MAX-DOAS#1, North Direction

Slides:



Advertisements
Similar presentations
What is motion? An object is in motion if it changes position over time compared to a reference point.
Advertisements

Numerical Modelling of Dust Events for DODO and the Development of a New Dust Scheme in the UM Duncan Ackerley Ellie Highwood Mark Harrison Claire McConnell.
JERAL ESTUPINAN National Weather Service, Miami, Florida DAN GREGORIA National Weather Service, Miami, Florida ROBERTO ARIAS University of Puerto Rico.
FIRE AND BIOFUEL CONTRIBUTIONS TO ANNUAL MEAN AEROSOL MASS CONCENTRATIONS IN THE UNITED STATES ROKJIN J. PARK, DANIEL J. JACOB, JENNIFER A. LOGAN AGU FALL.
Origin and distribution of ozone in the Eastern Mediterranean - Results with GEOS-CHEM simulations Origin and distribution of ozone in the Eastern Mediterranean.
Anthropogenic Aerosol – A Cause Of The Weekend Effect? A significant weekly cycle has been found in diurnal temperature range (DTR). A candidate for causing.
Demonstration of seasons. Procedure 1.Identify the corners of the room as North, South, East and West. 2. Student A is at the centre of the classroom.
Effects of Siberian forest fires on regional air quality and meteorology in May 2003 Rokjin J. Park with Daeok Youn, Jaein Jeong, Byung-Kwon Moon Seoul.
Regional Air Quality Modeling: Long Range Global Change Simulations.
Selected Problems from Chapter o.
ANTHROPOGENIC AND VOLCANIC CONTRIBUTIONS TO THE DECADAL VARIATIONS OF STRATOSPHERIC AEROSOL Mian Chin, NASA Goddard Space Flight Center Plus: Thomas Diehl,
Irie et al., Multi-component retrievals for MAX-DOAS, 2 nd CINDI workshop, Brussels, March 10-11, 2010 Multi-component vertical profile retrievals for.
Atmospheric Monitoring in the TA experiment
Comparative Resources, North and South, Comparative Transportation Systems, of 3.
Long − Range Transport of Asian Sulfate and Its Effects on the Canadian Sulfate Burden Aaron van Donkelaar, Randall V. Martin – Dalhousie University W.
SHINE SEP Campaign Events: Long-term development of solar corona in build-up to the SEP events of 21 April 2002 and 24 August 2002 A. J. Coyner, D. Alexander,
EQ 3: Where do people live and why? 10/29 Bellringer: Analyze the Cartogram below – write 3 observations and 1 inference for an observation.
Melanie Follette-Cook Christopher Loughner (ESSIC, UMD) Kenneth Pickering (NASA GSFC) CMAS Conference October 27-29, 2014.
Page 1© Crown copyright Aircraft observations of mineral dust.
Presented at the AQAST 9 th Semiannual Meeting Wednesday June 3 rd, 2015 Presentation by: Dan Goldberg, Ph.D. Candidate Co-authors: Tim Canty, Tim Vinciguerra,
AEROSOL & CLIMATE ( IN THE ARCTIC) Pamela Lehr METEO 6030 Spring 2006
Mitglied der Helmholtz-Gemeinschaft Unsere Ziele Observations of Cirrus Clouds and Trace Gases in the Extra-Tropical UTLS by CRISTA-NF Martin Riese (1),
One case study for the aerosol layer originated from siberian forest fire during the latter days of May Kohei HONDA Atmospheric Environment Division.
1 RADAR INTER-COMPARISON AS A REFLECTIVITY CALIBRATION CHECK RADAR MONITORING WORKSHOP ERAD 2010 SIBIU ROMANIA Mike Dixon National Center for Atmospheric.
Overview of the Canadian Contribution to INTEX-B Randall Martin, Aaron van Donkelaar, Thomas Walker, Tom Duck Dalhousie University Richard Leaitch, Anne.
February 21, 2006 Lab Dan Kurz & Matt Chyba Team 4.
Stars - Circumpolar.  These constellations can be seen all year long, for they never set below the horizon.  Examples include Ursa Major, Ursa Minor,
Springtime Airmass Transport Pathways to the US Prepared by: Rudolf B. Husar and Bret Schichtel CAPITACAPITA,Washington University, Saint Louis, Missouri.
Airborne in-situ measurements of transported mineral dust aerosols in the Mediterranean region 1 Cyrielle Denjean *, Paola Formenti, Claudia Di Biagio,
The regional chemical transport model, STEM, with advanced photochemical modules including SAPRC99 mechanism, KPP chemical solver and explicit photolysis.
Population10/23 Bellringer: Analyze the Cartogram below – what do you see (5 observations)? What does this map mean?
ORIGIN OF BACKGROUND OZONE IN SURFACE AIR OVER THE UNITED STATES: CONTRIBUTION TO POLLUTION EPISODES Daniel J. Jacob and Arlene M. Fiore Atmospheric Chemistry.
Assessment of Upper atmospheric plume models using Calipso Satellites and Environmental Assessment and Forecasting Chowdhury Nazmi, Yonghua Wu, Barry Gross,
Hitoshi Irie Center for Environmental Remote Sensing (CEReS)
Astronomy The Path of the Sun.
Moon Phases Simulation
CAST – sonde activities
Michigan Comprehensive Crash Data Analysis
Physical Features North Africa GOVERNMENT RELIGION RESOURCES
Gas & Aerosol boundary conditions to Chimere from GEOS-Chem
MAX-DOAS#1, North Direction
Lesson 3: Seasons on earth notes
Daniel J. Jacob Harvard University
Absolute calibration of sky radiances, colour indices and O4 DSCDs obtained from MAX-DOAS measurements T. Wagner1, S. Beirle1, S. Dörner1, M. Penning de.
Impact of the vertical resolution on Climate Simulation using CESM
Modelling the radiative impact of aerosols from biomass burning during SAFARI-2000   Gunnar Myhre, Terje K. Berntsen, James M. Haywood, Jostein K. Sundet,
Calculation of Background PM 2.5 Values
What is motion? An object is in motion if it changes position over time compared to a reference point.
Preliminary Ozone Results from the TF HTAP Model Intercomparison
Jenny L. Perry and Patrick M. Owens Department of Chemistry
William J Hernandez David Gonzalez April 29, 2016
SVA measurement for CHIBA Campaign 2017
Asian outflow and chemical evolution of ozone and nitrogen oxides over the Pacific Mathew Evans, Daniel Jacob, Harvard Group, TRACE-P Science Team et al.
How Do We Use Earth’s Motion to Determine the Length of a Day?
MAX-DOAS#1, North Direction
Weather Rainy season ended..
MAX-DOAS#1, North Direction
MAX-DOAS#1, North Direction
1. Air passing mountains ”…Although this conceptual model seems to work well for westerly flow over topography, an attempt to apply it to easterly flow.
MAX-DOAS#1, North Direction
MAX-DOAS#1, North Direction
MAX-DOAS#1, North Direction
MAX-DOAS#1, North Direction
CALIPSO Total Attenuated Backscatter 532 nm 7 June 2006 Volcanic plume
Objectives (Chiba Campaign 2018)
SVA measurement for CHIBA Campaign 2017
START DIRECTIONS QUIZ.
MAX-DOAS#1, North Direction
Simultaneous observation of above-anvil ice plume and plume-shaped BTD anomaly atop a convective storm Mária Putsay, André Simon, Martin Setvák, Ildikó.
MAX-DOAS#1, North Direction
Presentation transcript:

MAX-DOAS 2d plots for Chiba Campaign 2017 Observation day 5: 07/15/2017 Hoque

MAX-DOAS#1, North Direction

MAX-DOAS#2, West Direction

MAX-DOAS#3, East Direction

MAX-DOAS#4, South Direction

Comments after a quick look of the plots Another great day for measurements. Very clear sky with very few thin cirrus clouds above 6km [according to Masuda-san’s (Tohuku University) measurements, LIDAR and sky view camera]. So the aerosol measurements from our 4 AZ MAX-DOAS system were homogenous in all the directions. Interestingly, the trace gas concentrations (NO2(>5ppbv),SO2(>4ppbv, HCHO(>3 ppbv) in all the four directions are higher comparative to the previous day (07/14/2017), although it was Saturday. Besides, the SO2 concentration reached up to 10ppbv in the east (#3) and south (#4) direction, whereas concentration in the north (#1) and west (#1) direction were >4ppbv.The reason is not clear whether it is due to enhanced local emissions or anthropogenic activities or long range transport. From the two very clear sky day measurements it seems that, the aerosol distribution around Chiba is almost homogenous. Although Damiani san’s comparison shows that, the correlation between MAX-DOAS and Himawari 8 AOD varies in different directions. But more observations and further analysis are required to reach a comprehensive conclusion.