Mercury: Difference between revisions
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==== Recommendations for running v9-01-02 ==== | ==== Recommendations for running v9-01-02 ==== | ||
The following are recommendations for running the v9-01-02 Hg simulation at 4x5, based on the work of Amos et al (2011, in prep): | The following are recommendations for running the v9-01-02 Hg simulation at 4x5 with the GEIA 2005 anthropogenic emission inventory, based on the work of Amos et al (2011, in prep): | ||
1. Decrease photoreduction in the atmospheric and surface ocean. | 1. Decrease photoreduction in the atmospheric and surface ocean. | ||
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The following issues were discovered in after the release of [[GEOS-Chem v9-01-01]]. We shall correct these in the next version, [[GEOS-Chem v9-01-02]]. | The following issues were discovered in after the release of [[GEOS-Chem v9-01-01]]. We shall correct these in the next version, [[GEOS-Chem v9-01-02]]. | ||
==== De-hardwire file path BR_DIR in global_br_mod.f ==== | ==== De-hardwire file path BR_DIR in global_br_mod.f ==== | ||
Revision as of 16:20, 2 October 2011
On this page we include information relevant to the GEOS-Chem mercury simulations. Please also visit our Global Terrestrial Mercury Model page, which is an option that can be used with the GEOS-Chem mercury simulation.
For a list of current and on-going mercury projects, please visit the Hg and POPs Working Group page!
Code
GEOS-Chem v9-01-02
Recommendations for running v9-01-02
The following are recommendations for running the v9-01-02 Hg simulation at 4x5 with the GEIA 2005 anthropogenic emission inventory, based on the work of Amos et al (2011, in prep):
1. Decrease photoreduction in the atmospheric and surface ocean.
In mercury_mod.f, Old: K_RED_JNO2 = 3.5d-3 New: K_RED_JNO2 = 3.5d-3 / 2d0
In ocean_mercury_mod.f, Old: k_radbase = 1.73d-6 New: k_radbase = 0.90d0 * 1.73d-6
2. Dry deposit gaseous Hg(II) with near-near surface resistance.
In drydep_mod.f (for Hg2), Old: HSTAR(NUMDEP) = 1.0d+6 New: HSTAR(NUMDEP) = 1.0d+14
3. Adjust the speciation of fossil fuel combustion emissions from (Hg0:Hg2:HgP) 50:40:10 to 90:7:3. Fossil fuel emissions make up ~47% of total global anthropogenic emissions in the GEIA 2005 inventory.
In mercury_mod.f, apply the following scaling factors:
EHg0_an = 1.27d0 * EHg0_an
EHg2_an = 0.40d0 * EHg2_an
EHgP_an = 0.51d0 * EHgP_an
-- Helen M Amos, 13:23 23 Sep 2011 (EDT)
The following issues were discovered in after the release of GEOS-Chem v9-01-01. We shall correct these in the next version, GEOS-Chem v9-01-02.
De-hardwire file path BR_DIR in global_br_mod.f
A typo was discovered in the source code file global_br_mod.f.
Chris Holmes wrote:
- The variable BR_DIR was previously hard-coded with an absolute file path that would only work on the Harvard AS servers. With [my submitted fix], the directory with Br data is constructed from the DATA_DIR variable (in directory_mod.f), analogous to the way most other directories are found. This should make the code run more easily on systems outside Harvard.
--Bob Y. 11:35, 25 July 2011 (EDT)
Negative aquatic mercury concentrations
There was a bug in ocean_mercury_mod.f that occasionally allowed the concentrations of aqueous mercury in the ocean to be negative. This has been fixed by changing the way the rate of change of ocean mixed layer depths is calculated and adding error traps to set negative mixed layer depths and negative oceanic mercury concentrations to zero. This will be standard in GEOS-Chem v9-01-02.
--Jenny Fisher 17:46, 8 July 2011 (EDT)
Division by zero error
There is a div by 0 error in mercury_mod.f FUNCTION GET_BR that affects v8-03-02 and v9-01-01. It's a quick fix.
Replace: BR_FAC = ( 1440d0 / TTDAY(I,J) ) with: BR_FAC = SAFE_DIV( 1440d0, TTDAY(I,J), 0d0) Replace: BR_FAC = BR_FAC / ( 4D-4 * TTDAY(I,J) ) with: BR_FAC = SAFE_DIV( BR_FAC, 4D-4* TTDAY(I,J), 0d0) And add: !Refernces to F90 modules USE ERROR_MOD, ONLY: SAFE_DIV
Sometimes TTDAY is 0, so BR_FAC becomes Inf and C_BR becomes Inf. The problem trickles down and shows up as PL-HG2-$ diagnostics Hg2_OH, Hg2_O3, Hg2_BR, and Br diagnostics having NaNs in their arrays. Adding the SAFE_DIV fixes the problem. (H Amos, 9 Mar 2011)
This fix will be standardized in GEOS-Chem v9-01-02.
--hamos 10:46, 9 March 2011 (EST)
--Bob Y. 11:35, 25 July 2011 (EDT)
Bug fixes for ND03 mercury diagnostics
Chris Holmes found and fixed several issues with the ND03 diagnostic (which only affects the offline Hg simulation).
Chris Holmes wrote:
- I found a bug in ND03 diagnostics in GEOS-Chem v9-01-01 (last updated 2011-5-27). The PL-HG2-$ diagnostics were not in the ctm.bpch file and the tracer names for these diagnostics were not in tracerinfo.dat. The reason is because there are more ND03 diagnostics than the number given in PD03. This has been a confusing and muddled part of the code for a long time. I fixed the bug with the attached patch and also simplified diag03_mod.f to hopefully make it easier to maintain as diagnostics are added or changed in the future.
- I confirmed that my changes to diag03_mod.f do not alter the diagnostic outputs, within expected REAL*4 precision.
- At the same time I was fixing the diagnostics, I found and corrected (with SAFE_DIV) a floating point overflow error in mercury_mod.f and removed legacy comments in mercury_mod.f that were left over from my personal debugging. I also corrected a diagnostic tracer name in gamap_mod.f, which was introduced when Anne Soerensen's ocean was added.
We also have restored printing of the soil Hg emissions to the standard output (aka the GEOS-Chem log file). This error was probably a relic of someone debugging.
--Bob Y. 11:35, 25 July 2011 (EDT)
VEGEMIS/GCAP bug fix
There was a bug introduced in v8-02-03 with the introduction of the logical LGCAPEMIS, which is designed to turn on or off scaling of GEIA emissions to Streets' 2006 regional GCAP emissions. This logical was then also used to turn off Hg emitted through transpiration, but this should be handled independently from the anthropogenic emissions. We have now introduced a new logical LVEGEMIS that allows you to turn these transpiration emissions on or off independently. This will be standard in GEOS-Chem v9-01-02.
--Jenny Fisher 09:43, 13 April 2011 (EDT)
--Bob Y. 11:35, 25 July 2011 (EDT)
GEOS-Chem v9-01-01
The following issues were fixed in the re-release of GEOS-Chem v9-01-01 (07 Jun 2011).
Omitted code in Hg simulation
We created a patch to fix this issue. This update was standardized in the re-release of v9-01-01.
- Designated as: v9-01-01-Patch-Hg
- Applied: 2011-04-13
- Authors: Chris Holmes, Jenny Fisher
- Signed off by: Bob Yantosca
Jenny Fisher wrote:
- After some discussion between Chris Holmes and I, we realized that some of his updates to the Hg code (i.e. the version published in his paper) didn't get properly implemented in v9-01-01. I haven't looked *extensively* through his code, but I have done a quick look through the obvious mercury routines and found a number of differences:
(1) In LAND_MERCURY_FLUX (land_mercury_mod.f)
The first IF statement was
IF ( (SNOW_HT > 1D0) .OR. (IS_ICE(I,J)) ) THEN
But should have been
IF ( (IS_ICE(I,J)) .OR. (IS_LAND(I,J) .AND. SNOW_HT>10d0) )THEN
(2) In BIOMASSHG (land_mercury_mod.f)
We currently have (with Bess's 50% reduction):
BBRatio_Hg_CO=1.05D-7
However, we should use this value from Holmes et al 2010:
BBRatio_Hg_CO=1D-7
(3) In SOILEMIS (land_mercury_mod.f):
This IF statement was
IF ( IS_LAND(I,J) .AND. (SNOW_HT < 1d0) ) THEN
But should have been
IF ( IS_LAND(I,J) .AND. (SNOW_HT < 10d0) ) THEN
(4) In SNOWPACK_MERCURY_FLUX (land_mercury_mod.f):
Residence time when T > -3C was 7 days; i.e.
K_EMIT = 1.6D-6
Should have been 3 weeks; i.e.
K_EMIT = 5D-7
(5) In ADD_HG2_SNOWPACK (depo_mercury_mod.f):
This IF statement was
IF ( (SNOW_HT > 1d0) .OR. (IS_ICE(I,J)) ) THEN
But should have been
IF ( (IS_ICE(I,J)) .OR. (IS_LAND(I,J) .AND. SNOW_HT > 10d0) ) THEN
We allowed 100% of deposited Hg available for emission; i.e.
SNOW_HG(I,J,NN) = SNOW_HG(I,J,NN) + MAX( DEP_HG2, 0D0 )
This Should have only been 60%; i.e.
SNOW_HG(I,J,NN) = SNOW_HG(I,J,NN) + MAX( 0.6D0*DEP_HG2, 0D0 )
(6) In OCEAN_MERCURY_FLUX (ocean_mercury_mod.f):
We had the old definition
IF ((ALBD(I,J) <= 0.4d0) .and. (FRAC_L < 0.8d0) .and. (MLDCM > 0.99d0)) THEN
Holmes et al 2010 used consistent criteria for ocean/land/ice categories
IF ( ( IS_WATER(I,J) ) .AND. ( MLDCM > 0.99d0 ) ) THEN
The patch, which is present in the re-release of v9-01-01 (07 Jun 2011) contains 3 individual commits named:
Fixed minor error in depo_mercury_mod.f Add comments to denote updates to Holmes 2010 Hg Update to Holmes et al. 2010 version
--Jenny Fisher 09:43, 13 April 2011 (EDT)
--Bob Y. 11:35, 25 July 2011 (EDT)
GEOS-Chem v8-03-02
Diagnostics fix for Hg simulation (Helen Amos, 30 September 2010):
If the WETDLS-$ and WETDCV-$ diagnostics are only showing up for Hg2 (and not for HgP) in your ctm.bpch file, make the following change to the 'Diagnostics Menu' in input.geos:
ND38: Cld Conv scav loss: 47 all ND39: Wetdep scav loss : 47 all
ND38: Cld Conv scav loss: 47 2 3 ND39: Wetdep scav loss : 47 2 3
Recommendations for running code versions 8-03-02 and later (eds):
- Reduce geogenic emissions by 50%
- ref. Soerensen et al. 2010
- mercury_mod.f line 3470:
EHg0_nt = EHg0_nt * 0.5D0 - Reduce biomass burning emissions by 50%
- ref. Soerensen et al. 2010
- land_mercury_mod.f line 225:
REAL*8, PARAMETER :: BBRatio_Hg_CO = 1.05D-7 - Reduce intermediate water mercury concentration in Southern Ocean to 0.9pM total
- ref. low end of uncertainty range Sunderland and Mason 2007
- ocean_mercury_mod.f line 2950:
CDEEPSAT = (/ 0.8d-10, 4.1d-10, 4.1d-10 /) - Reduce concentration of BrO in Arctic during depletion events to 5pptv
- ref. low end of uncertainty range in Holmes et al. 2010
- ref. low [BrO] observed Neuman et al. 2010
- mercury_mod.f line 3805:
REAL*8, PARAMETER :: BRO_POLAR=5D0 - Adopt Qiaoqiao Wang's modification to rainout & washout (this is standard in GEOS-Chem v9-01-01 and later)
- ref. Wang et al. 2011
- uncomment wetscav_mod.f line 4101:
F_RAINOUT = F_PRIME
! Washout occurs where there is no rainout
F_WASHOUT = MAX( FTOP - F_RAINOUT, 0d0 )
ELSE
F_RAINOUT = 0d0
F_WASHOUT = 0d0
ENDIF
- comment out wetscav_mod.f line 4121:
!F_WASHOUT = 0d0
!IF ( PDOWN(L,I,J) > 0d0 ) THEN
! IF (QQ(L,I,J) > 0d0) THEN
! F_RAINOUT = MAX( FTOP, F_PRIME )
! ENDIF
! F_WASHOUT = MAX( FTOP - F_RAINOUT, 0d0 )
!ENDIF
Previous discussions (6/2008)
- Standardize the solver. Everyone should use the solver Chris developed for the Hg chemistry
(located at ~cdh/GC/RevisedChem.v7-04-06/mercury_mod.f)- outstanding issue - dry dep of Hg0* <- currently working on this (eds)
- See GEOS-Chem v8-03-02 and later for Holmes et al. 2010 Hg+Br simulation.
- Catalog all emissions options and develop clear flagging system to choose your own adventure. This will include:
- different anthropogenic emissions scenarios/corrections (i.e Jaffe vs. Streets) <- going to work on the anthro emissions soon (eds),
- different land emissions. <- nvd will work on this
- Logicals implemented to select anthropogenic emissions from GEIA 2000, GEIA 2005, or GEIA scaled to Streets et al. 2006 regional totals.
- different anthropogenic emissions scenarios/corrections (i.e Jaffe vs. Streets) <- going to work on the anthro emissions soon (eds),
- Diagnostics. See separate section below.
- Diagnostics have been updated.
- Comment everything in the code. Remove old bits of code that are hanging around & commented out.
- Ongoing.
- GEOS-5
- This is the standard meteorology to use at present. MERRA is in development.
- Get the land stuff out of ocean_mercury_mod.f and into it's own module <- nvd will work on this
- Implemented by ccarouge v8-03-02.
Chemistry 'issues'
Dry deposition of HgP over snow/ice
The HgP dry deposition velocity over snow/ice is now set to a constant value to better match observational constraints. HgP is treated the same as all other fine aerosols in this respect. This update will be standard in v9-01-02. For more information see the dry deposition page. (Jenny Fisher, Harvard).
Previous discussions
- Oxidant.
- Chris has a simulation with Hg-Br chemistry and SS aerosol deposition; the global budget is ok, but the Br concentrations in the BL are too low to generate diurnal cycles. (cdh working on it)
- Snow/ice scavenging of HgII
- Cold-temperature wet scavenging of HgII is now included in the standard code.
- Dry deposition of "aqueous HgII.
- (Explanation from Chris: We calculate the fraction of HgII, Fg, which is gas phase. But we're currently applying the dry deposition velocity to both gas and aqueous fractions. I think it would be better to deposit the aqueous fraction at the velocity of HgP; this would be slower dep, but I don't know how much. This is definitely up for discussion.)
- See Holmes et al. 2010 for discussion of chemistry in standard version.
Diagnostics
Notes
- Helen Amos is developing diagnostics for reactive gaseous mercury and reactive particulate mercury.
- Bess Corbitt is developing diagnostics for a tagged-tracer simulation with 17 world regions. For example, when running with this option, for prompt recycling of deposited mercury, instead of HG-SRCE category and Hg0_ln tracer name for the total tracer, I would have category HG0-RECY and tracername Hg0_usa, Hg0_can, etc.
Previous discussions
Here are some suggested changes:
- Emissions should have units 'kg/m2/s' or something of the form 'mass/area/time' (they are currently 'kg'). The HG-SRCE diagnostic currently has all of the Ocean tracers and fluxes; these should go elsewhere.
- The Ocean Hg0, Hg2, HgC should have concentration units not kg. Is 'molar' the best choice? Fluxes of these should be in concentration/time, not kg.
- The ocean restart files should have concentration units not kg. They currently use the category 'OCEAN-HG' which would make sense for the ND03 ocean Hg0, Hg2, HgC output too.
- 'PL-HG2-$' doesn't really describe all of the fluxes in our model. There are a lot of diagnostic quantities which are either chemical P/L fluxes or rate constants. I think these should all be in one diagnostic called something like 'PL-HG-$' (or maybe 'PL-HG-A', 'PL-HG-O' to separate the atmosphere and ocean). The fluxes in this diagnostic would include redox in air and water, colloidal sinking, ocean-atmosphere piston velocity, ...
Here are the current GEOS-Chem Hg outputs
CATEGORY ILUN TRCNAME TRC UNIT TAU0(DATE) DIMENSIONS 1 : IJ-AVG-$ 23 Hg0 1 pptv 157776.00(2003010100) 72 46 30 2 : IJ-AVG-$ 23 Hg2 2 pptv 157776.00(2003010100) 72 46 30 3 : IJ-AVG-$ 23 HgP 3 pptv 157776.00(2003010100) 72 46 30 4 : WETDCV-$ 23 Hg2 3002 kg/s 157776.00(2003010100) 72 46 30 5 : WETDCV-$ 23 HgP 3003 kg/s 157776.00(2003010100) 72 46 30 6 : WETDLS-$ 23 Hg2 3002 kg/s 157776.00(2003010100) 72 46 30 7 : WETDLS-$ 23 HgP 3003 kg/s 157776.00(2003010100) 72 46 30 8 : HG-SRCE 23 Hg0_an 34001 kg 157776.00(2003010100) 72 46 1 9 : HG-SRCE 23 Hg0_aq 34002 kg 157776.00(2003010100) 72 46 1 10 : HG-SRCE 23 Hg0_oc 34003 kg 157776.00(2003010100) 72 46 1 11 : HG-SRCE 23 Hg0_ln 34004 kg 157776.00(2003010100) 72 46 1 12 : HG-SRCE 23 Hg0_na 34005 kg 157776.00(2003010100) 72 46 1 13 : HG-SRCE 23 Hg2_an 34006 kg 157776.00(2003010100) 72 46 1 14 : HG-SRCE 23 Hg2_aq 34007 kg 157776.00(2003010100) 72 46 1 15 : HG-SRCE 23 Hg2_sk 34008 kg 157776.00(2003010100) 72 46 1 16 : HG-SRCE 23 HgP_an 34009 kg 157776.00(2003010100) 72 46 1 17 : HG-SRCE 23 KwHg 34010 cm/h 157776.00(2003010100) 72 46 1 18 : HG-SRCE 23 HgC 34011 kg 157776.00(2003010100) 72 46 1 19 : HG-SRCE 23 Hg_to_C 34012 kg 157776.00(2003010100) 72 46 1 20 : PL-HG2-$ 23 Hg2_Hg0 35001 kg 157776.00(2003010100) 72 46 30 21 : PL-HG2-$ 23 Hg2_OH 35002 kg 157776.00(2003010100) 72 46 30 22 : PL-HG2-$ 23 Hg2_O3 35003 kg 157776.00(2003010100) 72 46 30 23 : PL-HG2-$ 23 Hg2_SS 35004 kg 157776.00(2003010100) 72 46 1 24 : PL-HG2-$ 23 Hg2_SSR 35005 /s 157776.00(2003010100) 72 46 1 25 : DRYD-FLX 23 Hg0df 36001 molec/cm2/s 157776.00(2003010100) 72 46 1 26 : DRYD-FLX 23 Hg2df 36002 molec/cm2/s 157776.00(2003010100) 72 46 1 27 : DRYD-FLX 23 HgPdf 36003 molec/cm2/s 157776.00(2003010100) 72 46 1 28 : DRYD-VEL 23 Hg2dv 37002 cm/s 157776.00(2003010100) 72 46 1 29 : DRYD-VEL 23 HgPdv 37003 cm/s 157776.00(2003010100) 72 46 1
I think we should change lines 8-24 (I've kept the same line numbers and TRCNAME, but changed CATEGORY, TRC, or UNIT):
CATEGORY TRCNAME TRC UNIT 8 : HG-SRCE Hg0_an 34001 kg/m2/s 10 : HG-SRCE Hg0_oc 34002 kg/m2/s 11 : HG-SRCE Hg0_ln 34003 kg/m2/s 12 : HG-SRCE Hg0_na 34004 kg/m2/s 13 : HG-SRCE Hg2_an 34005 kg/m2/s 16 : HG-SRCE HgP_an 34006 kg/m2/s 9 : OCEAN-HG Hg0_aq xxxx1 mol/L 14 : OCEAN-HG Hg2_aq xxxx2 mol/L 18 : OCEAN-HG HgC xxxx3 mol/L 20 : PL-HG-A Hg2_Hg0 35001 kg/m3/s 21 : PL-HG-A Hg2_OH 35002 kg/m3/s 22 : PL-HG-A Hg2_O3 35003 kg/m3/s 23 : PL-HG-A Hg2_SS 35004 kg/m3/s 24 : PL-HG-A Hg2_SSR 35005 /s 15 : PL-HG-O Hg2_sk xxxx1 kg/m3/s 19 : PL-HG-O Hg_to_C xxxx2 kg/m3/s 17 : PL-HG-O KwHg xxxx3 cm/h
The only thing I have to add is that at first I didn't realize that wet deposition of Hg(II) was composed of both WETDCV and WETDLS. Is it important to save those components out as 2 separate parts? (nvd)
To answer Nicole, it is useful to have the large scale and convective wet scavenging written out separately for comparison to wet deposition observations. They are different processes in the model and can tell us different things about where the model is performing well and where it needs improvement (for example, convective scavenging over the Gulf Coast region). (eds)
GTMM
GEOS-Chem v8-03-02 and higher versions provide the option to use the Global Terrestrial Mercury Model, which is a detailed land-surface model for use with the Hg simulations. Please see the following references for more information.
- Global Terrestrial Mercury Model wiki page
- GTMM User's Manual (PDF)
Soil Emissions
Unless you are running GTMM, soil emissions are a function of soil mercury concentrations in a prespecified file. The soil concentrations distributed in the mercury_201007 data directory were calculated by Holmes et al. (2010) using a highly-modified version of v8-02-03 and the method of Selin et al. (2008). This method calculates steady-state soil concentration and emissions for the preindustrial period, then imposes a 15% enhancement according to anthropogenic Hg deposition.
In principle, the soil Hg concentrations should be recalculated after any changes to the model, meteorology, or resolution to ensure self-consistent treatment of deposition and emissions. In practice, the changes to soil emissions may be small for some model updates and recalculating soil Hg may be unnecessary. But it is the model users' responsibilities to determine when to update his or her soil Hg files.
Users who want to update their soil Hg files may use IDL code developed by Chris Holmes. Please contact him directly.
Helen Amos wrote:
Here are step-by-step instructions for making a new soil distribution if you are not using GTMM. You will need to use the following IDL scripts written by Chris Holmes:
soilhgdist_uniform.pro soilhgdist.pro
Step 1: Use soilhgdist_uniform.pro to create a uniform soil distribution. Save file as 'soilhg.uniform.bpch'.
Step 2: In mercury_mod.f SUBROUTINE MERCURY_READYR, specify that you want to run with 'soilhg.uniform.bpch'.
Step 3: Run three years (e.g. 2004-2006) of pre-industrial simulation with uniform soil distribution. Specify that it's a pre-industrial simulation in the input.geos file.
Step 4: Use soilhgdist.pro to create a new, scaled soil distribution (saved as a bpch file) and to calculate the ratio of deposition/emission.
Step 5: Adjust SOIL_EMIS_FAC in land_mercury_mod.f by multiplying SOIL_EMIS_FAC * (deposition/emission), where deposition/emission is the ratio from Step 4.
Step 6: In mercury_mod.f SUBROUTINE MERCURY_READYR, change input file to new soil distribution created in Step 4.
Step 7: Run three years (e.g. 2004-2006) of pre-industrial simulation. Start this run from where Step 3 left off by renaming the restart.totHg.* and ocean.totHg.* files (i.e. rename restart.totHg.2007010100 to restart.totHg.2004010100).
Step 8: Repeat Steps 4-7 until pre-industrial soil distribution converges. You can check for convergences with Gamap routine CTM_PLOTDIFF.
Step 9: Once the pre-industrial soil distribution has converged to with 5%, run three years (e.g. 2004-2006) of a present day simulation with ONLY direct anthropogenic emissions. Specify that it's a present day simulation by setting 'Is it a pre-industrial sim?' to 'F' in the input.geos file. Specifiy that you only want direct anthropogenic emissions by setting the logical LAnthroHgOnly to 'T' in mercury_mod.f SUBROUTINE INIT_MERCURY. Make sure to read soil distribution from last steady-state pre-industrial run.
Step 10: Use soilhgdist.pro to create a present day soil distribution.
--Helen Amos 03:44, 13 Aug 2011 (EST)
References
- Wang, Q., D.J. Jacob, J.A. Fisher, J. Mao, E.M. Leibensperger, C.C. Carouge, P. Le Sager, Y. Kondo, J.L. Jimenez, M.J. Cubison, and S.J. Doherty, Sources of carbonaceous aerosols and deposited black carbon in the Arctic in winter-spring: implications for radiative forcing, Atm. Chem. Phys. Discuss., 11, 19395-19442, 2011.
- Holmes, C.D., D.J. Jacob, E.S. Corbitt, J. Mao, X. Yang, R. Talbot, and F. Slemr, Global atmospheric model for mercury including oxidation by bromine atoms, Atm. Chem. Phys., 10, 12,037-12,057, 2010
- Soerensen, A.L., E.M. Sunderland, C.D. Holmes, D.J. Jacob, R.M. Yantosca, H. Skov, J.H. Christensen, and R.P. Mason, An improved global model for air-sea exchange of mercury: High concentrations over the North Atlantic, Environ. Sci. Technol., 44, 8574-8580, 2010
- Smith-Downey, N.V., Sunderland, E.M., and Jacob, D.J., Anthropogenic impacts on global storage and emissions of mercury from terrestrial soils: insights from a new global model, J. Geophys. Res., 115, G03008, 2010
- S. Strode, L. Jaeglé, and N. E. Selin, Impact of mercury emissions from historic gold and silver mining: Global modeling, Atmos. Environ., 43, 2012-2017,2009
- Holmes, C.D., D.J. Jacob, R.P. Mason, D.A. Jaffe, Sources and deposition of reactive gaseous mercury in the marine atmosphere, Atm. Environ., 43, 2278-2285, 2009
- S. Strode, L. Jaeglé, D. A. Jaffe, P. C. Swartzendruber, N. E. Selin, C. Holmes, and R. M. Yantosca, Trans-Pacific Transport of Mercury, J. Geophys. Res., 112, D02308, 2008
- Selin, N.E. and D.J. Jacob. Seasonal and spatial patterns of mercury wet deposition in the United States: North American vs. intercontinental sources, Atm. Environ, 42, 5193-5204, 2008
- Selin, N.E., D.J. Jacob, R.M. Yantosca, S. Strode, L. Jaegle, and E.M. Sunderland, Global 3-D land-ocean-atmosphere model for mercury: present-day vs. pre-industrial cycles and anthropogenic enrichment factors for deposition, Glob. Biogeochem. Cycles, 22, GB2011, 2008
- Selin, N.E., D.J. Jacob, R.J. Park, R.M. Yantosca, S. Strode, L. Jaegle, and D. Jaffe, Chemical cycling and deposition of atmospheric mercury: Global constraints from observations, J. Geophys. Res, 112, DO2308, doi:10.1029/2006JD007450, 2007.
- Strode, S.A., L. Jaegle, N.E. Selin, D.J. Jacob, R.J. Park, R.M. Yantosca, R.P. Mason, and F. Slemr, Air-sea exchange in the global mercury cycle, Glob. Biogeochem. Cycles, 21, GB1017, 2006.
- Holmes, C. D., D. J. Jacob, and X. Yang, Global lifetime of elemental mercury against oxidation by atomic bromine in the free troposphere, Geophys. Res. Lett., 33, L20808, 2006.
--Bob Y. 11:40, 25 July 2011 (EDT)