuickTime Dekompressor TIFF (LZW) benötigt. Spatial coverage and temporal trends of land-based atmospheric mercury measurements in the Northern and Southern Hemispheres Ralf Ebinghaus, Cathy Banic, Steve Beauchamp, Dan Jaffe, Hans Herbert Kock, Nicola Pirrone, Laurier Poissant, Francesca Sprovieri and Peter Weiss-Penzias
2 Past trends Chemical analysis of lake sediments, ice cores and peat deposits from both hemispheres indicates about a threefold increase of mercury deposition since pre-industrial times
3 Monitoring of more recent change Asian mercury emissions are suggested to be rapidly increasing at least in the past decade (Pacyna et al., 2006). In principal, an increase of the global atmospheric pool should also be reflected in the background concentration in ambient air. Regional differences, temporal trends and potential sources and source regions can be identified by monitoring networks.
4 Monitoring networks on regional scales - ambient air EUROPE
5 MEDITERRANEAN ATMOSPHERIC MERCURY CYCLE SYSTEM (MAMCS) and Mercury Species over Europe (MOE) 1. Mallorca ( N, E); 2. Calabria (39 25 N, E); 3. Sicily (36 40 N, 15 l0 E); 4. Turkey ( N, E); 5. Israel (32 40 N, E); 6. Germany ( N, ); 7. Germany ( N, E); 8. Sweden ( N, ll E); 9. Sweden ( , E); 10. Ireland (53 20 N, 9 54 W)
6 RGM (pg m -3 ) TPM (pg m -3 ) TGM (ng m -3 ) MAMCS / MOE field campaigns TGM MOE MAMCS CAMPAIGNS START DATE STOP DATE MAMCS-1/ MOE-1 MAMCS-2 / MOE-2 MAMCS-3 / MOE-3 MAMCS-4 / MOE TPM MOE MAMCS MOE RGM MOE MAMCS
7 Results of MAMCS / MOE field campaigns Observed concentrations of total gaseous mercury (TGM), particulate mercury (TPM), and reactive gaseous mercury (RGM) were generally slightly higher in the Mediterranean region than in Northwest Europe (Wangberg et al. (2001)
8 Possible explanations for northsouth gradient More geologic sources of Hg 0 in Mediterranean region Enhanced reemission fluxes from warm sea surface More photochemical transformations in Mediterranean MBL
9 Monitoring networks on regional scales - ambient air U.S.A
10 Sites in the U.S. where gaseous Hg species have been measured
11 Spatial characteristics of atmospheric Hg in U.S. Sites near point sources (urban areas and mines (< 50 km) Sites influenced by regional point sources (< 500 km) Background sites High altitude site (3 km) Hg 0 Range of Means (ng/m3) RGM Mean - Max (pg/m3) Hgp Mean - Max (pg/m3) Precip. [Hg T ] Mean - Max (ng/l) NA
12 Monitoring networks on regional scales - ambient air CANADA
13 In 1995 Fitzgerald has plead for and defined the basic requirements of an Atmospheric Mercury Network (AMNET). This has partly been accomplished on a regional scale within the Canadian Atmospheric Mercury Network (CAMNet) that may be considered as seminal in this respect
14 CAMNet Alert CAMNet active other CAMNet closed Little Fox Lake Fort Chipewyan Whistler Bratts Lake Reifel Island Esther Kuujjuarapik Mingan ELA St. Anicet Burnt Island Egbert Pt. Petre South Hampton Kejimkujik St. Andrews Station Code Province Latitude (deg) Longitude (deg) Altitude (meter a.s.l.) Period Alert ALT NU /95-12/05 Kejimkujik KEJ NS /96-12/04 St. Andrews STA NB /96-12/04 St. Anicet WBZ QC /97-12/05 Point Petre PPT ON /96-12/05 Egbert EGB ON /96-12/05 Burnt Island BNT ON /98-12/05 Bratt's Lake BRL SK /01-12/05 Esther EST AB /98-04/01 Fort Chipewyan FCH AB /00-07/01 Reifel Island RFL BC /99-02/04 a.s.l. = above sea level
15 11 CAMNet sites were analyzed for temporal trends ( ) (Temme et al., 2007) decreasing trend for TGM concentrations at several rural sites was seen for the time period 1995 to 2005 (- 2.2 to -16.6%) changes are mostly driven by local or regional changes in mercury emissions other sites reflect hemispherical global background concentrations of airborne mercury, where slight decreases or no statistically significant trend in TGM concentrations exist over the same time period
16 The current global Hg-background concentration General scientific consensus exists about the current global background concentration*: It is currently taken as ca. 1.5 to 1.7 ng m -3 in the Northern Hemisphere and ca. 1.1 to 1.3 ng m -3 in the Southern Hemisphere (Lindberg et al., 2007) *refers to the average sea-level atmospheric Hg(0) at remote sites
17 Long-term monitoring at single background locations The question of trends
18 GAW stations
19 Mercury GAW stations
20 GAW Station Mace Head, Ireland 53,2 o N, 9,5 o W
21 Aug/ 95 Jan/ 96 Jul/ 96 Jan/ 97 Jul/ 97 Jan/ 98 Jul/ 98 Jan/ 99 Jul/ 99 Jan/ 00 Jul/ 00 Jan/ 01 Jun/ 01 Dec/ 01 Jun/ 02 Dec/ 02 Jun/ 03 Dec/ 03 Jun/ 04 Dec/ 04 Jun/ 05 Dec/ 05 Jun/ 06 Dec/ 06 May/ 07 Nov/ 07 Long-term measurements at Mace Head, Irish west coast from today TGM (24 h av. ), Mace Head, Ireland, Since 2003 funded by: Since 2003 funded by:
22 GAW station Cape Point, RSA (34 o 21 S, 18 o 29 E) Cape of Good Hope GAW station
23 Long-term measurements at Cape Point, from Slemr et al. 2008, submitted to GRL, results based on manual methodology with low temporal resolution
24 More recent trends Asian mercury emissions are suggested to be rapidly increasing at least in the past decade however, this is neither reflected in the long-term measurement of TGM at Mace Head, Ireland or Cape Point - covering the period between 1995 to 2007, nor in the precipitation data of the North American Mercury Deposition Network ( MDN - not shown)
25 TGM [ng/m3] An attempt to reconstruct the past 30 years... Slemr et al., 2003 Ship Wank Rörvik Mace Head Lista Ny Alesund Alert Year Automated, highly time resolved measurements
26 Added value of long-term observational data with high time resolution - new insights in emissions and regional transport - unexpected findings -...
27 Emission estimates and source attribution Simultaneous Hg Observations at Mt. Bachelor and Okinawa (Jaffe et al., 2005) 2.7 km asl Okinawa MBO
28 Emission estimates and source attribution Elevated levels were associated with transport from E. Asia Since both Hg(0) and CO are long lived, this ratio should be preserved during long-range transport and be identical to source ratio. Since CO emissions from E. Asia have been quantified and validated, this can be used to estimate Hg(0) emissions from E.Asia. Jaffe et al., 2005; Weiss-Penzias et al., 2007
29 Example of Asian pollution plume detected at Mt. Bachelor Hg 0 / CO ng m -3 ppbv -1 This yields an estimate of 620 tons/yr for Chinese Hg 0 emission, which is 2x higher than estimate by Streets et al., 2005.
30 Unexpected findings...
31 AMDEs in Polar Regions
32 TGM concentrations at temperate and polar coasts Alert Data: Schroeder, Steffen and co-worker Mace Head Data: Ebinghaus, Kock and co-worker
33 TGM (ng Hg/m3) Hg-measurements with high time-resolution at Mace Head and Cape Point in 2007 TGM (ng Hg/m3), 1 h average, Cape Point, South Africa and Mace Head, Ireland, ,5 2,0 1,5 1,0 0,5 0,0 Date
34 Conclusions - monitoring data: - can identify regional differences, temporal trends and are useful scientific tools for source attribution reproducibility of regional changes cannot definitively answer Asian question. - are necessary to evaluate the effectiveness of control measures (on a regional basis) - can be used to verify / improve emission estimates - give new insights, for example based on unexpected observations - help us to understand the global mercury cycle in order to evolve purposeful regulations (on a global basis) The value of long-term atmospheric Hg monitoring stations and the need for additional sites is obvious,
Long range transport of mercury to the Arctic and across Canada
Atmos. Chem. Phys.,, 66 686, www.atmos-chem-phys.net//66// doi:.594/acp--66- Author(s). CC Attribution. License. Atmospheric Chemistry and Physics Long range transport of mercury to the Arctic and across
More informationGlobal Mercury Modeling at Environment Canada. Ashu Dastoor &Didier Davignon. Air Quality Research Division Environment Canada
Global Mercury Modeling at Environment Canada Ashu Dastoor &Didier Davignon Air Quality Research Division Environment Canada Atmospheric Mercury Cycling in Environment Canada s Mercury Model - GRAHM Transport
More informationOverview of Atmospheric Mercury. Mae Gustin and Jiaoyan Huang Department of Natural Resources and Environmental Science
Overview of Atmospheric Mercury Measurement Uncertainties Mae Gustin and Jiaoyan Huang Department of Natural Resources and Environmental Science Funding sources Acknowledgments U. S. National Science Foundation
More informationChemical Transport of Atmospheric Mercury over the Pacific
Chemical Transport of Atmospheric Mercury over the Pacific C. Jerry Lin 1, Li Pan 1, David G. Streets 2, Carey Jang 3, and Terry Keating 4 1 College of Engineering, Lamar University, Beaumont, TX 2 ANL
More informationEstimation of Speciated and Total Mercury Dry Deposition. Leiming Zhang. Pierrette Blanchard, David Gay, and many others
Estimation of Speciated and Total Mercury Dry Deposition Leiming Zhang Air Quality Research Division, Science and Technology Branch Environment Canada, Toronto. leiming.zhang@ec.gc.ca Contributors: Pierrette
More informationTransport of Hg from Atmospheric mercury depletion events to the mainland of Norway and its possible influence on Hg deposition
GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L09802, doi:10.1029/2008gl033586, 2008 Transport of Hg from Atmospheric mercury depletion events to the mainland of Norway and its possible influence on Hg deposition
More informationChemical sources and sinks of Hg(II) in the remote atmospheric marine boundary layer
Cruise May 22 Atlantic Cruise August 23 April 24 Chemical sources and sinks of Hg(II) in the remote atmospheric marine boundary layer Christopher D. Holmes Daniel J. Jacob Department of Earth & Planetary
More informationMae Gustin University of Nevada
Mae Gustin Mae Gustin University of Nevada General -atmospheric Hg and watersheds Atmospheric contribution i from mining i Sources Form Measuring deposition Effect of mining on deposition Local Nevada
More informationTime-Series Trends of Mercury Deposition Network Data
Time-Series Trends of Mercury Deposition Network Data Peter Weiss 1, David Gay 2, Mark Brigham 3, Matthew Parsons 4, Arnout Ter Schure 5 1 University of California, Santa Cruz, 2 National Atmospheric Deposition
More information5. Atmospheric Supply of Mercury to the Baltic Sea in 2015
Atmospheric Supply of Mercury to the Baltic Sea in 2015 69 5. Atmospheric Supply of Mercury to the Baltic Sea in 2015 In this chapter the results of model evaluation of mercury atmospheric input to the
More informationEstimation of speciated and total mercury dry deposition at monitoring
SUPPORTING INFORMATION Estimation of speciated and total mercury dry deposition at monitoring locations in eastern and central North America L. Zhang, P. Blanchard, D.A. Gay, E.M. Prestbo, M.R. Risch,
More informationAdvances in our Understanding of the Chemical Forms and Concentrations of GOM in the Atmosphere
Advances in our Understanding of the Chemical Forms and Concentrations of GOM in the Atmosphere Mae Sexauer Gustin Acknowledgements NSF EPRI Local scale air toxics grant from EPA through Nevada Division
More informationMOZAIC-IAGOS : Its role in the satellite validation and in assessing the ozone trends.
MOZAIC-IAGOS : Its role in the satellite validation and in assessing the ozone trends. MOZAIC Aug. 1994 Jun. 2009 http://mozaic.aero.obs-mip.fr 32 000 flights 230 000 Hours http://www.iagos.org V. Thouret,
More informationJesper H. Christensen NERI-ATMI, Frederiksborgvej Roskilde
Jesper H. Christensen NERI-ATMI, Frederiksborgvej 399 4000 Roskilde The model work is financially supported by the Danish Environmental Protection Agency with means from the MIKA/DANCEA funds for Environmental
More informationBaseline Ozone in Western North America: Measurements and Models. David Parrish
Baseline Ozone in Western North America: Measurements and Models David Parrish CIRES University of Colorado NOAA/ESRL Chemical Sciences Division Boulder, Colorado USA Consultant with David.D.Parrish, LLC
More informationAdvances in our Understanding of the Chemical Forms and Concentrations of GOM in the Atmosphere. Mae Sexauer Gustin
Advances in our Understanding of the Chemical Forms and Concentrations of GOM in the Atmosphere Mae Sexauer Gustin Acknowledgements NSF EPRI Local scale air toxics grant from EPA through Nevada Division
More information4.0 MODELING MERCURY EMISSIONS
26 4.0 MODELING MERCURY EMISSIONS Analysis of the impact of air pollutant emissions requires determination of the spatial distribution and magnitude of sources and sinks, and an understanding and quantifying
More informationSupplement of Monsoon-facilitated characteristics and transport of atmospheric mercury at a high-altitude background site in southwestern China
Supplement of Atmos. Chem. Phys., 16, 13131 13148, 2016 http://www.atmos-chem-phys.net/16/13131/2016/ doi:10.5194/acp-16-13131-2016-supplement Author(s) 2016. CC Attribution 3.0 License. Supplement of
More informationKinetic Studies of the Oxidation Pathways of Gaseous Elemental Mercury
University of Miami Scholarly Repository Open Access Dissertations Electronic Theses and Dissertations 2008-06-11 Kinetic Studies of the Oxidation Pathways of Gaseous Elemental Mercury Deanna L. Donohoue
More informationAntarctic Springtime Depletion of Atmospheric Mercury
Environ. Sci. Technol. 2002, 36, 1238-1244 Antarctic Springtime Depletion of Atmospheric Mercury RALF EBINGHAUS* AND HANS H. KOCK Institute for Coastal Research/Physical and Chemical Analysis, GKSS Research
More informationRecent Climate History - The Instrumental Era.
2002 Recent Climate History - The Instrumental Era. Figure 1. Reconstructed surface temperature record. Strong warming in the first and late part of the century. El Ninos and major volcanic eruptions are
More informationModeling the global atmospheric transport and deposition of mercury to the Great Lakes
Modeling the global atmospheric transport and deposition of mercury to the Great Lakes Mark D. Cohen 1, * Roland R. Draxler 1, Richard S. Artz 1 Pierrette Blanchard 2 Mae Sexauer Gustin 3 Young-Ji Han
More informationAndrew Lee BEng (Hons) CEng MIStructE FGS FPWS
Jim Twaddle BSc (Hons) FGS Andrew Lee BEng (Hons) CEng MIStructE FGS FPWS 22 January 2010 ME50231/RE001 !! "# # $ " %! &' ( "# # $ ) # ' %! "# # $ # "# # $ * + # "# # $ "! # "# # $, # "# # $! -( +.!!/
More informationDust storm variability over EGYPT By Fathy M ELashmawy Egyptian Meteorological Authority
WMO WORKSHOP ON CLIMATE MONITORING INCLUDING THE IMPLEMENTATION OF CLIMATE WATCH SYSTEMS FOR ARAB COUNTRIES IN WEST ASIA, AMMAN, JORDAN, 27-29 MAY 2013 Dust storm variability over EGYPT By Fathy M ELashmawy
More informationVariability and trends in daily minimum and maximum temperatures and in diurnal temperature range in Lithuania, Latvia and Estonia
Variability and trends in daily minimum and maximum temperatures and in diurnal temperature range in Lithuania, Latvia and Estonia Jaak Jaagus Dept. of Geography, University of Tartu Agrita Briede Dept.
More informationDefinitions Weather and Climate Climates of NYS Weather Climate 2012 Characteristics of Climate Regions of NYS NYS s Climates 1.
Definitions Climates of NYS Prof. Anthony Grande 2012 Weather and Climate Weather the state of the atmosphere at one point in time. The elements of weather are temperature, t air pressure, wind and moisture.
More informationClimates of NYS. Definitions. Climate Regions of NYS. Storm Tracks. Climate Controls 10/13/2011. Characteristics of NYS s Climates
Definitions Climates of NYS Prof. Anthony Grande 2011 Weather and Climate Weather the state of the atmosphere at one point in time. The elements of weather are temperature, air pressure, wind and moisture.
More informationIMPACTS OF A WARMING ARCTIC
The Earth s Greenhouse Effect Most of the heat energy emitted from the surface is absorbed by greenhouse gases which radiate heat back down to warm the lower atmosphere and the surface. Increasing the
More informationGlobal temperature record reaches one-third century
Dec. 16, 2011 Vol. 21, No. 7 For Additional Information: Dr. John Christy, (256) 961-7763 john.christy@nsstc.uah.edu Dr. Roy Spencer, (256) 961-7960 roy.spencer@nsstc.uah.edu Global temperature record
More informationWet plus Dry Deposition of Atmospheric Hg in the SE U.S. NADP Technical Meeting Sept , 2007 Boulder, CO, USA
Wet plus Dry Deposition of Atmospheric Hg in the SE U.S. NADP Technical Meeting Sept. 10-12, 2007 Boulder, CO, USA Outline Routine Measurements and Deposition Estimates Coarse Particle Hg Further Thoughts
More informationAnfang. German Arctic expeditions ASSW, March 27 April 1, 2011, Seoul, Korea. Foto: L. Tadday
Anfang German Arctic expeditions 2010-2011 ASSW, March 27 April 1, 2011, Seoul, Korea Foto: L. Tadday Overview: Research facilities around the globe Arctic Science Summit Week, March 27 April 1, 2011,
More informationAssessment of Ozone Variability in East Asia during Recent Years
EANET Research Fellowship Program 2005 Assessment of Ozone Variability in East Asia during Recent Years Eyi Wang 1) *, Tatsuya Sakurai 2) and Hiromasa Ueda 2) 1) Division of Air Polluting Monitoring, China
More informationCHAPTER 1. Geo Challenges 1A to 1D. & World Map Activity
CHAPTER 1 Geo Challenges 1A to 1D & World Map Activity SELECT YOUR CHALLENGE World Map Activity Challenge 1A Challenge 1B Challenge 1C Challenge 1D Challenge 1A WS PG. 2 STEP #1 Label the largest continent
More informationCORRELATION OF CLIMATIC AND SOLAR VARIATIONS OVER THE PAST 500 YEARS AND PREDICTING GLOBAL CLIMATE CHANGES FROM RECURRING CLIMATE CYCLES
Easterbrook, D.J., 2008, Correlation of climatic and solar variations over the past 500 years and predicting global climate changes from recurring climate cycles: International Geological Congress, Oslo,
More informationModelling of Mercury in the Arctic with the Danish Eulerian Hemispheric Model
Atmos. Chem. Phys., 4, 2251 2257, 2004 SRef-ID: 1680-7324/acp/2004-4-2251 European Geosciences Union Atmospheric Chemistry and Physics Modelling of Mercury in the Arctic with the Danish Eulerian Hemispheric
More informationAtlantic Ocean-North Africa-Middle East climate linkages through the Holocene
ACCWW Meeting, LDEO, July 29 Atlantic Ocean-North Africa-Middle East climate linkages through the Holocene Yochanan Kushnir (LDEO) and Mordechai Stein (Geological Survey of Israel) Work inspired by discussions
More informationRevisi&ng the GEOS- Chem atmospheric Hg simula&on: chemistry and emissions
Revisi&ng the GEOS- Chem atmospheric Hg simula&on: chemistry and emissions Hannah M. Horowitz Daniel J. Jacob, Helen M. Amos, Theodore S. Dibble, Franz Slemr, Johan A. Schmidt, Daniel A. Jaffe, Seth Lyman,
More informationMarch was 3rd warmest month in satellite record
April 4, 2016 Vol. 25, No. 12 For Additional Information: Dr. John Christy, (256) 961-7763 john.christy@nsstc.uah.edu Dr. Roy Spencer, (256) 961-7960 roy.spencer@nsstc.uah.edu Global Temperature Report:
More information1 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 informationVertical distribution of gaseous elemental mercury in Canada
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. D9, 4264, doi:10.1029/2002jd002116, 2003 Vertical distribution of gaseous elemental mercury in Canada C. M. Banic, 1 S. T. Beauchamp, 2 R. J. Tordon, 2 W.
More information1 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 informationFactors that Affect Climate
Factors that Affect Climate What is climate? Climate is the average weather conditions over a long period of time Includes average temperatures and precipitation, wind patterns, humidity, air pressure
More informationAddressing water quantity and quality concerns in the Peace-Athabasca Delta, northern Alberta, from perspectives of the past
Addressing water quantity and quality concerns in the Peace-Athabasca Delta, northern Alberta, from perspectives of the past Brent Wolfe, PhD Associate Professor Department of Geography and Environmental
More informationThe Arctic Energy Budget
The Arctic Energy Budget The global heat engine [courtesy Kevin Trenberth, NCAR]. Differential solar heating between low and high latitudes gives rise to a circulation of the atmosphere and ocean that
More informationNew Science Implementation in CMAQ-Hg: Test over a Continental United States Domain
New Science Implementation in CMAQ-Hg: Test over a Continental United States Domain Che-Jen Lin 1, Pruek Pongprueksa 1, Taruna Vanjani Thomas C. Ho 1, Hsing-wei Chu 1 & Carey Jang 2 1 College of Engineering,
More informationCMAQ Modeling of Atmospheric Mercury
CMAQ Modeling of Atmospheric Mercury CMAQ Model Peer Review December 17, 2003 O. Russell Bullock, Jr.* Atmospheric Sciences Modeling Division NOAA - Air Resources Laboratory * On assignment to the National
More information3. Climate Change. 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process
3. Climate Change 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process 3.1 Observations Need to consider: Instrumental climate record of the last century or
More informationL.O Students will learn about factors that influences the environment
Name L.O Students will learn about factors that influences the environment Date 1. At the present time, glaciers occur mostly in areas of A) high latitude or high altitude B) low latitude or low altitude
More informationGlobal Temperature Report: December 2018
Jan 2, 2019 Vol. 28, No. 9 For Additional Information: Dr. John Christy, (256) 961-7763 christy@nsstc.uah.edu Dr. Roy Spencer, (256) 961-7960 spencer@nsstc.uah.edu Global Temperature Report: December 2018
More informationWhat is the IPCC? Intergovernmental Panel on Climate Change
IPCC WG1 FAQ What is the IPCC? Intergovernmental Panel on Climate Change The IPCC is a scientific intergovernmental body set up by the World Meteorological Organization (WMO) and by the United Nations
More informationThe MSC Beaufort Wind and Wave Reanalysis
The MSC Beaufort Wind and Wave Reanalysis Val Swail Environment Canada Vincent Cardone, Brian Callahan, Mike Ferguson, Dan Gummer and Andrew Cox Oceanweather Inc. Cos Cob, CT, USA Introduction: History
More informationJ17.3 Impact Assessment on Local Meteorology due to the Land Use Changes During Urban Development in Seoul
J17.3 Impact Assessment on Local Meteorology due to the Land Use Changes During Urban Development in Seoul Hae-Jung Koo *, Kyu Rang Kim, Young-Jean Choi, Tae Heon Kwon, Yeon-Hee Kim, and Chee-Young Choi
More informationCauses of high PM 10 values measured in Denmark in 2006
Causes of high PM 1 values measured in Denmark in 26 Peter Wåhlin and Finn Palmgren Department of Atmospheric Environment National Environmental Research Institute Århus University Denmark Prepared 2 October
More informationImpacts of Climate Change on Autumn North Atlantic Wave Climate
Impacts of Climate Change on Autumn North Atlantic Wave Climate Will Perrie, Lanli Guo, Zhenxia Long, Bash Toulany Fisheries and Oceans Canada, Bedford Institute of Oceanography, Dartmouth, NS Abstract
More informationLAB J - WORLD CLIMATE ZONES
Introduction LAB J - WORLD CLIMATE ZONES The objective of this lab is to familiarize the student with the various climates around the world and the climate controls that influence these climates. Students
More informationAniekan Eyoh 1* Department of Geoinformatics & Surveying, Faculty of Environmental Studies, University of Uyo, Nigeria
Available online at http://euroasiapub.org/journals.php, pp. 53~62 Thomson Reuters Researcher ID: L-5236-2015 TEMPORAL APPRAISAL OF LAND SURFACE TEMPERATURE DYNAMICS ACROSS THE NINE STATES OF NIGER DELTA
More informationDELINEATION OF A POTENTIAL GASEOUS ELEMENTAL MERCURY EMISSIONS SOURCE IN NORTHEASTERN NEW JERSEY SNJ-DEP-SR11-018
DELINEATION OF A POTENTIAL GASEOUS ELEMENTAL MERCURY EMISSIONS SOURCE IN NORTHEASTERN NEW JERSEY SNJ-DEP-SR11-18 PIs: John R. Reinfelder (Rutgers University), William Wallace (College of Staten Island)
More informationCyclogenesis in the Western Mediterranean causing Heavy-Rain Events (NEPTUN)
Cyclogenesis in the Western Mediterranean causing Heavy-Rain Events (NEPTUN) A Proposal for a coordinated mission of the HALO research aircraft in the field Transport processes and atmospheric dynamics
More informationEddy and Chlorophyll-a Structure in the Kuroshio Extension Detected from Altimeter and SeaWiFS
14th Symposium on Integrated Observing and Assimilation Systems for the Atmosphere, Oceans, and Land Surface (IOAS-AOLS), AMS Atlanta, January 17-21, 21 Eddy and Chlorophyll-a Structure in the Kuroshio
More informationAtmospheric Aerosol in High Latitudes: Linkages to Radiative Energy Balance and Hydrological Cycle
Atmospheric Aerosol in High Latitudes: Linkages to Radiative Energy Balance and Hydrological Cycle Irina N. Sokolik School of Earth and Atmospheric Sciences Georgia Institute of Technology Atlanta, GA,
More informationPage 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 informationMet Éireann Climatological Note No. 15 Long-term rainfall averages for Ireland,
Met Éireann Climatological Note No. 15 Long-term rainfall averages for Ireland, 1981-2010 Séamus Walsh Glasnevin Hill, Dublin 9 2016 Disclaimer Although every effort has been made to ensure the accuracy
More information2016 Meteorology Summary
2016 Meteorology Summary New Jersey Department of Environmental Protection AIR POLLUTION AND METEOROLOGY Meteorology plays an important role in the distribution of pollution throughout the troposphere,
More informationWhat is Climate? Understanding and predicting climatic changes are the basic goals of climatology.
What is Climate? Understanding and predicting climatic changes are the basic goals of climatology. Climatology is the study of Earth s climate and the factors that affect past, present, and future climatic
More informationSPATIAL AND TEMPORAL DISTRIBUTION OF AIR TEMPERATURE IN ΤΗΕ NORTHERN HEMISPHERE
Global Nest: the Int. J. Vol 6, No 3, pp 177-182, 2004 Copyright 2004 GLOBAL NEST Printed in Greece. All rights reserved SPATIAL AND TEMPORAL DISTRIBUTION OF AIR TEMPERATURE IN ΤΗΕ NORTHERN HEMISPHERE
More informationAmmonia from space: how good are current measurements and what could future instruments tell us
Ammonia from space: how good are current measurements and what could future instruments tell us Karen Cady-Pereira 1, Mark Shephard 2, Daven Henze 3, Juliet Zhu 3, Jonathan Wrotny 1, Jesse Bash 5, Armin
More informationSO2 observation at the summit of Mt. Fuji
SO observation at the summit of Mt. Fuji Yasuhito Igarashi 1, Yosuke Sawa 1, Katsuhiro Yoshioka, Hiroshi Takahashi 3, Hidekazu Matsueda 1, Yukiko Dokiya 1 Geochemical Research Department, Meteorological
More informationTropical 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 informationA Synoptic Climatology of Heavy Precipitation Events in California
A Synoptic Climatology of Heavy Precipitation Events in California Alan Haynes Hydrometeorological Analysis and Support (HAS) Forecaster National Weather Service California-Nevada River Forecast Center
More informationImplications 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 informationReal World Globes Investigating Surface Currents around the Globe Authored by Ryan Glaubke, Graduate Student at Old Dominion University, Norfolk, VA
Real World Globes Investigating Surface Currents around the Globe Authored by Ryan Glaubke, Graduate Student at Old Dominion University, Norfolk, VA Purpose: - To practice basic plotting techniques using
More informationApproach Estimating Mercury Dry Deposition for AMNeT Leiming Zhang
Approach Estimating Mercury Dry Deposition for AMNeT Leiming Zhang Air Quality esearch Division Science and Technology Branch Environment Canada, Toronto Gaseous oxidized Hg (GOM) Particulate-bound Hg
More informationImpact of Climate Change on Water Availability in the Near East
GLOWA Jordan River Impact of Climate Change on Water Availability in the Near East H. Kunstmann, P. Suppan, A. Heckl Forschungszentrum Karlsruhe, IMK-IFU S. Krichak, P. Alpert, C. Price Tel Aviv University
More informationGerman Arctic Expeditions
German Arctic Expeditions 2015-2016 FARO/ASSW, 2016, Fairbanks Dirk Mengedoht (Alfred Wegener Institute, Germany) Dirk Mengedoht, AWI Logistics 2015 Polarstern Arctic Expeditions 2015 Leg Start End Mission
More informationJRC MARS Bulletin Crop monitoring in Europe January 2016 Weakly hardened winter cereals
Online version Issued: 25January 2016 r JRC MARS Bulletin Vol. 24 No 1 JRC MARS Bulletin Crop monitoring in Europe January 2016 Weakly hardened winter cereals A first cold spell is likely to have caused
More informationlecture 12 Paleoclimate
lecture 12 Paleoclimate OVERVIEW OF EARTH S CLIMATIC HISTORY Geologic time scales http://www.snowballearth.org/index.html Features of the climate during the Cretaceous period the land-sea distribution
More informationWHAT IS THE EARTH MADE OF? LITHOSPHERE AND HYDROSPHERE
UNIT 8 WHAT IS THE EARTH MADE OF? LITHOSPHERE AND HYDROSPHERE TABLE OF CONTENTS 1 THE STRUCTURE OF THE EARTH... 2 2 THE FORMATION OF THE RELIEF: INTERNAL AND EXTERNAL FORCES.... 2 2.1 Internal forces:
More informationSeasonal forecast from System 4
Seasonal forecast from System 4 European Centre for Medium-Range Weather Forecasts Outline Overview of System 4 System 4 forecasts for DJF 2015/2016 Plans for System 5 System 4 - Overview System 4 seasonal
More informationGlobal atmospheric model for mercury including oxidation by bromine atoms
Global atmospheric model for mercury including oxidation by bromine atoms The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters. Citation
More information2. There may be large uncertainties in the dating of materials used to draw timelines for paleo records.
Limitations of Paleo Data A Discussion: Although paleoclimatic information may be used to construct scenarios representing future climate conditions, there are limitations associated with this approach.
More informationWorld Geography Chapter 3
World Geography Chapter 3 Section 1 A. Introduction a. Weather b. Climate c. Both weather and climate are influenced by i. direct sunlight. ii. iii. iv. the features of the earth s surface. B. The Greenhouse
More informationAntarctic Automatic Weather Station Data for the calendar year 2000
Antarctic Automatic Weather Station Data for the calendar year 2000 by Linda M. Keller George A. Weidner Charles R. Stearns Matthew T. Whittaker Robert E. Holmes Matthew A. Lazzara Space Science and Engineering
More informationFactors influencing the large-scale distribution of Hg In the Mexico City area and over the North Pacific
University of New Hampshire University of New Hampshire Scholars' Repository Earth Sciences Scholarship Earth Sciences -11- Factors influencing the large-scale distribution of Hg In the Mexico City area
More informationMajor Domain of the Earth
Major Domain of the Earth The surface of the earth is a complex zone in which three main components of the environment meet, overlap and interact. The solid portion of the earth on which we live is called
More informationEuro Chlor Science Dossier 14. February 2009
Euro Chlor Science Dossier 14 February 2009 This publication is the fourteenth in a series of Science Dossiers providing the scientific community with reliable information on selected issues. If you require
More informationStream Discharge and the Water Budget
Regents Earth Science Unit 6: Water Cycle & Climate Name: Lab # Stream Discharge and the Water Budget Introduction: The United States Geological Survey (USGS) measures and publishes values for the daily
More informationTotal depletion of Hg in the upper troposphere lower stratosphere
GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L23804, doi:10.1029/2007gl031366, 2007 Total depletion of Hg in the upper troposphere lower stratosphere R. Talbot, 1 H. Mao, 1 E. Scheuer, 1 J. Dibb, 1 and M. Avery
More informationOceanic air-water exchange of Persistent Organic Pollutants (POPs) and aerosol carbon at a global scale
Oceanic air-water exchange of Persistent Organic Pollutants (POPs) and aerosol carbon at a global scale Elena Jurado 1, Rafel Simó 2, Jordi Dachs 1 1 Environmental Chemistry Department, CSIC Barcelona
More informationRegional Climate Change: Current Impacts and Perspectives Greater Lake Nipissing Stewardship Council Annual Meeting Wednesday April 16, 2014
Regional Climate Change: Current Impacts and Perspectives Greater Lake Nipissing Stewardship Council Annual Meeting Wednesday April 16, 2014 Speaker: Peter Bullock, Stantec Consulting Information Source:
More informationEarth s Heat Budget. What causes the seasons? Seasons
Earth s Heat Budget Solar energy and the global heat budget Transfer of heat drives weather and climate Ocean circulation A. Rotation of the Earth B. Distance from the Sun C. Variations of Earth s orbit
More informationURBAN HEAT ISLAND IN SEOUL
URBAN HEAT ISLAND IN SEOUL Jong-Jin Baik *, Yeon-Hee Kim ** *Seoul National University; ** Meteorological Research Institute/KMA, Korea Abstract The spatial and temporal structure of the urban heat island
More informationClimate Dynamics (PCC 587): Hydrologic Cycle and Global Warming
Climate Dynamics (PCC 587): Hydrologic Cycle and Global Warming D A R G A N M. W. F R I E R S O N U N I V E R S I T Y O F W A S H I N G T O N, D E P A R T M E N T O F A T M O S P H E R I C S C I E N C
More informationExamples of Pressure Gradient. Pressure Gradient Force. Chapter 7: Forces and Force Balances. Forces that Affect Atmospheric Motion 2/2/2015
Chapter 7: Forces and Force Balances Forces that Affect Atmospheric Motion Fundamental force - Apparent force - Pressure gradient force Gravitational force Frictional force Centrifugal force Forces that
More informationAPPENDIX G-7 METEROLOGICAL DATA
APPENDIX G-7 METEROLOGICAL DATA METEOROLOGICAL DATA FOR AIR AND NOISE SAMPLING DAYS AT MMR Monthly Normals and Extremes for Honolulu International Airport Table G7-1 MMR RAWS Station Hourly Data Tables
More informationTropical Climates Zone
Tropical Climates Zone RAIN FOREST CENTRAL AFRICA, SOUTH AMERICA (AMAZON), CENTRAL AMERICA, S.E. ASIA HUMID/WARM ANNUAL RAINFALL 200 CM TYPE #1: TROPICAL DESERT N. AFRICA (SAHARA) & S.W. ASIA < 25 CM
More informationD15: Simulation of a Dust Event over Cyprus
D15: Simulation of a Dust Event over Cyprus An episode of low visibility was observed over Cyprus in late September 2011. It appears that it was caused by an increase in the atmospheric dust concentration
More informationRegents Earth Science Unit 1 Earth Dimensions
Regents Earth Science Unit 1 Earth Dimensions www. BarnesWeb.org 2014-15 edition Name: Name: OBJECTIVES Correctly define: isolines, gradient, topographic map, contour interval, hachured lines, profile,
More informationarc setup and seasonal adjustments manual Solar timepiece
arc setup and seasonal adjustments manual Solar timepiece 1 Welcome / Care of your heliosphere Parts of your Heliosphere Welcome to experiencing solar time for your specific spot on the globe with your
More information1 What Is Climate? TAKE A LOOK 2. Explain Why do areas near the equator tend to have high temperatures?
CHAPTER 3 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 informationClimate Variability in South Asia
Climate Variability in South Asia V. Niranjan, M. Dinesh Kumar, and Nitin Bassi Institute for Resource Analysis and Policy Contents Introduction Rainfall variability in South Asia Temporal variability
More information