BEE-spoke-data/govdocs1-by-extension huggingface dataset:
402              TRAVELS   IN
to watch the fruit when it is ripe. All the timber confifls in two up-rights and one crofs pole; it is covered with a matted roof, but this is well lined within by a quantity of bark. The inner fpace is rather below the level of the ground, and the entrance by a little fide-door; in the middle of the hut is the fire-place, from which the fmoke af-cends by an opening in the roof. On each fide of the fire, are raifed two branches, which run the length of the hut, and ferveto fleep on; thefe are covered with ikins and bark. Befide the favage who fpoke French, in this hut, there was afquah, the name given to the Indian women, who had taken him as her fecond, and was bringing up a child by her firft hufband; two old men compofed the remainder of the family, which had a melancholy and poor appearance. The fquah was hideous, as they all are, and her hufband almoft ftupid, fo that the charms of this fociety did not make me forget that the day was advancing, and that it was time to fet out. All that I could learn from the Colonel, or from the favages was, that the State gives them rations of meat, and fome-
times
Use your browser's 'File/Save As' option to save this entire page 
in your SHARP/RAOB directory (this text at the bottom won't matter).  

The default name for the saved file will be 'get_sharp.cgi'.  
Rename this file to 
                    DE000000.O54

and you should be able to run SHARP.

If SHARP doesn't recognize this site, you can update SHARP's
location.dat file by following the instructions pointed
to by the '?' link on the previous page.

You will probably NOT be able to modify this sounding in SHARP if the
dewpoint is missing.  HOWEVER, if you change the missing surface
dewpoint in the TTBB portion of the report from '//' to '99', you will
be able to modify the sounding if SHARP reads the sounding at all.
IN THE EAST AND WEST INDIES.
347
military navy ; and commerce will acquire a greater book
degree of extenfion throughout the whole univerfe.         XIX-
Commerce produces nothing of itfelf; for it is not commerce,
of a plaflic nature. Its bufinefs confifts in exchanges,
gy its operations, a town, a province, a nation, a part
of the globe, are difencumbered of what is ufelefs to
them, and receive what they are in want of. It is
perpetually engaged in fopplying the refpedive wants
ofmen. Its knowledge, its funds, and its labours, are
all devoted to this honourable and neceffary office. Its
influence could not exift without the arts and without
cultivation: but thefe would be very infignificant with-
out its influence. By pervading the earth, by eroding
the feas, by raifing the obftacles which oppofed them-
felves to the intercourfe or nations, by extending the
iphere or wants and the thirft of enjoyments, it mul-
tiplies labour, it encourages induftry, and becomes, in
fome meafure, the moving principle ofthe world.
The Phoenicians were the firft merchants of whom
hiftory hath preferved the remembrance. Situated on
the borders of the fea. on the confines of Afia and
Africa, to receive and difpenfe all the riches ofthe an-
cient world, they founded their colonies, ahd built
their cities, with no other view but that of commerce.
At Tyre, they were the mafters ofthe Mediterranean;
at Carthage, they laid the foundations of a republic
that traded, by the ocean, upon the richeft of the Eu-
ropean coafts.
The Greeks fucceeded the Phoenicians, as the Ro-
ws did the Carthaginians and the Greeks: they held
the dominion of the fea as well as of the land ; but
they carried on no other kind of commerce, except
that of conveying into Italy, for their own ufe, all the
tiches of Africa, Afia, and the conquered world. When
Rome had invaded the whole world, and had loft all
to acquifitions, commerce returned, as it were, to its
original fource towards the Eaft. There it was efta-
blifhed, while the Barbarians overran Europe. The
raphe was divided ; the din of arms, and the art of
% remained in the Weft ; Italy, however, preferved
BREEDING BIRD HABITAT USE IN RIPARIAN WET MEADOWS: DOES REED CANARY GRASS AFFECT 
BIRD TERRITORY PLACEMENT?

Eileen M. Kirsch, Wayne E. Thogmartin, Tim Fox, and Brian R. Gray 
USGS, Upper Midwest Environmental Sciences Center, La Crosse, WI, 54603.

Riparian wet meadows are rare in the upper Midwestern US due to river 
development, conversion of floodplains to agriculture, and urbanization.  Most 
remaining wet meadows are dominated by invasive reed canary grass (Phalaris 
arundinacea), and wet meadows dominated by native vegetation communities are 
very rare.  The prevailing notion among resource managers is that reed canary 
grass is of little value to birds and other wildlife.  In 2001 and 2002, we 
studied breeding bird habitat use and estimated an index of productivity in 
riparian wet meadows across a range of reed canary grass dominance.  We selected 
12 riparian wet meadows in southeastern Minnesota and southwestern Wisconsin for 
study in 2001 and added another in 2002.  We used spot mapping to estimate 
locations and sizes of bird territories, and indexed productivity from observed 
behavior.  Vegetation features were estimated every 50 meters in a grid pattern 
at each study plot in late July.  Because the sampling units were territories, 
we developed an ArcView III extension to randomly sample areas outside of 
territories (e.g. null-territories).  Inverse distance weighted surfaces for 
percent reed canary grass cover, index of reed canary grass dominance, 
vegetation height density, percent cover of forbs, percent cover of shrubs, and 
average litter depth were estimated in ArcMap 8.1.  Ten a priori logistic 
regression models of associations of vegetation variables with Common 
Yellowthroat and Sedge Wren territory presence/absence were averaged to address 
model selection issues.  The averaged models revealed that for Common 
Yellowthroats amount of shrub was positively associated with territory 
placement.  For Sedge Wrens percent cover of reed canary grass was positively 
associated with territory presence.  For Common Yellowthroats, model averaged 
weights indicated that shrub cover, vegetation height density, and average 
litter depth were more important than reed canary grass cover, reed canary grass 
dominance, and percent forb cover.  However, for Sedge Wrens, model averaged 
weights indicated that none of the other variables approached the importance of 
reed canary grass percent cover in the suite of models.  Thus, Common 
Yellowthroats do not seem to be affected by reed canary grass presence and 
dominance, whereas Sedge Wrens actually show a slight affinity for reed canary 
grass in the study area.

Keywords: breeding birds, habitat use, Phalaris arundinacea, reed canary grass, 
wet meadows
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"Cascade du Chaudron","sm/sm1881/20800","20896","013.gif","13","13","","013.tif"
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"Cascade du Chaudron","sm/sm1881/20800","20896","015.gif","15","15","","015.tif"
"Cascade du Chaudron","sm/sm1881/20800","20896","016.gif","16","16","","016.tif"
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1;
From: Max Rottersman [maxrottersman@yahoo.com]
Sent: Tuesday, August 20, 2002 8:34 PM
To: rule-comments@sec.gov
Subject: S7-21-02

Hello,

I believe that officers of investment companies should be required to sign
off on NSAR filings.  These are well-thought out, but it appears seldom
used, filings that the SEC requires.  Because few Investment companies take
these filings seriously there are many errors and missing data.  Even in
N-30Ds I have recently found that the following funds were late in their
filings (past the 60 day mark)

Eaton Vance Emerging Markets Fund
Liberty Fund
Morgan Stanley Tax-Free Income
Alliance Muni Funds

The investment management companies have grown complacent and are ripe for
fraud and abuse.  The Sarbanes Oxley Act of 2002 is a perfect opportunity to
make sure the mutual fund industry keeps its hard-earned reputation.

Sincerely,
Max Rottersman
www.FundDocs.com
212-254-3232
%  Compute finite difference approximation to solution of ODE BVP
%      -d^2u/dx^2 = f(x), 0 < x < 1,
%       u(0) = 1,
%       u(1) = 0.
%  Test the code by taking f(x) = 9*pi^2/4 * cos(3*pi*x/2), with  
%  exact solution u_exact = cos(3*pi*x/2).
%
%    Approximate solutions are computed on a sequence of grids.
%  For each grid the solution error is computed. A log-log
%  plot of solution error vs. grid spacing is generated.

  nlevels = input(' No. of grid levels = ');
  nvec = zeros(nlevels,1);
  for k = 1:nlevels
    N = 2 * 2^k - 1        %  No. of unknowns = no. of interior grid points.
    nvec(k) = N;           %  Save no. of unknowns.
    h = 1/(N+1)            %  Grid spacing.
    x = [0:h:1]';          %  Grid points, including boundary.
    x_interior = x(2:N+1); %  Interior grid points.
  
%  Set up N-by-N matrix A_h = tridiag(-1,2,-1). Use sparse
%  storage mode.  First set up main diagonal and subdiagonal of A_h.
%  Since A_h is symmetric, the sub- and superdiagonals are the same.
  
    Ah_diag = 2 * ones(N,1);
    Ah_sub = -1 * ones(N-1,1);
    A_h = spdiags([[Ah_sub;0],Ah_diag,[0;Ah_sub]],[-1 0 1],N,N);

%  Set up right-hand-side vector b_h. First evaluate r.h.s function f(x)
%  at interior grid points. Then add contribution from boundary conditions.

    rhs_function = WHAT IS IT?
    u_left = 1;   %  Left BC
    u_right = 0;  %  Right BC
    b_h = h^2 * rhs_function;
    b_h(1) = WHAT IS IT?
    b_h(N) = WHAT IS IT?
    
%  Solve linear system A_h*uh_interior = b_h and append boundary values. 
    
    uh_interior = A_h\b_h;
    uh = [u_left; uh_interior; u_right];
    
%  Evaluate exact solution and compute discrete solution error.

    u_exact = cos(3*pi*x/2);
    Eh = norm(uh - u_exact,'inf');
    
%  Save error and mesh spacing.
    
    Ehvec(k) = Eh;
    hvec(k) = h;

%  Plot true and approximate solutions in figure 1.

  figure(1)
      plot(x,u_exact,";exact solution;g*-", x,uh,";FDE solution;ro-")
      xlabel('x axis')
      ylabel('u(x)')
      title_str = ['Grid spacing h = ', num2str(h)];
      title(title_str)

      disp(' Hit any key to continue.'); 
      pause

  end

%  Plot error vector Eh vs. h on a log-log scale.

  figure(2)
    loglog(hvec,Ehvec,"bo-")
    xlabel('mesh size h')
    ylabel('E_h = max |u_h - u_{exact}|')
    title('Log-log plot of solution error E_h vs. mesh size h')
        
%  Estimate rate of convergence.

  conv_rate = mean( diff(log(Ehvec)) ./ diff(log(hvec)) );
  fprintf('Estimated rate of convergence is h^p, where p = %4.3e\n',conv_rate);
4G
THE DOCTOR.
in the habit of promoting gentility by eating a little at
home before they started.
My reasoning, however, had no other effect than to excite
a smile from the Doctor, and the very philosophic reply,
"that they should prefer to adhere to their own custom
until they got to the lady's house, when they would try to
conform to that of the white people of London." The
drollness of these remarks from this droll old gentleman
entirely prevented Mr. Melody and myself from intruding
any further suggestions, until the hour arrived, and it was
announced that the carriage was at the door.
FXUS61 KBUF 050630
AFDBUF

AREA FORECAST DISCUSSION 
NATIONAL WEATHER SERVICE BUFFALO NY
230 AM EDT SUN OCT 5 2003

KTYX RADAR SHOWING A BAND OF MODEST LAKE EFFECT ACROSS NORTHERN 
OSWEGO...SOUTHERN LEWIS AND SOUTHERN JEFFERSON COUNTIES. SPOTTER 
REPORTS INDICATING MOST OF THIS LAKE ACTIVITY IN THE FORM OF RAIN 
AND GRAUPEL SHOWERS. COLD AIR WILL CONTINUE TO DEEP OVER THE NEXT FEW 
HOURS AND WE WILL SOME OF THIS PRECIPITATION CHANGE OVER TO SNOW...
BUT ONLY FOR ELEVATIONS ABOVE 1500 FEET. ANY ACCUMULATION TOUGH TO 
PIN DOWN DUE TO UNCERTAINTY OF EXACT CHANGE OVER. ETA AND RUC 
SUGGESTING QPF UP TO A THIRD OF AN INCH...THEREFORE A 1 TO 3 INCH 
ACCUMULATION BY 15Z NOT OUT OF THE QUESTION.

KBUF RADAR SHOWING SCATTERED LAKE EFFECT ACTIVITY ALONG THE WESTERN 
SOUTHERN TIER. ETA AND RUC QPF MUCH LESS HERE...THEREFORE ANY HIGHER 
ELEVATION SNOW WILL BE LIMITED TO AN INCH OR LESS.

RUC/ETA/MM5 SUGGESTING LAKE EFFECT WILL DIMINISH BETWEEN 15Z AND 18Z 
TODAY...COMPLETELY END OFF LAKE ERIE. UPPER TROUGH WILL BEGIN TO LIFT 
OUT TODAY...SO DO NOT EXPECT AS MUCH DIURNAL CONVECTION AS WE 
HAVE SEEN PAST FEW DAYS.  

LOW LEVEL FLOW VEERING NORTHWEST TONIGHT AND 850 MB TEMPERATURES 
MARGINALLY COLD ENOUGH TO GENERATE SOME LAKE EFFECT. ROC AND SYR 
BUFKIT PROFILES SHOWING MODEST LAKE INDUCED CAPES WITH NO CAPPING... 
BUT LIMITING FACTORS WILL BE INCREASING DRY AIR AND INCREASING SHEAR.

A PATTERN CHANGE EXPECTED NEXT WEEK AS ZONAL FLOW DEVELOPS ALOFT AND 
HIGH PRESSURE AT THE SURFACE BUILDS INTO THE AREA. THIS PATTERN 
LOOKS LIKE IT WILL REMAIN FOR THE AREA INTO THE COMING WEEKEND
AND THIS SHOULD RESULT IN A DRY AND INCREASINGLY MILD WEATHER PERIOD 
FOR THE AREA AS 850 MB TEMPERATURES WARM ABOVE +5C BY MID WEEK. 

.BUF...NONE.

$$
(57)
- ' Le colon des Antilles surpasse de beaucoup celui
du levant en blancheur, en finesse  et en lon-
gueur (i).
LE   CACAOYER.
Le cacaoyer (Cacao theobroma Linni) est un
arbre de moyenne grandeur, indigne des Antil-
les et de l'Amrique. Les Aborignes de ces con-
tres faisaient un grand usage du chocolat ; leurs
vainqueurs adoptrent cet aliment qu'ils perfec-
tionnrent en y ajoutant une lgre quantit de
Vanille, pour en faciliter la digestion (2).
Linn a regard le chocolat comme un mets cli-
gne des dieux, en le qualifiant du nom pompeux de
theobroma.
Les Franais ne commencrent  s'occuper de
la culture du cacaoyer, qu'en 1664; ce fut le juif
Benjamin Dacosta qui l'introduisit aux Antilles.
Cette culture n'y prit de l'accroissement que vers
1684, parce que, jusqu'alors, le chocolat n'avait
pas t d'un grand usage en France.
(1)  D'Auberteuil, 1" vol. page 176. Abrg de Bryan Ed-
wards , page 316.
(2)  La vanille (vanilla) est une plante sarmenteuse, grim-
pante,  fleurs, de la classe des orchides, dont le fruit est une
gousse remplie de graines, ou espce d'amandes aromatiques,
digestives et stomachiques. Elle crot dans les forts d'Amrique
et, comme le lierre, s'accroche aux arbres qu'elle rencontre
Metadata
Antarctic Regional Seas
Week 0f 08 October 2001

**Note that the WMO egg code used in the Antarctic analysis has 
been restricted. No partials will be used and the stage of 
development will be limited to ice of land origin, old ice (7.), 
First year ice (6), Young ice (3), and New ice (1).

Amery Sea (30E-90E): IceEdge and northern edge of pack ice from
77E4 to 90E9, and fast ice along coast from 60E6 to 90E9 analyzed
using DMSP OLS f13.01281.1325. IceEdge and northern edge of pack
ice from 35E8 to 47E1 analyzed using DMSP OLS f13.01281.0718.
Remainder of edge and outer pack ice estimated using a
combination of SSM/I and Quikscat from 08 Oct, meteorology and
climatology.
Summary: 30% DMSP OLS, 70% Estimated.

Wilkesland (90E-150E): Entire area was estimated using a
combination of SSM/I and Quikscat from 08 Oct 2001,
meteorology and climatology.
Summary: 100% Estimated.

Ross Sea (150E-150W): All inner pack ice visible and portions of 
outer pack ice in the west/central Ross visible on OLS 282.0933Z, 
281.1818Z, 281.1635Z, 281.1548Z, 281.0947Z, 280.1831Z, 280.1648Z, 
280.1646Z, and 280.1000Z. Remainder of edge and outer pack ice 
estimated using a combination of SSM/I and Quikscat from 08 Oct 
2001, meteorology and climatology.  
Summary: 70% OLS, 30% Estimated.

Amundsen Sea (150W-90W): Most of the areas near the ice edge were 
analyzed using DMSP OLS f15.01281.1548Z, f15.01279.1618Z, f13.01281.1312Z,
and f13.01281.0947Z.  Areas near the coast and ice shelf were analyzed using
DMSP OLS f13.01281.0947Z and f15.01281.1548Z.  Most of the ice edge was
estimated using QUIKSCAT from 8 OCT 2001.

Summary: 50% DMSP OLS, 50% estimated.

Bellinghausen (90W-30W): Area 70-72S and 74-80W analyzed using
DMSP OLS 282.1534.  Area 61-65S and 36-43W analysed using DMSP 282.0933.
Areas between 75-77S 40-50W and 65-70S 50-60W analyzed using DMSP
279.0832. Remainder of area estimated using SSMI from 09 OCT 01. 
Summary: 25% DMSP OLS, 75% estimated.

Weddell Sea (30W-30E):  Small area of inner pack and small
portion of edge was analyzed using DMSP OLS f15.01283.0648Z,
and f15.01281.0718Z.  Remainder of area was estimated using
a combination of SSM/I and Quikscat from 08 Oct 2001,
meteorology and climatology.
Summary: 10% OLS, 90% Estimated.
From: Steve Burling [kj7yl@kendra.com]
Sent: Thursday, December 04, 2003 5:26 PM
To: voipforum
Subject: Materials Submitted to the VoIP Forum

Name:
 Steve Burling

E-mail:
 kj7yl@kendra.com

Organization:
 Private Citizen

Comments:
------------------------------------------------------------
I do not see any need to regulate Voice Over IP. I think the new technology spear heads free enterprise. The phone companies for year have had a strangle hold on consumers wallets, and have had a cash Cow for years.


Clearly if the Bells want to hold on to the market share than maybe the should improve thier Service be offering a competitive flat long distance of thier own.

Givin that technology gets cheaper every than it stands to reason that the prices should also go.

Also if the bells want to hold on to market share than maybe they should improve thier service and network quality.


My local phone line is so bad that I can not even get a reasonable internet connection. So why would I want to support old technology. I should be able to fire the Verzion and have a cheaper more reliable choice.

Regulation always seems to be about making money and not about helping consumers.

------------------------------------------------------------
EMBARGOED UNTIL:  10:00 a.m. CST Monday, January 15, 1996

PHOTO NO.: STSCI-PRC96-01a

HUBBLE'S DEEPEST-EVER VIEW OF THE UNIVERSE
UNVEILS MYRIAD GALAXIES  BACK TO THE BEGINNING 
OF TIME

Several hundred never before seen galaxies are visible in this
"deepest-ever" view of the universe,  called the Hubble Deep Field
(HDF), made with NASA's Hubble Space Telescope.  Besides the classical
spiral and elliptical shaped galaxies, there is a bewildering variety
of other galaxy shapes and colors that are important clues to
understanding the evolution of the universe. Some of the galaxies may
have formed less that one billion years after the Big Bang.

Representing a narrow "keyhole" view  all the way to the visible
horizon of the universe, the HDF image covers a speck of sky 1/30th the
diameter of the full Moon (about 25% of the entire HDF is shown here).
This is so narrow, just a few foreground stars in our Milky Way galaxy
are visible and are vastly outnumbered by the menagerie of far more
distant galaxies, some nearly as faint as 30th magnitude, or nearly
four billion times fainter than the limits of human vision.  (The
relatively bright object with diffraction spikes just left of center
may be a 20th magnitude star.) Though the field is  a very small sample
of sky area it is considered representative of the typical distribution
of galaxies in space because the universe, statistically, looks the
same in all directions.

The image was assembled from many separate exposures (342 frames total
were taken, 276 have been fully processed to date and used for this
picture) with the Wide Field and Planetary Camera 2 (WFPC2), for ten
consecutive days between December 18 to 28, 1995.  This picture is from
one of three wide-field CCD (Charged Coupled Device) detectors on the
WFPC2.

This "true-color" view was assembled from separate images were taken in
blue, red, and infrared light.  By combining these separate images into
a single color picture, astronomers will be able to infer -- at least
statistically -- the distance, age, and composition of galaxies in the
field.  Bluer objects contain young stars and/or are relatively close,
while redder objects contain older stellar populations and/or farther
away.

This material was presented to the 187th meeting of the American
Astronomical Society in San Antonio, Texas on January 15, 1996.

Credit: Robert Williams and the Hubble Deep Field Team (STScI) and NASA
Muon radiative energy loss (in 1.0E06 cm^2/g)
   in Rubber butyl (C%4#H8)%n#
   with Z/A =  0.57034
   (f12.0,4f12.4)
     E (GeV)      b_brem      b_pair      b_nucl     b_total
          2.      0.2231      0.0948      0.4818      0.7998
          5.      0.3030      0.2372      0.5090      1.0491
         10.      0.3698      0.3642      0.4929      1.2269
         20.      0.4410      0.5031      0.4694      1.4135
         50.      0.5390      0.6978      0.4438      1.6807
        100.      0.6136      0.8364      0.4312      1.8812
        200.      0.6835      0.9648      0.4248      2.0730
        500.      0.7676      1.0996      0.4237      2.2909
       1000.      0.8222      1.1831      0.4304      2.4358
       2000.      0.8679      1.2427      0.4421      2.5527
       5000.      0.9142      1.2958      0.4639      2.6740
      10000.      0.9393      1.3208      0.4860      2.7462
      20000.      0.9572      1.3366      0.5121      2.8060
      50000.      0.9729      1.3489      0.5530      2.8747
     100000.      0.9798      1.3540      0.5883      2.9220
SEXX03 KNEC 131530
EQRQED
 
U.S. DEPARTMENT OF THE INTERIOR                          NO. 5-347
GEOLOGICAL SURVEY                                     DEC 13, 2005
NEIC QUICK EPICENTER DETERMINATIONS
 
UTC TIME    LAT     LONG    DEP GS MAGS  SD STA  REGION--COMMENTS
HRMNSEC                         MB  Msz     USED
 
DEC 06
003713.5f 38.970N  21.080E  20               12 GREECE. <ATH>. MD
                                               3.4 (ATH).
011813.8s 40.615N 126.761W  10G 3.0     0.9  36 OFF CST N CALIF.
                                               ML 3.5 (GS).
025649.7f 43.055N   0.811W   2               14 PYRENEES. <LDG>.
                                               ML 2.6 (LDG).
040602.0f 38.160N  21.750E  23                6 GREECE. <ATH>. MD
                                               3.0 (ATH).
050147.4f 38.190N  22.590E   5               10 GREECE. <ATH>. ML
                                               2.7 (ATH).
054014.9s  2.471N  96.349E  61  5.0     0.7  20 SIMEULUE, IND.
055309.0   6.095S  29.524E  10G 5.4 4.8 0.6 100 LAKE TANGANYIKA
        REGION, CONGO-TANZANIA. Felt at Kalemie.
063924.1s 22.059S 179.642W 577? 4.4     0.7  30 SOUTH OF FIJI ISL
064723.2f 37.630N  20.890E   5                9 IONIAN SEA. <ATH>.
                                               MD 3.6 (ATH).
073705.1f 37.660N  20.890E  26                4 IONIAN SEA. <ATH>.
                                               MD 3.5 (ATH).
082829.0f 35.792N 120.346W  10               10 CEN CALIF. <NC>.
                                               ML 3.1 (NC).
084638.5  16.192N  95.528W  31D 4.5     0.8  40 OAXACA, MEXICO
084719.5s 18.611S 177.982W 597* 4.5     1.0  11 FIJI REGION
095516.4f 37.559N 118.868W   8               11 CEN CALIF. <NC>.
                                               ML 3.1 (NC).
100540.0s 36.567N  71.290E 105* 4.5     1.3  18 HINDU KUSH REGION,
                                               AFGHANISTAN
125938.7s  8.648S  79.504W  47D 5.0     0.9  25 NEAR COAST N PERU
162413.0f 38.440N  89.190W   5G              15 ILLINOIS. <CERI>.
                                               mbLg 2.7 (GS).
173825.0f 40.321N 124.599W  21                7 OFFSHORE NORTHERN
        CALIFORNIA. <NC>. MD 2.8 (NC).
golden co usa 2005 DEC 13 12:12
NASA Photo ID: STS006-06-456      File Name: 10061077.jpg
Film Type: 35mm CN                Date Taken: 04/09/83
Title: MS Peterson eats while reviewing procedures with Commander Weitz on middeck
Description:
Mission Specialist (MS) Peterson, holding food container, eats while
reviewing procedures with Commander Weitz (wearing bifocals) on middeck in
front of starboard wall.  Weitz points out an item in the frew activity
plan  (CAP) to Peterson as the mission specialist uses a spoon to eat a
meal aboard  the Earth-orbiting Challenger, Orbiter Vehicle (OV) 099.
Weitz and Peterson  are wearing the shirt and trouser portions of the light
blue cotton  multi-piece constant wear garments.
AWUS83 KFSD 081715
RWSSD 
SDZ001>074-090300-
WEATHER SUMMARY FOR SOUTH DAKOTA
NATIONAL WEATHER SERVICE SIOUX FALLS SD
1115 AM CST SUN FEB 8 2009
HIGH PRESSURE MOVED SOUTHEAST ACROSS SOUTH DAKOTA OVERNIGHT BRINGING 
MOSTLY CLEAR SKIES AND LIGHT WINDS. LOW LEVEL CLOUDS ACROSS THE 
SOUTHEAST AND CENTRAL DISSIPATED EARLY SATURDAY EVENING...AND  
SHORTLY BEFORE DAWN...HIGH LEVEL CLOUDINESS INCREASED OVER THE 
SOUTHWEST. 
OVERNIGHT LOW TEMPERATURES WERE IN THE UPPER TEENS AND LOWER 20S 
ACROSS THE SOUTH AND WEST...FROM 10 TO 15 DEGREES NORTH CENTRAL AND 
EAST CENTRAL...AND FROM 5 TO 10 DEGREES NORTHEAST AND NEAR 
BROOKINGS. AT 4 DEGREES...ABERDEEN AND WATERTOWN WERE THE COLDEST IN 
THE STATE. 
OVERNIGHT WINDS WERE MOSTLY LIGHT OR CALM BUT INCREASED FROM THE 
SOUTH AT 10 TO 20 MPH LATE NEAR PINE RIDGE AND FAITH.
AT 11 AM CST SKIES WERE MOSTLY CLOUDY OVER THE SOUTHWEST...AND SUNNY 
OVER THE REMAINDER OF THE RUSHMORE STATE. TEMPERATURES WERE IN THE 
20S NORTHEAST...THE LOWER AND MIDDLE 30S NORTHWEST THROUGH SOUTHEAST
...AND THE MIDDLE AND UPPER 30S SOUTHWEST AND SOUTH CENTRAL. 
EXTREMES WERE FROM 20 DEGREES AT WATERTOWN TO 43 DEGREES AT 
SPEARFISH. WINDS WERE SOUTHERLY ACROSS THE STATE AT 7 TO 14 MPH 
EXCEPT STRONGER...AROUND 20 MPH...AT RAPID CITY...FAITH AND PINE 
RIDGE. GUSTS NEAR 30 MPH WERE OCCURRING AT RAPID CITY.../28 MPH/ AND 
PINE RIDGE.../29 MPH/.
THIS DATE IN 1899 WAS BRUTALLY COLD WITH TEMPERATURES IN THE 30S 
BELOW ZERO ACROSS EASTERN AND MUCH OF CENTRAL SOUTH DAKOTA. LOW 
TEMPERATURES INCLUDE...
27 BELOW ZERO AT YANKTON
28 BELOW ZERO AT ALEXANDRIA AND TYNDALL
30 BELOW ZERO AT ACADEMY AND MITCHELL
31 BELOW ZERO AT ARMOUR
32 BELOW ZERO AT MILBANK
34 BELOW ZERO AT FLANDREAU...HURON...MIDLAND AND WENTWORTH
35 BELOW ZERO AT ABERDEEN...HIGHMORE...MELLETTE AND WATERTOWN
36 BELOW ZERO AT BROOKINGS AND KENNEBEC
37 BELOW ZERO AT IPSWICH
38 BELOW ZERO AT HOWARD...SIOUX FALLS AND WESSINGTON SPRINGS
40 BELOW ZERO AT FORESTBURG
42 BELOW ZERO AT GANN VALLEY
HIGH TEMPERATURES ACROSS THE NORTHEAST AND EAST CENTRAL WERE ONLY 20 
BELOW TO 25 BELOW ZERO.  
A TWO DAY SNOWSTORM BEGAN ON THIS DATE IN 1909 ACROSS SOUTHEAST 
SOUTH DAKOTA. STORM TOTALS INCLUDE...
21 INCHES AT SIOUX FALLS
18 INCHES AT CENTERVILLE AND MENNO
12 INCHES AT DE SMET...FORESTBURG AND VERMILLION
10.8 INCHES AT HURON
10 INCHES AT MITCHELL
9.5 INCHES AT WENTWORTH
7.5 INCHES AT MARION
6.1 INCHES AT WHITE LAKE
6 INCHES AT BROOKINGS AND YANKTON     
 
$$
SHEEHAN
Subject: FVAG01 SABM 202100
FVAG01 SABM 202100
VOLCANIC ASH ADVISORY
ISSUED: 2008 0620/2100Z
VAAC: BUENOS AIRES
VOLCANO: CHAITEN 1508-41
LOCATION: S42.50 W72.39
AREA: CHILE-S
SUMMIT ELEVATION: 962M
ADVISORY NUMBER: 2008/193
INFORMATION SOUR
OBS ASH DATE/TIME: 20/0739Z
OBS ASH CLOUD: VA CLD IDENTIFIABLE FROM GOES 12 ON IMAGE 1745Z.
?                          VA CLD OBS AT 1425Z TOP FL 150 MOV SE
FCST ASH CLD + 06HR: 210300 SFC/FL200 300 ? S4400 W07300 ? S4430
W07200 ? S4600 W07200
FL200/350 NO ASH EXP
FL350/550 NO ASH EXP
FCST ASH CLD + 18HR: 210800 SFC/FL200 S4530 W07000 ? S4430 W06900 ?
 S4200
W07100 ? S4230 W07300 ? S4400 W07230 ? S4430 W07100 ? S4530 W07100 ?
S4530 W07000
FL200/350 NO ASH EXP
FL350/550 NO ASH EXP
NEXT ADVISORY: 21/0300Z
REMARKS:  VA CLD IDENTIFIABLE ON GOES 12 IMAGERY.

.
AND   REPUBLIC   OF   HAYTI.                 [165
xviii. and assuring him he was without any feeling of
animosity or prejudice against France.*
Thus the long sufferings of the Haytians, the cru-
elties they had sustained from the French, all, all was
unable to make the slightest impression on Ption's
heart, he was without any feeling of animosity or preju-
dice* against a nation which had, not above twelve
years since, burned, hung, drowned and torn in pieces by
blood hounds, his brethren and his countrymen. The
commerce of 1789, slavery and the slave trade,
constituted, according to him, the welfare of both coun-
tries ; and he had at the same time Malouet's secret
instructions in his pocket; he knew the French cabinet
desired the re-establishment of slavery, and dared
even to avow it. I ask then every impartial observer
whether there can be any person more decidedly a
Frenchman, or more thoroughly a traitor, than this
Ption was ?
After this open consummation of his guilt in the
eyes of the people, and deceiving the generals and ma-
gistrates of the republic, he gave Dauxion Lavaysse his
secret instructions, in which he pointed out to the
French government the means to be adopted for the
subjugation of the Haytians, as we shall find in the
sequel. He rewarded his accomplice with some thou-
sand dollars, and sent him away in a Haytian schooner.
Was the crime pf high treason ever more glaring,
or more fully proved ? Was it ever attended with cir-
cumstances so abominable and disgraceful ?
From the arrival of Dauxion Lavaysse at Port-au-
Prince, to his first opening, one could see the thread of
this perfidious conspiracy which was to knit itself by
those combinations of words and those ambiguous modes
of expression by which our tyrants reckon upon de-
* Appendix B. No. 7, page xxix.
47$                            POUVOIRS DtS RECOLLETS
solo, dummod nullo modo attingat primum gradum, cum iis qui ab haeresi, vel infidelitate convertunturad fidem catho-licam et in prsedictis casibus proletn susceptam declarandi legitimam.
5 Dispensandi super impedimento criminis, neutro tamen conjugum machinante et restituendi jus petendi debitum amissum.
6 Dispensandi super impedimento publicae honestatis, justi-tiae, ex sponsalibus proveniente.
7 Dispensandi in impedimento cognationis spiritualis, prae-terquam inter levantem et levatum.
8 Hae ver matrimoniales dispensationes videlicet 4, 5, 6 et 7, non concedantur nisi cum clausul, dummod mulier rapta non fuerit, et si rapta fuerit, in potestate raptoris non existt, neque in utroque foro, ubi erunt episcopi, sed in foro conscientiae tantm et in illis expediendis, tnor hujus modi facultatum inferantur cum expressione temporis ad quod fuerint concessae.
90 Dispensandi cum gentilibus et infidelibus plures uxores habentibus ut post conversionem et baptismum, quam malue-rint in illis, si etiam fidelis fit, retinere possint, nisi prima voluerit converti.
io Absolvendi ab haeresi et apostasi  fide et  schismate quoscumque etiam ecclesiasticos, tam saeculares quam regu-lares, non tamen eos qui ex locis fuerint in quibus sanctum officium exercetur, nisi in locis missionum, in quibus impun grassantur, hreses deliquerint, nec illos qui judicialiter abju-raverint, nisi isti nati sint, ubi impun grassantur hreses et post judicialem abjurationem illc reversi in haaresim relapsi fuerint et has in foro conscientiae tantm.
:Product: 20000216events.txt
:Created: 2000 Feb 19 0302 UT
:Date: 2000 02 16
# Prepared by the U.S. Dept. of Commerce, NOAA, Space Environment Center.
# Please send comments and suggestions to sec@sec.noaa.gov 
#
# Missing data: ////
# Updated every 30 minutes.
#                            Edited Events for 2000 Feb 16
#
#Event    Begin    Max       End  Obs  Q  Type  Loc/Frq   Particulars       Reg#
#-------------------------------------------------------------------------------

2840 +     0040   ////      0041  LEA  C   RSP  030-08    III/2                 

2850       0243   0246      0250  LEA  3   FLA  N28W69    SF                    

2860       0317   ////      0318  LEA  C   RSP  030-05    III/1                 

2870       0534   0537      0547  LEA  3   FLA  N27W69    SF                    

3000       0556   ////      0556  CUL  C   RSP  18-70     III/1                 

3010       0605   0617      0629  GO8  5   XRA  1-8A      C1.7    2.0E-03       

2880       0719   ////      0719  SVI  C   RSP  035-08    V/1                   
2880 +     0719   ////      0720  LEA  C   RSP  030-08    III/3                 

2890 +     0842   0846      0907  SVI  3   FLA  S14W53    SF      ERU       8867
2890 +     0843   0848      0854  GO8  5   XRA  1-8A      C1.3    8.1E-04   8867

2900       1004   1008      1016  LEA  3   FLA  N27W69    SF                    

2910 +     1141   1145      1153  GO8  5   XRA  1-8A      C1.3    8.4E-04       
2910       1149   ////      1149  SVI  C   RSP  035-08    III/1                 
2910       1149   1149      1150       F   RBR  204       42                    

2920       1536   1536      1540  HOL  3   FLA  S22W04    SF                8869
2920       1536   1541      1554  GO8  5   XRA  1-8A      C1.3    1.3E-03   8869

2930       1609   1613      1619  HOL  3   FLA  S24W55    SF                8868

2940       1721   1724      1728  GO8  5   XRA  1-8A      C1.0    3.6E-04   8867
2940       1723   1724      1729  HOL  3   FLA  S15W58    SF                8867

2950       1830   1833      1848  G10  5   XRA  1-8A      B9.2    9.3E-04   8869
2950       1831   1831      1840  HOL  3   FLA  S25W03    SF                8869

2960 +     1924   1924      1925  SAG  G   RBR  245       430                   
2960 +     1924   ////      1925  SAG  C   RSP  030-08    III/3                 

2970 +     1926   1929      1931  GO8  5   XRA  1-8A      B9.0    2.2E-04       

2980 +     2024   2032      2038  GO8  5   XRA  1-8A      C2.4    1.7E-03   8867
2980       2030   2035      2038  HOL  3   FLA  S17W62    SF      ERU       8867

3020       2128   ////      2129  CUL  C   RSP  30-160    III/1                 

2990 +     2132   2139      2158  GO8  5   XRA  1-8A      C1.8    2.2E-03       
2990 +     2134   ////      2136  CUL  C   RSP  20-160    III/2                 

3030       2224   ////      2224  CUL  C   RSP  45-90     III/1                 

3040       2343   ////      2346  CUL  C   RSP  35-160    III/1
title "S. cerevisiae ORC";

default out-of-range reduce-range;
default numbering piece;

(* 
Celniker1984 Fig 1 says go to their ref40 or 2
the entire YRp7 is in U03501
JOURNAL   Proc. Natl. Acad. Sci. U.S.A. 76, 1035-1039 (1979)
*)
organism C.vector;
chromosome C.vector;
name "ARS1";    piece U03501; get from 601 -100 to 601 +100;

organism S.cerevisiae; chromosome S.cerevisiae;

(*
K01600
IS
  AUTHORS   Kearsey,S.
  TITLE     Structural requirements for the function of a yeast chromosomal
            replicator
  JOURNAL   Cell 37, 299-307 (1984)
*)
name "HO ARS";  piece K01600; get from 55 -100 to 55 +100;

(*
  AUTHORS   Bouton,A.H. and Smith,M.M.
  TITLE     Fine-structure analysis of the DNA sequence requirements for
            autonomous replication of Saccharomyces cerevisiae plasmids
  JOURNAL   Mol. Cell. Biol. 6, 2354-2363 (1986)
*)
name "H4 ARS";  piece M13626; get from 29 -100 to 29 +100;

(*
X04219
X04221
X04222
X04220
*)
name "ARS307a";  piece X04219; get from 183 +100 to 183 -100;
name "ARS307b";  piece X04220; get from 330 -100 to 330 +100;

(*
  AUTHORS   Walker,S.S., Francesconi,S.C. and Eisenberg,S.
  TITLE     A DNA replication enhancer in Saccharomyces cerevisiae
  JOURNAL   Proc. Natl. Acad. Sci. U.S.A. 87, 4665-4669 (1990)
*)
name "ARS121";  piece M37752; get from 383 -100 to 383 +100;

(*
  AUTHORS   Brand,A.H., Micklem,G. and Nasmyth,K.
  TITLE     A yeast silencer contains sequences that can promote autonomous
            plasmid replication and transcriptional activation
  JOURNAL   Cell 51, 709-719 (1987)
*)
name "HMR E ARS";  piece M18069; get from 205 +100 to 205 -100;

(* Shirahige1993 *)
name "ARS601";  piece D13938; get from 533 +100 to 533 -100;
name "ARS602";  piece D13938; get from 287 -100 to 287 +100;
name "ARS603a"; piece D13937; get from 280 -100 to 280 +100;
name "ARS603b"; piece D13937; get from 290 +100 to 290 -100;
name "ARS604";  piece D13936; get from 127 -100 to 127 +100;
name "ARS605";  piece D13935; get from 192 -100 to 192 +100;
name "ARS606";  piece D13934; get from 321 -100 to 321 +100;
name "ARS607";  piece D13933; get from 362 -100 to 362 +100;
name "ARS608";  piece D13932; get from 239 -100 to 239 +100;
name "ARS609";  piece D13931; get from 340 -100 to 340 +100;

(*
  AUTHORS   Skryabin,K.G., Eldarov,M.A., Larionov,V.L., Bayev,A.A.,
            Klootwijk,J., de Regt,V.C., Veldman,G.M., Planta,R.J.,
            Georgiev,O.I. and Hadjiolov,A.A.
  TITLE     Structure and function of the nontranscribed spacer regions of
            yeast rDNA
  JOURNAL   Nucleic Acids Res. 12 (6), 2955-2968 (1984)
*)
name "rDNA ARS";  piece X00486; get from 1863 -100 to 1863 +100;

(*
name "z";  piece z; get from z -100 to z +100;
*)
FXUS66 KHNX 160501
AFDFAT

INTERIOR CENTRAL CALIFORNIA FORECAST DISCUSSION
NATIONAL WEATHER SERVICE HANFORD CA
950 PM PDT TUE JUL 15 2003

WEATHER PATTERN RELATIVELY SUBDUED TONIGHT...ALTHO THERE ARE
SOME MESOSCALE CHANGES IN THE MAKING WHICH WILL EVENTUALLY
LEAD TO A MORE INTERESTING PATTERN IN THE DAYS TO FOLLOW.

FIRSTLY...ONSHORE GRADIENTS ARE SOMEWHAT STRONGER THAN THEY
WERE 24 HRS AGO...AVERAGING CLOSE TO 7.0 MB BETWEEN SFO AND LAS.
HOWEVER...THE MARINE LAYER REMAINS QUITE SHALLOW THIS EVENING...
LESS THAN 1K FEET DEEP ACCORDING TO THE FORT ORD PROFILER AND
ONLY ABOUT 550 FT DEEP AS OBSERVED BY THE 00Z OAK SOUNDING.
NONETHELESS...A MARINE PUSH HAS OCCURED ACROSS THE SACRAMENTO
VALLEY AND NORTHERN SJ VLY. IN THIS REGION...TEMPS AND DEWPOINTS
ARE SEVERAL DEGREES LOWER THAN MONDAY EVENING. WHILE ONSHORE
GRADIENTS SUPPORT A NW BREEZE IN THE CENTRAL AND SOUTHERN SJ VLY 
TONIGHT...THE MARINE LAYER IS FAR TOO SHALLOW ALONG THE COAST
TO SUPPORT ANY COOLING THIS FAR SOUTH. IN THAT RESPECT...MAX
TEMPS LOOK ON TRACK FOR WED...AND THIS IS SUPPORTED BY MOS
GUIDANCE. IF ANYTHING...THE 00Z RUN OF THE MESO ETA CONTINUES
TO NUDGE MAX TEMPS UPWARD A DEGREE OR TWO EACH OF THE NEXT TWO
DAYS...BUT THIS PARTICULAR MODEL HAS BEEN OVERZEALOUS WITH TEMPS
LATELY. 

MORE IMPORTANTLY...THE BROADER PICTURE IS CHANGING ACROSS THE
WEST. THE FIRST HINTS OF CHANGE BECAME EVIDENT OVER THE HIGH
SIERRA THIS AFTN WITH THE PRESENCE OF HIGH BASED CU. THIS IS 
THE INITIAL INDICATION THAT THE DOOR TO MONSOONAL MOISTURE IS
BEGINNING TO OPEN. THAT DOOR WILL OPEN WIDER DURING THE NEXT 48
HRS AS THE CENTER OF THE UPPER LEVEL RIDGE SHIFTS EAST OF THE
ROCKIES AND WIND CURRENTS ALOFT STEER TROPICAL MOISTURE IN THIS
DIRECTION. SURELY...CU DEVELOPMENT OVER THE HIGH SIERRA WILL BE
MORE PRONOUNCED THE NEXT COUPLE OF AFTNS. THE QUESTION IS WHEN
THE INVERSION CAP WILL BREAK. THE 00Z RUN OF THE GFS HINTS THAT
IT COULD BE AS EARLY AS TOMORROW AFTN NEAR THE CREST OF THE
SIERRA FROM TULARE CO SOUTHWARD. THIS MODEL FORECASTS 700-500 MB
REL HUM TO INCREASE TO ABOUT 60% WITH THETA E TEMPS AROUND 336 K.
HOWEVER...RELATIVE HUMIDITIES ARE COMPARITIVELY LOWER WITH THE
00Z MESO-ETA...EVEN THO 850 MB DEWPOINTS ARE FORECAST TO RISE
TO NEAR 8 C. BY THU PM...BOTH MODELS POSITION THE THETA E RIDGE
ALONG THE SPINE OF THE SOUTHERN SIERNEV WITH FURTHER INCREASE
IN MID TO HIGH LEVEL REL HUM. HENCE...ISOLD...HIGH BASED TSTMS WITH
DRY LIGHTNING SEEM A GOOD POSSIBILITY BY THEN. WITH THE ARRIVAL
OF RICHER TROPICAL MOISTURE FRIDAY THRU SATURDAY...ISOLD TSTMS
BECOME A POSSIBILITY AT LOWER ELEVATIONS OF THE SRN SIERNEV...
AND NOT EXCLUSIVE TO JUST THE DAYLIGHT HOURS.  FINALLY...IF YOU 
THOUGHT OUR SJ VLY HEAT HAS BEEN PATHETIC LATELY...THERE WILL
BE ADDED DISCOMFORT TO OUR PATTERN LATER IN THE WEEK. BY FRIDAY...
THE ARRIVAL OF MONSOONAL MOISTURE COULD SEND DEWPOINTS IN SOME
SJ VLY LOCALES CLOSE TO THE 70 DEGREE MARK...ESPECIALLY IN THE
SOUTH VALLEY.    

.HNX...NONE.

$$
DURFEE
ZCZC NFDSPENES ALL
SPENES
.
SATELLITE PRECIPITATION ESTIMATES..DATE/TIME 07/01/07 2255Z
SATELLITE ANALYSIS BRANCH/NESDIS---NPPU---TEL.301-763-8678
LATEST DATA USED: GOES-12 2245Z  RUMINSKI
.
LOCATION...TEXAS...OKLAHOMA...
.
ATTN WFOS...TSA...FWD...OUN...
ATTN RFCS...ABRFC...WGRFC...
.
EVENT...INCREASING CONVECTION OVER SOUTHEAST OKLAHOMA AND ADJOINING
AREAS OF TEXAS
.
SATELLITE ANALYSIS AND TRENDS...CNVTN IS BECOMING MORE NUMEROUS AND
ORGANIZED ACRS MUCH OF SE OK AND SPILLING OVER INTO N TX. CYCLONIC LO
LEVEL CIRC IS PRODUCING BROAD AREA OF LOW LEVEL MOISTURE CONV WHICH
THE CNVTN IS LINED UP WELL WITH. MID/UPR LEVEL VORT IS ALSO SEEN IN
IMAGERY JUST E OF KJCT AND IS AIDING CNVTV DEVELOPMENT. BASED ON SATELLITE
DEPICTION AND EARLIER OBSERVED RAINFALL EXPECT GENERAL 1.0-1.5" HRLY AMNTS
WITH LOCALLY HIGHER AMNTS UP TO 2" UNDER THE CORES OF MERGERS. LARGEST
CLUSTER OF CELLS APPEARS TO BE ARND BRYAN..MARSHALL..ATOKA AND JOHNSTON
COUNTIES IN OK ATTM. EXPECT THIS CNVTN TO GRDLY WORK ITS WAY INTO THE
REST OF SE OK AND EXTRM NE TX THRU THE EVE. SOME CONCERN THAT EARLIER
CNVTN IN THIS AREA MAY HAVE STABILIZED ATMOS AND SUPPRESS CNVTN FROM
MVG IN BUT FEEL THAT THE SUPPORT NOTED ABV WILL BE SUFFICIENT TO SUSTAIN
CNVTN THIS AREA.
.
SEE NCEP HPC DISCUSSION AND QPF/S FOR FORECAST.
....NESDIS IS A MEMBER OF 12 PLANET....
.
SSD/SAB WEB ADDRESS FOR PRECIP ESTIMATES:
HTTP://WWW.SSD.NOAA.GOV/PS/PCPN/
...ALL LOWER CASE EXCEPT /PS/PCPN/
.
LAT...LON 3641 9610 3548 9455 3298 9673 3437 9818
.
NNNN
TITLE
Field Study Results for VOCs with the Perkin-Elmer Sequential Tube
Sampler


AUTHOR(S)
Maribel Colon and William A. McClenny, Keith G. Kronmiller,
Christopher R. Fortune, and E. Hunter Daughtrey, Jr.

PERFORMING ORGANIZATION NAME AND ADDRESS
National Exposure Research Laboratory
Office of Research and Development
U.S. Environmental Protection Agency
Research Triangle Park, NC 27711

ManTech Environmental Technology, Inc.
2 Triangle Drive
Research Triangle Park, NC 27711

SPONSORING AGENCY NAME AND ADDRESS
National Exposure Research Laboratory
Office of Research and Development
U.S. Environmental Protection Agency
Research Triangle Park, NC 27711

ABSTRACT
Two Perkin-Elmer Sequential Tube Samplers (Model STS-25) were
evaluated for their performance, portability, and convenience of
operation.  Results obtained from both samplers and from a
collocated Summa-polished stainless steel canister were compared
for seven 3-h periods at three sites.  Special attention was given
to the monitoring of carbonyl sulfide and carbon disulfide.  The
samplers were loaded with three sampling tubes, each one packed
with 70 mg of Carboxen 1000 (60/80 mesh) and 160 mg of Carbotrap
graphitized carbon black (20/40 mesh).  An identical tube was used
as a field blank.  Each tube collected 1200 cm3 of ambient air (20
cm3/min for 60 min).  At the end of each sampling period, tubes
were sealed and stored in a capped glass tube to prevent
contamination and for transportation to a mobile laboratory for
analysis.  Advantages for the use of the STS-25 are low cost,
portability, ease of use, and a design suitable for obtaining sub-
part-per-billion detection limits with a standard analytical
finish.  Disadvantages are that it is a *one-short* technique and
no universal solid adsorbent material exists.
<< GX06101 >>

(Rev, &~11 Suer~O~ne ~o T~tiiy~sforw Gc~ni Jwy
	FOR TIlE	DL$TRICT OF	COLU~IBTA

TO:	Office of the Vice President
The White Rouse
	1600 Pennsylvania Avenue, Ig.w.	SUBPOENA TO TESTiFY
	ATTN~ Mr. David Addington	BEFORIE
		     GRAND JURY
Counsel to the Vice President
	51JBPOENA FOR:
	EPERSON	DOCUMENTIS) OF~ OBJECTr3~

	YOU ARE HEREBY COMMANOED to app~ar and testily before the (~and Jury of tt~e United States District C&.~rr at
the place, date, and time specified below,
		Cr~URT~OOM-
	ZTnlted States District. ~ourtho~u.se	 Grand Jury 03-3
	r	________________
	3	an.ci Co~stit~tion Avexiu~  NW
	WasLttigton.~ . DC 20001	January 30~ 2004

	YOU AREALSO COMMANOED to bring with you the following docurnentf si or object(sh

1.	Any and all records of telephone calls made to and from Air Force Two onJuly 12, 2003.

2.	Any and all records of telephone calls made to and from the government vehicles in
which members of the. staff of. the Office of the Vice President traveled from Andrews
Air Force Base on. July 12, 2003.
	GOVERNMENT
EXHIBIT
	1611
	O Pfeeae se~ addlfzoaai Intojvnarjan an revers&	(ID)
I

This subpoena a  n in elfect until you are granted 1ea~e to depart by the court or by an office acting on
 benaif of the ecu	i.3~tT I~O
u.s MAG71~AT)!	ecU	DAre
Nancy&t. ~r-W4	_______
	-~ .	January 22, 2004
		           A?dO ~1ONC NUh45E3~3 OFASS;5ThNTu2.ATZtrnNEY
This auripoen ~	p	R5naldRoos
af.tIie United ~	Deputy Special Counsel
	U.S. Department of Justice
	Washington, D.C. 20005