BEE-spoke-data/govdocs1-by-extension huggingface dataset:
177 
vous allez sont plus grands que les maux imaginaires que vous
fuyez ? Risquerez-vous de commettre une si dplorable erreur?
Tout le monde se dclare satisfait de l'Union, si les droits
constitutionnels y sont maintenus. Est-il vrai ds lors qu'aucun
des droits nettement crits dans la constitution ait t ni? Je
ne le pense pas. L'esprit humain est heureusement constitu de
telle sorte, qu'aucun parti n'aurait assez d'audace pour le faire.
Rappelez-vous, si vous le pouvez, un seul cas dans lequel
une clause clairement crite dans la constitution ait t nie?
Si par la simple force numrique, une majorit privait une mi-
norit quelconque d'aucun des droits constitutionnels franche-
ment tablis, cela pourrait,  un point de vue moral, justifier
la rvolution, et cela la justifierait pleinement s'il s'agissait
d'un droit vital. Mais tel n'est pas le cas.
Tous les droits vitaux des minorits et des individus leur
sont $i pleinement assurs par des affirmations et des ngations,
par des garanties et des prohibitions dans la constitution, qu'il
ne s'lve jamais de controverse  ce sujet. Mais aucune loi or-
ganique ne peut tre faite avec une provision spcialement ap-
plicable  chaque question qui surgit dans l'administration pra-
tique. Aucune prvoyance n'empchera cela, aucun document
de longueur convenable ne contiendra des clauses spciales 
toutes les questions possibles.
Les fugitifs du travail servile seront-ils rendus par les auto-
rits nationales ou par les autorits d'Etal? La constitution ne
le dit pas. Le congrs doit-il protger l'esclavage dans les ter-
ritoires? La constitution ne le dit pas expressment. De ces
sortes de questions sont nes toutes nos controverses constitu-
tionnelles, et elles nous divisent en majorit et en minorit.
Si la minorit ne se rend pas, la majorit doit le faire ou le
gouvernement cesser d'exister, U n'y a pas d'alternative pour
qu'il continue  vivre, sinon la soumission d'un ct ou de
l'autre. Si une minorit en pareil cas se spare plutt que de
se soumettre, elle tablit un prcdent qui la ruinera et la divi-
12
Hello, I'm new to the list. In response to Daphne, I used the ALE Wiki to identify leads to recent research on my dissertation topic, which is the persistence and transfer rates of low-income women students/learners across the trajectories of adult education and literacy and community college programs. 
On that same note, I thought members of the list might have some suggestions for me (based on my topic). I'm looking for very recent (2004-2006) literature, and I've already included some of the well-known reports listed on the NCSALL website (e.g. Comings, Soricone, Beder, Reder, etc.). 
What I really need are "cases" that address the question: Why are low-income women's rates of persistence and transfer across the trajectories of adult education and literacy and community college programs so low? At a less institutional and more social psychological level, the issue is sometimes framed as one of educational (and occupational) aspirations and expectations and/or one of motivation and achievement, which is of course relevant and the point at which I actually began my inquiry into the topic. However, this dissertation is for the Ph.D. in sociology, so a more institutional and/or policy-oriented approach is being taken. 
I've come across the literature that identifies the big "risk factors," but much of this is quantitative analysis of nationally representative data sets, and although an important contribution to my own investigation, my research will be qualitative because I'm interested in the relationship between these factors and in how they organize to influence or shape the (often poor) educational outcomes of women learners, particularly in terms of their longer-range ability to access occupational opportunity structures. So other very recent studies that investigate this or similar issues using qualitative methodologies is what I need. And I'm particularly interested in studies that address the implications of gender, age, race/ethnicity, class, and location (or place) in rates of persistence an transfer. 
For example, being a single parent is a risk factor to stopping out or dropping out, but being a single parent often means something very different to a man than to a woman (i.e. gender). Being an older student/learner (non-traditional in terms of age) means something very different to one who is a twenty-five year old mother than it does to one who is a forty-five year old grandmother . . . etc.
Finally, in addition to any "tips" on studies/research I might want to consider, I invite any suggestions or comments about my topic, approach . . . whatever anyone might share with a graduate student who is struggling to frame a dissertation proposal in the area of adult education and literacy, given the interests I've described and the sociological perspective I'm using.  
Thank you. --Ditmar
C. Ditmar Coffield
Northeastern University
Subject: NOAA-18, SBUV/2, Calibration Update,
Topic:
Change to Operational NOAA-18 SBUV/2 calibration

Satellite(s) Involved:
NOAA-18

Instrument(s) Involved:
SBUV/2

Product(s) Involved/Affected:
Total and Profile Ozone distributed via daily and orbital Product Master 
File (PMF) in Binary and BUFR format

Date/Time(UTC) of Initial Implementation:
4 March, 2006, Time ~1500 UTC

Contact Person(s) Name/Email/Phone Number for Questions:
Donna.McNamara@noaa.gov 301-763-8142 ext. 145

Web site(s) that contain other relevant information (where applicable):
http://www.osdpd.noaa.gov/PSB/OZONE/OZONE.html

Details/Specifics of Change:
This message is to notify users of an update to NOAA-18 calibration.  
This is the follow-on calibration change initially mentioned in the Mar 
15 notification message regarding a calibration table change for 
NOAA-18.  All available calibration changes have now been updated in 
operations.  NASA contract scientists, who provide our calibration 
updates report "While we have applied our best efforts to creating the 
updated NOAA-18 calibration, there are still some significant 
differences between SSAI test processing results at the Equator and 
concurrent ozone data from NOAA-16 and NOAA-17.  The NOAA-18 profile 
ozone values are significantly lower at layer 5 and above, with 
differences reaching 15-20% at 1 hPa.  NOAA-18 best total ozone values 
are approximately 3-5 DU lower than NOAA-16 data, and approximately 6-8 
DU lower than NOAA-17 data.  We are working to understand the origin of 
the inconsistencies between NOAA-18 calibration data and results from 
other SBUV/2 instruments, and will notify you if we develop an improved 
calibration."  Layer 5 is 32 MB and above.   On a positive note, we have 
noticed in our testing that this change increases total ozone at the 
very highest latitude, bringing it more closely in line with NOAA-16 and 
NOAA-17. 

-- 
Donna P. McNamara
Physical Scientist
NOAA/NESDIS/OSDPD/SSD/PIB
5200 Auth Rd., Rm 510 
Camp Springs MD 20746
Phone: (301)763-8142x145
Fax: (301)899-9196
364                    PAPERS RELATING TO THE
The Artois battalion, which is at Louisburg, amounts to 547 men, including the recruits arrived from France, who are at  tached to it whilst waiting for instructions from Court on this subject.
That of Burgundy numbers 543, including the recruits.
M. Delpriel, Sub-Lieutenant of Grenadiers in the Burgundy regiment, died at Louisburg on the 9lh of April, 1755.
Total of vacancies by death, three.
M.  DE MONTCALM  TO COUNT D'ARGENSON
Quebec, 21 May, 1756.
My Lord: Although I have reason to believe that this letter, which I am dispatching by way of Louisburg, will not reach you before the one I shall have the honor to write you from this place, at all events, I have the pleasure of informing you of my arrival on the 13lh. Le Heron is here since the 12th, and of the nine companies of the Regiment of Lasarre on board that vessel, only one man died on the passage; twenty-three were sick; of these, only one dangerously. I flatter myself that it will be the same on board the two other ships and the other two frigates which we may consider arrived, as le Leopard and la Sirenne are at anchor nine leagues below, and the remainder were at Bic island on the fifteenth. The first wind from the northeast will bring them all up. Our Staff, Engineers and troops are therefore all arrived. We have also four other ships in port, with stores and recruits on board, and a fifth is at anchor with our men of war. M. de Bourlamaque and N. De-8androiiins, Engineer, are already here, having come up by land from Cape Torment, as I likewise did. I heard from Chevalier de Levis the 15th. He was> at Bic island in very good health, awaiting a favorable wind.
The day following my arrival, I sent a courier to the Marquis de Vaudreuil, and to-morrow I proceed to join him. Everything is in movement for the opening of the campaign. The winter has been less severe than usual. I found it impossible to repair sooner to Montreal, as the rain had rendered the roads impassable, and the winds were contrary. The same reasons have retarded M. Doriel's arrival, who is coming to receive the troops, and with whom I expect to confer on the way. During my eight days' sojourn, I have taken information respecting a country and a war, in which everything is
<META Name="photo_id" Content="S69-40302">
<META Name="filename" Content="10075308.jpg">
<META Name="caption" Content="View of Mission Control Center celebrating conclusion of Apollo 11 mission">
<META Name="description" Content="Overall view of the Mission Operations Control Room in the Mission Control Center, bldg 30, Manned Spacecraft Center (MSC), at the conclusion of the Apollo 11 lunar landing mission. The television monitor shows President Richard M. Nixon greeting the Apollo 11 astronauts aboard the U.S.S. Hornet in the Pacific recovery area (40301); NASA and MSC officials join the flight controllers in celebrating the conclusion of the Apollo 11 mission. From left foreground Dr. Maxime A. Faget, MSC Director of Engineering and Development; George S. Trimble, MSC Deputy Director; Dr. Christopher C. Kraft Jr., MSC Director fo Flight Operations; Julian Scheer (in back), Assistant Adminstrator, Offic of Public Affairs, NASA HQ.; George M. Low, Manager, Apollo Spacecraft Program, MSC; Dr. Robert R. Gilruth, MSC Director; and Charles W. Mathews, Deputy Associate Administrator, Office of Manned Space Flight, NASA HQ (40302).">
Keywords">
">
<META Name="credit" Content="Image and text courtesy of Johnson Space Center">
<META Name="order_info" Content="JSC Office of Public Affairs<br>External Affairs Branch<br>Mail Code AP4<br>2101 NASA Road 1<br>Houston, TX 77058<br>Fax: (713) 483-2000<br>">
*Pages 1--1 from  file://C:WINDOWSTEMPACTN1120.PDF*
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1
(CO-99-13) Population of Counties by Age Group:  April 1, 1990
  
Source:  Population Estimates Program, Population Division, U.S. Census Bureau, Washington, DC  20233
Contact:  Statistical Information Staff, Population Division, U.S. Census Bureau (301-457-2422)
          pop@census.gov (please include a phone number with email correspondence)
  
Internet Release Date:  August 30, 2000

Area Name                               Total      Ages     Ages     Ages     Ages     Ages     Ages     Ages     Ages     Ages
                                   Population       0-4     5-17    18-24    25-44    45-64      16+      21+      65+      85+
                                                                                                                               
    NEW HAMPSHIRE                     1109252     85786   193999   118499   386892   199552   857496   776479   124524    13075
Belknap County                          49216      3556     9093     3924    16290     9645    37886    34865     6708      672
Carroll County                          35410      2435     6089     2384    11574     7264    27695    25896     5664      549
Cheshire County                         70121      5005    12153     8913    21823    13049    54708    48359     9178      971
Coos County                             34828      2298     6294     2855    10407     7252    27210    24985     5722      635
Grafton County                          74929      5033    12224    11892    23352    13219    59409    51521     9209      974
Hillsborough County                    335838     27490    58986    34514   121519    58987   258066   235003    34342     3577
Merrimack County                       120240      9143    21302    11467    42323    21469    92773    84663    14536     1818
Rockingham County                      245845     20193    44000    22414    93123    43625   187906   172756    22490     2259
Strafford County                       104233      7787    16801    16885    34256    17464    82062    71124    11040     1041
Sullivan County                         38592      2846     7057     3251    12225     7578    29781    27307     5635      579
Modeling the ionosphere topside to plasmasphere electron density distribution
using ISIS and IMAGE/RPI satellite data

Bodo W. Reinisch, Patrick Nsumei, Xueqin Huang, and Dieter Bilitza


We represent the F layer topside Ne profile from hmF2 to the plasmasphere by an
a-Chapman like function with a Chapman scale height H(h) that varies
continuously with height. This profile function is called a vary-Chap function.
For given F2 peak values foF2 and hmF2, we find H(h) by fitting the vary-Chap
function to Ne(h) profiles measured by the ISIS topside sounders.  Our initial
results show that H(h) at the F2 peak is almost constant with height; a rapid
increase occurs ~300 to 900 km above hmF2, reflecting the O+ to light-ion
transition. A hyperbolic tangent function suitably represents this variation,
and allows the parameterization of the scale height function in terms of the
transition height hT, the scale height HT at hT, and the steepness of the
transition, b. We explore two different approaches to determine these
parameters. One is to find the vary-Chap functions that smoothly interpolates
between plasmasphere profiles and the F2 layer peak. Measurements by the Radio
Plasma Imager (RPI) on the IMAGE satellite provide plasmasphere profiles down to
~3000 km altitude [Reinisch et al., Plasma Density Distribution Along the
Magnetospheric Field: RPI Observations from IMAGE, Geophys. Res. Ltrs., 28, 24,
4521-4524, 2001]. For the F2 peak we use the IRI profiles [Bilitza, D.,
International Reference Ionosphere 2000, Radio Science 36, #2, 261-275, 2001].
The other approach makes a least-squares fit of vary-Chap functions to topside
profiles measured by the ISIS topside sounders [Huang et al., Electron Density
Profiles of the Topside Ionosphere, Annali di Geofisica, 45 (1), 125-130, 2002]. 

_______________
Spring Joint Assembly, American Geophysical Union, Baltimore, Maryland, U.S.A., 
23-26 May 2006
Tornado Protection: Selecting Refuge Areas in Buildings 

Chapter 1: Tornado Profile

The National Weather Service defines a tornado as a violently rotating column of air 
pendant from a thunderstorm cloud that touches the ground. 
From a local perspective, a tornado is the most destructive of all atmospheric-
generated phenomena. In an average year, a little more than 800 tornadoes hit various 
parts of the United States, though the number has varied from 500 
Determining Tornado Risk 
Detailed guidance for determining the magnitude of the tornado risk in a specific area 
of the United States is presented in FEMA publication 361, Design and Construction 
Guidance for Community Shelters (for more information, see the section of this booklet 
titled Information Sources).

Tornado Characteristics

The time of day when tornadoes are most likely to occur is the mid-after-noon, 
between 3:00 p.m. and 6:00 p.m. (Figure 1-3). Occasionally, severe tornadoes have 
been recorded in the early morning or late evening. 
The direction of movement is predominantly from the southwest to the northeast. 
However, tornadoes have been known to move in any direction along with the parent 
thunderstorms. 
The length of path averages 5 miles, but some tornado paths have exceeded 100 miles. 
The width of path averages 300 to 400 yards, but may reach up to 1 mile. 
The travel speed (translational) averages 25 to 40 miles per hour (mph), Figure 1-3 
Tornado occurrence by time of day. but speeds from 5 to 60 mph have been recorded. 
Rotation is generally counterclockwise in the northern hemisphere (Figure 1-6). About 
10 percent of tornadoes have been known to rotate clockwise. 
Wind speed is the sum of rotational speed and translational speed. The rotational speed 
decreases as the distance from the center of a tornado increases. With a 
counterclockwise rotation, the wind speed on the right side of the tornado is higher 
because the translational speed adds to the rotational speed. 
Because of the unpredictability of tornado paths and the destruction of commonly used 
instruments, direct measurements of wind speeds have not been made in tornadoes. 
Rather, wind speeds are judged from the intensity of damage to buildings. Engineering 
assessment of damage puts the maximum wind speed at 200 mph in most destructive 
tornadoes, and the speed is not likely to exceed 250 mph near ground level. 
Typical tornado rotation.
Janvier
-Riviere de
Sa Magde -
laine.
* Notez,
Ce fouv. t
eftre ce que
lesEffagmls
ont ai i iii
Rio efcan-
dido, Rivie-
re cache.
o Journal Hiftorique,
Beaujeu au retour de ces Mef-
fieurs , pour favoir au jufte le
lieu o nous eftions, Se la route
que nous devions tenir ; les uns
fotenant que nous eftions plus
avant que nous ne penfions, &
que les courans nous avoient fait
driver;les autres que nous tions
proche de la Riviere de la Mag-
delaine.
Le premier avis fut le plus fort,
d'o M. de la Sale jugea, refle-
xion faite ,'qu'il devoit avoir paf-
f fa Riviere; & il n'eftoit que
trop vray ; car comme ce Fleuve
fe jette dans la Mer par deux ca-
naux , il falloit que l'une de fes
embouchures paffaft par les ba-
tres que nous avions remarques
le fix du courant; d'autant plus
que * la hauteur de ces batres
que nous avions prife eftoit  peu
de chofe prs coforme  celle que
M.delaSale avoit remarque,lorf-
qucparle Canada il eftoit venu
reconnotre   l'embouchure   de
|STAGE-|-----IMPACT STATEMENT 
 32.0 - All areas along the Duck River near Centerville will be 
        covered by flood waters. Defeated Creek, Bears Creek, 
        Swan Creek, Lowes Bend, and Horse Branch Creek will be 
        flooded due to backwater. Many roads near the river 
        will be impassable due to high water 


 25.0 - Flood waters cover the soccer fields and bottomland 
        along the river. Hickman Springs Road, Defeated Creek 
        Road, and Leatherwood Road will be impassable. 
        Defeated Creek will flood due to backwater from the 
        Duck River 


 22.0 - Flood waters will cover the flood plain along the 
        river. Several roads near the river will be partilally 
        covered. In Centerville, Hickman Springs Road and 
        Defeated Creek Road will be affected. Leatherwood 
        Road between Shady Grove and Primm Springs near 
        Totty's Bend will also be affected 
 


 17.0 - Water begins to overflow the banks
36                              UN NAUFRAGE AU TEXAS
Aprs plusieurs jours de proccupation et de mditation sur
une question aussi singulire, voici l'explication  laquelle,
sauf meilleur avis, je crus devoir m'arrter :
Sur le Nuremberg les lits taient placs dans le sens de la
longueur du navire, les pieds tourns vers 1 avant et les ttes
vers l'arrire, dans le sens du tangage par consquent.
Sur I'Ariel, au Contraire, les lits sont placs paralllement 
la largeur, dans le sens du roulis, qui, alternativement alors,
abaisse et relve la tte et les pieds.
J'eus la pense d'examiner quels rapports pouvaient avoir
ces mouvements avec la forme, la position et la fonction de
l'estomac.
Cet organe, espce de sac conique assez semblable  celui
d'une cornemuse, est plac transversalement au-dessous du
ct gauche de la poitrine. Sa petite extrmit, rpondant an
creux de l'estomac (l'pigastre), a deux ouvertures contractiles,
une suprieure, nomme cardia, et une infrieure, nomme
pylore.
Ces ouvertures sont doues d'une extrme sensibilit : lors-
que les mouvements du navire i (tangage ou roulis) agissent
paralllement  la longueur du corps et, par consquent, trans-
versalement  celle de l'estomac, les aliments, qui sont conte-
nus dans cet organe, tant ballotts de haut en bas et de bas
en haut, frappent directement et alternativement les deux ou-
vertures dont je viens de parler. Ce choc direct cause un mal-
aise beaucoup plus grand que le simple froissement produit
par l'ondulation des aliments dans le sens transversal du corps
et paralllement  la longueur de l'estomac.
La contradiction entre les deux quipages du Nuremberg et
de VAriel, ainsi que nos observations tout opposes sur ces
deux navires, avaient donc une explication.
Si elle est juste, comme je crois l'avoir exactement constat,
elle doit avoir pour consquence le prcepte suivant : placer
toujours la longueur du corps en travers du mouvement le
plus proronc du navire, ou, en d'autres termes, placer tou-
jours le grand diamtre de l'estomac paralllement  ce plus
grand mouvement.
Quant  l'application du prcepte, il faut convenir qu'elle
n'est pas toujours facile, car le temps ne permet pas toujours
qu'on puisse aller s'tendre sur le pont; et les lits, placs
//////////////////////////////////////////////////////////////////////
TITLE:           GCN/SWIFT NOTICE
NOTICE_DATE:     Fri 26 Aug 05 06:19:14 UT
NOTICE_TYPE:     Swift-BAT GRB Position
TRIGGER_NUM:     152113,   Seg_Num: 0
GRB_RA:           87.729d {+05h 50m 55s} (J2000),
                  87.800d {+05h 51m 12s} (current),
                  87.101d {+05h 48m 24s} (1950)
GRB_DEC:          -2.680d {-02d 40' 46"} (J2000),
                  -2.679d {-02d 40' 42"} (current),
                  -2.692d {-02d 41' 31"} (1950)
GRB_ERROR:       4.00 [arcmin radius, statistical only]
GRB_INTEN:       30879 [cnts]    Image_Peak=533 [image_cnts]
TRIGGER_DUR:     8.192 [sec] 
TRIGGER_INDEX:   490     E_range: 25-100 keV
BKG_INTEN:       221667 [cnts]
BKG_TIME:        22600.00 SOD {06:16:40.00} UT
BKG_DUR:         64 [sec]
GRB_DATE:        13608 TJD;   238 DOY;   05/08/26
GRB_TIME:        22690.28 SOD {06:18:10.28} UT
GRB_PHI:          52.20 [deg]
GRB_THETA:        17.68 [deg]
SOLN_STATUS:     0x3
RATE_SIGNIF:     12.44 [sigma]
IMAGE_SIGNIF:    8.16 [sigma]
MERIT_PARAMS:     +1  +0  +0  +4  +2  +3  +0  +0 -36  +1 
SUN_POSTN:       155.06d {+10h 20m 14s}  +10.36d {+10d 21' 35"}
SUN_DIST:         68.20 [deg]
MOON_POSTN:       55.75d {+03h 43m 00s}  +23.39d {+23d 23' 42"}
MOON_DIST:        40.67 [deg]
MOON_ILLUM:      54 [%]
GAL_COORDS:      208.35,-14.68 [deg] galactic lon,lat of the burst (or transient)
ECL_COORDS:       87.47,-26.10 [deg] ecliptic lon,lat of the burst (or transient)
COMMENTS:        SWIFT-BAT GRB Coordinates.  
COMMENTS:        This is a rate trigger.  
COMMENTS:        A point_source was found.  
COMMENTS:        This does not match any source in the on-board catalog.  
COMMENTS:        This does not match any source in the ground catalog.  
COMMENTS:        This is a GRB.
FXUS64 KCRP 100114
AFDCRP

COASTAL BEND FORECAST DISCUSSION
NATIONAL WEATHER SERVICE CORPUS CHRISTI TX
815 PM CDT FRI MAY 9 2003

BREEZY/WINDY CONDITIONS WILL PERSIST INTO THE NIGHT AS LOW PRESSURE 
REMAINS OVR THE PLAINS W/ STRONG PGRAD ALONG THE TX COAST AND THE 
SCA IS VERIFYING IN SEVERAL LOCATIONS IN THE BAYS AND OFFSHORE. 
OVERALL EXPECT CONDITIONS SIMILAR TO THOSE THE PAST SEVERAL NIGHTS 
W/ LOWS IN THE MID-UPR 70S...LOW CLOUDS SPREADING NORTH AND 
WEST...AND WINDY/BREEZY ONSHORE FLOW PREVAILING BEYOND MIDNIGHT. 
CURRENT FORECASTS ARE ON TRACK AND THERE ARE NO MAJOR CHANGES 
PLANNED.

AFTN PRELIMS...
CRP BE 078/092 077/090 075 000
VCT BE 076/092 075/089 073 000
LRD BB 079/105 078/100 076 000

.CRP...SCA FOR THE BAYS AND COASTAL WATERS FROM BAFFIN BAY TO THE 
MATAGORDA SHIP CHANNEL OUT TO 60 NM.

88/MJG
January 19, 1965

Dr. P. N. Makela
Department of Serology and Bacteriology
University of Helsinki
Helsinki, Fin&add

Dear Helen:

Thank you for letting me see your manuscript.  It is of course a great pleasure
to see this story unfold, even if we have now redirected the research here
completely to the B. subtilis system.

1s there no indication that the expression of V is also conditioned by a
lysogenic conversion?

You probably know what has been going on here from papers in Genetics, J. Mol.
Biol. and PNAS.  When we can eventually get around to it, some reprints will
be mailed out too.  Gan has a very interesting project now, the association of
DNA synthesis with a complex of RNA, protein and DNA probably at the cell wall.   73

Since you were here I have become very much interested in the development of    qE
computers for biological research, since Stanford actually has one of the
vorld's leading facilities for computer research.  There are some complex ques-   ST
tions of strategy and it is rather slow getting this moving-what a paradox,      9
considering microsecond operational speeds!  So far the main efforts are       =e
rather mathematical and in chemistry rather than biol
interested let me know,and you will also see somethi t gy.  If you are especially   @
                                  In the January 1965 PNSS.

Ollie will be amused to lear  we also have a rather extensive prograrrl in genetic
demography, using the 2 x 10 f records of the U.S. 1960 census (5X sample).
Among other things we certainly will extract what we can on sequence of sexes.
So far we see nothiitggvery clearcut on, e.g., interval between children by sex
of previous child, but have much more to do.  Any suggestions (even if they may
seem obvious and of course most of the plan will be obvious) would be welcome.
`vfe have a rather unusual arrangeraent with the Census Bureau to be able to study
these data diredctfy

While you were here I was perhaps just in the transition between working mainly
with my own hands in the lab, and being responsible for a larger group.  The
former is much pleasanter in many way6, and it takes some time both to acquire
some efficiency in the second role and to subdue resentments about leaving the
first.  One advantage of computation is that (tn a sense) the machines can carry
on even while one is interrupted.  It takes a lot of thought, but this can be
applisd at any time or place.  Eventually we will be literally programming the
machines to execute our experiments; it will take a little longer before the
machines will be programming us.

Best wishes,

Joshua Lederberg
Professor of Genetics
WWAK72 PAFC 100019
NPWALU

URGENT - WEATHER MESSAGE
NATIONAL WEATHER SERVICE ANCHORAGE AK
419 PM ADT SUN SEP 9 2007

.A LOW SOUTH OF THE WESTERN ALEUTIANS WILL RAPIDLY INTENSIFY
TONIGHT AND CROSS THE CENTRAL ALEUTIANS INTO THE SOUTHERN BERING
SEA EARLY MONDAY MORNING. IT WILL THEN TRACK TO THE NORTHERN
BERING SEA LATE MONDAY. THE LOW WILL PUSH A VERY STRONG FRONT
ACROSS THE EASTERN ALEUTIANS LATE SUNDAY NIGHT THROUGH MONDAY
AFTERNOON...RESULTING IN A PERIOD OF STRONG SOUTHERLY WINDS.

AKZ185-101330-
/X.UPG.PAFC.HW.A.0014.070910T1200Z-070910T2200Z/
/X.NEW.PAFC.HW.W.0020.070910T1400Z-070910T2100Z/
EASTERN ALEUTIANS-
INCLUDING THE CITIES OF...UNALASKA...NIKOLSKI
419 PM ADT SUN SEP 9 2007

...HIGH WIND WARNING IN EFFECT FROM 6 AM TO 1 PM ADT MONDAY...

THE NATIONAL WEATHER SERVICE IN ANCHORAGE HAS ISSUED A HIGH WIND
WARNING...WHICH IS IN EFFECT FROM 6 AM TO 1 PM ADT MONDAY. THE
HIGH WIND WATCH IS NO LONGER IN EFFECT. 

SOUTHERLY WINDS WILL RAPIDLY INCREASE LATE TONIGHT AS A STRONG
FRONT APPROACHES. SOUTH WINDS OF 40 TO 55 MPH WITH GUSTS TO 75 MPH
CAN BE EXPECTED EARLY MONDAY MORNING THROUGH THE EARLY AFTERNOON HOURS.
WINDS WILL DIMINISH LATER MONDAY AFTERNOON AS THE FRONT MOVES PAST
AND WINDS SWITCH TO THE SOUTHWEST.

A HIGH WIND WARNING MEANS A HAZARDOUS HIGH WIND EVENT IS EXPECTED
OR OCCURRING. PEOPLE ARE URGED TO SECURE LOOSE OBJECTS THAT COULD
BE BLOWN AROUND OR DAMAGED BY THE WIND.

$$
000
WTNT41 KNHC 081440
TCDAT1
TROPICAL STORM FLORENCE DISCUSSION NUMBER  20
NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL   AL062006
1100 AM EDT FRI SEP 08 2006
 
THE CLOUD PATTERN REMAINS SHAPELESS WITH VERY ASYMMETRIC
CONVECTION...AND DVORAK T-NUMBERS REMAIN UNCHANGED AT 35 KNOTS. I
WAS TEMPTED TO LOWER THE INTENSITY BUT I WILL HOLD IT AT 45 KNOTS
FOR THE SAKE OF CONTINUITY AND BASED ON SEVERAL..BUT LESS RELIABLE
HI-RES QUIKSCAT WIND VECTORS ON THE EDGE OF THE SWATH.  FLORENCE
HAS REFUSED TO STRENGTHEN WHILE IN THE TROPICS...LIKE MOST THE
SYSTEMS SO FAR THIS YEAR. HOWEVER...THE CYCLONE HAS THE OPPORTUNITY
TO DO SO AS IT MOVES NORTHWESTWARD AND NORTHWARD AHEAD OF THE
APPROACHING TROUGH DURING THE NEXT 2 TO 3 DAYS...AND BEFORE THE
SHEAR INCREASES SIGNIFICANTLY. THEREAFTER...IT SHOULD BECOME AN
INTENSE EXTRATROPICAL SYSTEM. THE INTENSITY FORECAST FOR FLORENCE
SEEMS MORE UNCERTAIN THAN USUAL.
 
THE LOW-LEVEL CENTER IS DIFFICULT TO FIND...BUT THERE MUST BE ONE
GIVEN THE LARGE AND WELL DEFINED CIRCULATION OF THE STORM. THE
AVERAGE MOTION OF THE LARGE GYRE IS ESTIMATED AT 300/15. THERE HAS
BEEN NO CHANGE IN THE STEERING CURRENTS AND FLORENCE CONTINUES
MOVING AROUND THE SUBTROPICAL RIDGE. IT SHOULD REACH THE WESTERN
PERIPHERY OF THE RIDGE IN ABOUT 36 HOURS AND GRADUALLY TURN
NORTHWARD WITH A DECREASE IN FORWARD SPEED. THEREAFTER...IT SHOULD
BEGIN TO ACCELERATE AS IT INTERACTS WITH THE TROUGH. THE GUIDANCE
IS CLUSTERED THROUGH THE NEXT 3 DAYS. THEREAFTER...ALL MODELS SHOW
THE NORTHEASTWARD TURN BUT THEY VARY ON THE FORWARD SPEED.
 
DUE TO THE UNUSUALLY LARGE AREA OF TROPICAL STORM FORCE WINDS...THE
BERMUDA WEATHER SERVICE WILL LIKELY ISSUE WATCHES OR WARNINGS
LATER TODAY.
 
NOTE: LAST TWO VISIBLE SATELLITE IMAGES PRIOR TO SENDING THIS
ADVISORY SUGGESTS THAT THE CLOUD PATTERN IS A LITTLE BETTER
ORGANIZED AND THE CENTER APPEARS TO BE TUCKED INTO THE CONVECTION.
IF THIS TREND TOWARD ORGANIZATION CONTINUES...SCIENCE WILL HAVE
PREVAILED.
 
 
 
 
FORECAST POSITIONS AND MAX WINDS
 
INITIAL      08/1500Z 23.0N  59.1W    45 KT
 12HR VT     09/0000Z 23.8N  60.9W    50 KT
 24HR VT     09/1200Z 25.5N  63.2W    55 KT
 36HR VT     10/0000Z 27.0N  64.5W    65 KT
 48HR VT     10/1200Z 28.5N  65.0W    75 KT
 72HR VT     11/1200Z 33.0N  64.0W    85 KT
 96HR VT     12/1200Z 39.0N  60.0W    75 KT...EXTRATROPICAL
120HR VT     13/1200Z 48.0N  49.0W    65 KT...EXTRATROPICAL
 
$$
FORECASTER AVILA
Plin. Lib. S cap. (6.
Sn.ibo , Lib. il. p. 350. & 560.
Arm.  Lib. bil. Indic.
.1

i' 

Gai. e,ap..t 4. v. 5 *'- 7-
r84    MOEURS DES  SAUVAGES
>hie
lefqucls
aufli
la
ancienne, leiqueis etoient Mer Cafpienne. Pline les confond avec les adu-fiens, Strabon les diftingue, Se dit queles Cadu-fiens avoient prefqu autant de gens de pied que Jes Peuples de l'Ariane. Il n'y avoit pas au refte un fi grand loignement d;es Etats de ces deux Princes,, en les plaant dans le Pont en tirant vers j'Afie Mineure, de ceux de leurs deux autres Confederez.'jcar il eft rapport dans Arrien, que pendant qu'Alexandre traverfoit la Perfe, il lui vint des Ambaffadeurs des Nations , qui habi-toient vers le Pont-Euxin , par un chemin trs-court , de forte que ce Prince en fut trs -furpris. On peut ajouter que les Villes & hs Nations tant ambulantes dans ces premiers temps , on pourroit r'approcker encore plus facilement les Etats des deux autres Roys, fur-tout deceluy des Elamites, dont le pas n'toit pas fi loign , ni fi tendu qu'il le fut depuis. On ne peut nier que les Elamites, oues Perfes, jtifquesau temps de Cy-rus., n'aient vcu  la faon des Sauvages , ain.fi que je l'ay prouv par Hrodote.
>Cette Guerre dont parle l'Ecriture,.n'toit pas dans un fe-ns fi petite qu'on veut la faire -y car quoique Iqs Rois de la Pencapole fuffent voifins, la Guerre ne laiffoit pas 4'embraier une grande tendue de pas -, ce qui parot manifeftement par la fainte Ecriture mme j puifque ces quatr.e Rois alliez, avant de vaincre les cinq autres .dtruifi* rent plufieurs Nations, lefquelks to^e!: appa-
remmen
February 16, 1965

Dr. Marianne Grunberg-Manago
Department of Biochemistry
Institut Biologic, Physico-Chimique
13 Rue Pierre Curie
Paris 5e, France

Dear Marianne:

This letter has been written often, in my head,  but as usual time

flies,  In spite of my silence, the various parcels you sent around Christmas
time were received, and enthusiastically, The children love the records, and
are acquiring good French pronunciation from them.
American school system will eventually spoil them!
the ''cookbook" and will probably go on enjoying it for many years.
really one of the most delightful things I have ever seen!
for being so vwy nice.

It's too bad that the
All of us have enjoyed
           It is

We all thank you

As you may or may not have heard, the triplet synthesis did go very

well indeed.
Phil Leder and I are workfng on a manuscript describing the syntheses and
the products.

To date, about 20 different triplets have been prepared.

A draft dl1 be ready shortly and we'll send it to you.

The triplets as well as various other things have kept us away from the

phosphorylase stability problem.
started working myself on it--so there is no nws on that front.
Hcward, who had started out to work on it, has instead been studying, using
phosphorylase, various properties of a triple helix of 2 poly U and 1 diamino-
purine riboslde.
phosphorylase, as well as the potassium activated phosphodiesterase are really
very sensitive reagents for the study of eecondary structure.

Only lately have I gone back to it and

Frank

This helix was discmered by Frank and Todd Miles.

The

I have agreed to write a chapter on polynucleotide phosphorylase for a

        This is to described preparative methods for the enzyme,
         I noticed in your recent papers that you have been

new series entitled "Procedures in Nucleic Acid Chemistry," edited by Giulio
and David Davies.
not general aspects.
using Azotobacter enzyme, prepared according to the original procedure
(Grunberg-Manago, Ortie, and Ochoa, 1956) for polymer preparation. Do you
have any comments on the procedure, or growth of cells, or designation of
the cell strain, that Mould up date the procedure as described?
be very helpful in making the article 88 useful as possible.

This would

For the same reasons, I would be interested in any comments on the

-- E. coli preparation you recently published.
point at which one can stop and have enzyme good enough for polymer prepara-
tion, or fa It adviaable to go all tha way through?

In particular, is there any

-2-

Recently we looked, in crude 20,000 x & extracts,  at the relative

       The diesteraee is about 40-50 tfmss more active (for

activities of po1yn;cleotide phosphorylase and potassium-activated phos-
phodiesterase.
polymer breakdown, than is phosphorylase. Neither one is changed appre-
ciably in 2 mutant6 that lack the "ribosomal" Was8 (A-19 of Gilbert and
Vatson, and MBE-600 of Made).

Vhen are you coming for your lectures?

Best regard6 to Armand and

the children,

Yours,

Mutine Singer

MS: peig
At the Tevatron, protons and antiprotons collide with a center-of-mass energy
of 1.8 TeV. In this energy range the dominant source of top quarks is the 
production of $t\bar{t}$ pairs via quark-antiquark annhilation and gluon-gluon 
fusion. We present our analyses to determine the 
mass of the top quark reconstructed through the ``lepton+jets'' decay channel
in the 106 $\pm$ 4.1 pb$^{-1}$ of data collected by the Collider Detector at 
Fermilab (CDF) from 1992-1996. 

In the past, the top mass was obtained by comparing the observed 
kinematic features of top events to those predicted for different top quark 
masses. These distributions are known as $templates$. While 
any kinematic variable, which exhibits sensitivity to the top mass can be used 
to calculate the mass of the top quark, the lowest statistical uncertainty is 
achieved by reconstructing the top mass from the decay products of the 
$t\bar{t}$ pair. It was also observed that it is possible to obtain a better 
estimate of the top mass by fitting the different templates to a smooth 
function. Previously, we have used a combination of a Gaussian and a Gamma 
function to fit the distributions. In this analysis, we find that using a
Neural Network (NN) to fit the distribution gives slightly better results, and 
that the NN fitting technique is applicable to any kinematic variable.  
Following this recipe the top mass is measured to be 
$177.9 \pm 4.7(stat.) \pm 4.6(syst.)$ GeV/c$^2$ when using the reconstructed 
mass, $M_{rec}$. When we use the total transverse energy of the events, $\Ht$, 
the mass of the top quark is found to be 
$204.4 \pm 9.2(stat.) \pm  9.2(syst.)$ GeV/c$^2$. 

As noted, there are different kinematic variables that can be used to 
calculate the top mass. A Neural Network provides a simple and elegant way 
of combining all of these variables which have mass information. The idea is 
that combining the information from more than one kinematic variable would
result in a more accurate measurement of the top mass. Therefore, this NN based 
technique uses a combination of $M_{rec}$, $H_T$, the invariant mass of the 
$t\bar{t}$ system, $M_{t\bar{t}}$, and the sum of the $P_T$'s of the two 
leading jets, $P_T(1) + P_{T}(2)$. These variables were chosen because they 
exhibit the greatest mass dependence. The Neural Networks attempt to classify 
the events as $t\bar{t}$ signal or background. For each event the NN provides 
a set of probabilities that it has come from any of the top masses used in this 
analysis, as well as background. Using this information we construct a 
discrete likelihood function from which the top mass is calculated to be 
$181.9 \pm 5.1 (stat.) \pm 5.2(syst.)$ GeV/c$^2$. 
 



Posted to /cdf/pub/thesis/cdf6216_topMass_NN_thesis.ps
    http://www-cdf.fnal.gov/thesis/cdf6216_topMass_NN_thesis.ps

Posted by csanchez@cdfsga
000
NWUS54 KJAN 062224
LSRJAN
PRELIMINARY LOCAL STORM REPORT
NATIONAL WEATHER SERVICE JACKSON MS
423 PM CST SAT JAN 06 2007
..TIME...   ...EVENT...      ...CITY LOCATION...     ...LAT.LON...
..DATE...   ....MAG....      ..COUNTY LOCATION..ST.. ...SOURCE....
            ..REMARKS..
1227 AM     TORNADO          2 SW SOSO               31.73N 89.30W
01/05/2007  F1               JONES              MS   NWS STORM SURVEY
            NUMEROUS TREES SNAPPED AND UPROOTED. ONE TREE FELL ON A
            CAR. A STORAGE BUILDING WAS COMPETELY DESTROYED. A SINGLE
            WIDE TRAILER WAS PUSHED OFF ITS BLOCKS BUT REMAINED
            UPRIGHT. ROOF DAMAGE OCCURRED TO A DOUBLE WIDE TRAILER.
            THE DAMAGE WAS ALL ESTIMATED TO BE IN THE 75 TO 100 MPH
            RANGE. PATH LENGTH 1.2 MILES. MAXIMUM WIDTH 100 YARDS.
&&
$$
SCW
Chapter 2: Reinforced Concrete Components 
System: Reinforced Concrete 
Component Type: Isolated Wall or Stronger Wall Pier 
Predominant Behavior Mode: FlexureMleb Crushing 
Secondary Behavior Mode: -
Damage at +3-in. deflection 
A = 3 In Ah, = 0.017 dg = 1.0 
Example 2 of 3 
Load versus deflection relationship 
Damage at -3-in. deflection 
A = 3 in Ah, = 0.017 ag = 1.0 
Damage after web crushing 
A = 5 in Ah, = 0.028 dg= 0.6 
Technical Resources FEMA 307 
Chapter 2: Reinforced Concrete Components 
DAMAGE PATTERNS AND HYSTERETIC RESPONSE 
System: Reinforced Concrete 
Component Type: Isolated Wall or Stronger Wall Pier 
Example 3of 3 
Predominant Behavior Mode: Flexure web Crushing 
Secondary Behavior Mode: -
Damage at +3-in. deflection 
A=3in dlh,,=0.017 lQ=l.O 
I in. * 25.4 mm 
I kip = 4.448 kN 
Damage at -34. deflection 
A = 3 in A/h, = 0.017 lQ= 1.0 
Load versus deflection relationship 
Damage after web crushing 
A= 3 in A/h, = 0.017 AQ = 0.3 
FEMA 307 Technical Resources 
Chapter 2: Reinforced Concrete Components 
System: Reinforced Concrete 
Component Type: 
Isolated Wall or Stronger Wall Pier 
Example 1 of 2 
Predominant Behavior Mode: Flexure Sliding Shear 
Secondary Behavior Mode: -
Crack pattern of specimen CI-1 at end of phase II. 
I in.=25.4mm 
Ikip.4.4S kN 
Load versus top deflection relationship for 
specimen CI-1. 
Technical Resources FEMA 307
2005

Ring 12:
Volumetric soil moisture not available for entire year. (Sep.-Dec.)
01R12102.xls
02R12102.xls
03R12102.xls
04R12102.xls
05R12102.xls
06R12102.xls
07R12102.xls
08R12102.xls

Ring 21:
Volumetric soil moisture not available for entire year. (Sep.-Dec.)
01R21102.xls
02R21102.xls
03R21102.xls
04R21102.xls
05R21102.xls
06R21102.xls
07R21102.xls
08R21102.xls


Ring 33:
Volumetric soil moisture not available for entire year. (Oct.-Dec.)
01R33102.xls
02R33102.xls
03R33102.xls
04R33102.xls
05R33102.xls
06R33102.xls
07R33102.xls
08R33102.xls
09R33102.xls


Ring 34:
Volumetric soil moisture not available for entire year. (Oct.-Dec.)
01R34102.xls
02R34102.xls
03R34102.xls
04R34102.xls
05R34102.xls
06R34102.xls
07R34102.xls
08R34102.xls
09R34102.xls
000
WGUS84 KOUN 310720
FLSOUN
FLOOD STATEMENT 
NATIONAL WEATHER SERVICE NORMAN OK
220 AM CDT THU MAY 31 2007

OKC013-311520-
220 AM CDT THU MAY 31 2007

...THE FLOOD WARNING CONTINUES FOR
  THE BLUE RIVER NEAR BLUE IN SOUTHEASTERN OKLAHOMA...
  
* UNTIL FURTHER NOTICE.
  
* AT 1 AM THURSDAY THE STAGE WAS 26.0 FEET. 
  
* MINOR FLOODING IS OCCURRING.
  
* FLOOD STAGE IS 24.0 FEET.
  
* FORECAST...THE BLUE RIVER HAS CRESTED AND WILL CONTINUE FALLING. 
  THE BLUE RIVER WILL FALL BELOW FLOOD STAGE AROUND 8 AM THURSDAY.
  
DO NOT DRIVE INTO FLOODED AREAS OR ATTEMPT TO CROSS ROADWAYS COVERED 
BY HIGH WATER. STAY TUNED FOR FURTHER INFORMATION BY LISTENING TO 
WEATHER RADIO OR LOCAL MEDIA SOURCES.

$$
SEXX01 KNEC 031727
EQREQB






The following  is  from  the  United  States  Geological  Survey,
National  Earthquake  Information Center:  Preliminary hypocenter
for earthquake of 2003 Apr 02, SOUTH OF THE FIJI  ISLANDS,  about
510  km  (320  miles)  SSW  of  Ndoi Island, Fiji:  latitude 25.1
degrees south, longitude 179.8 degrees east, origin  time  21  31
38.4  utc,  depth  500  km,  magnitude  5.7.   The  magnitude and
location may be revised when additional data and further analysis
results  are  available.   No damage is expected.  For additional
information,     see     the     USGS     NEIC      web      page
http://neic.usgs.gov/neis/bulletin/
Stations used:  SNZO eP 213504.7 TAU eP 213724.6
STKA eP 213743.2 epP 213909.9 POHA eP 213951.2
KIP eP 213953.7 epP 214133.0 GUMO eP 213957.3
VNDA eP 214010.1 e 214109.4 SBA eP 214011.2 e 214112.2
epP 214156.5 NWAO eP 214020.0 MBWA eP 214023.2
e 214201.7 MAJO eP 214216.7 ADK eP 214237.3
UNV eP 214252.0 YSS eP 214252.6 SAC eP 214309.9
SAO eP 214310.2 ABL eP 214311.7 LKC eP 214311.9
NSHM eP 214312.3 epP 214504.0 SNAA eP 214312.6
HOPS eP 214312.8 MWC eP 214313.3 BAR eP 214313.8
ISA eP 214316.5 epP 214504.8 CMB eP 214317.1 epP 214508.8
PFO eP 214317.2 epP 214508.9 OHCM eP 214317.7
WDC eP 214318.8 epP 214511.3 GSC eP 214320.8 epP 214510.2
MTUM eP 214321.3 epP 214511.6 GLA eP 214321.8 epP 214512.3
YBH eP 214322.4 epP 214513.2 BEKR eP 214322.8 epP 214512.2
WCN eP 214323.1 epP 214515.8 HUMO eP 214324.2 epP 214515.6
KDAK eP 214324.2 MNV eP 214325.1 epP 214518.1
LDFC eP 214326.4 TPH eP 214327.2 epP 214520.2
TPNV eP 214327.3 epP 214516.8 NEN eP 214329.1 epP 214517.4
MOD eP 214329.1 epP 214520.0 ENH eP 214331.9 epP 214527.1
MA2 eP 214333.5 qpP 214527.4 TUC eP 214333.7 epP 214523.4
BMN eP 214333.7 epP 214522.5 BJT eP 214335.0
WVOR eP 214335.5 epP 214524.3 OCWA eP 214337.5 qpP 214529.9
WUAZ eP 214338.2 GNW eP 214339.4 PGC eP 214341.3
FIB eP 214341.5 PMR eP 214343.2 EYAK eP 214343.3
epP 214535.2 HAWA eP 214344.0 epP 214537.3
MVU eP 214344.4 epP 214535.7 SML eP 214345.2
DIV eP 214345.6 epP 214537.6 DUG eP 214345.9
TNA eP 214348.0 qpP 214545.4 MPU eP 214349.2
HLID eP 214349.9 epP 214541.7 CTU eP 214350.3 epP 214545.8
LENM eP 214350.3 LAZ eP 214350.4 qpP 214541.9
LTX eP 214350.8 epP 214544.0 JLU eP 214351.2
BNM eP 214351.3 epP 214547.0 MCK eP 214351.6 epP 214544.2
HWUT eP 214352.7 qpP 214545.8 PV10 eP 214352.8
ANMO eP 214353.4 epP 214545.0 NEW eP 214354.0
GDL2 eP 214354.4 epP 214549.1 COLA eP 214357.1 epP 214549.7
AHID eP 214357.3 MCMT eP 214357.7 qpP 214549.9
MSO eP 214358.1 epP 214554.1 DLBC eP 214359.0
CHMT eP 214400.5 epP 214552.6 BOZ eP 214402.2 epP 214554.0
LCCM eP 214402.3 epP 214554.9 SDCO eP 214402.3 qpP 214554.2
YMR eP 214402.8 epP 214548.9 DAWY eP 214404.2 epP 214556.4
HRY eP 214404.3 epP 214555.9 WALA eP 214404.4
JCT eP 214405.8 ULN eP 214419.1 epP 214611.7
RSSD eP 214419.9 INK eP 214424.9 SUR ePKP 214932.3
LBTB ePKP 214941.2 SPB4 ePKP 214943.6 KMBO ePKP 215003.7







                                                                Page 2




BR131 ePKPdf 215025.5 ePKPbc 215028.6 EIL ePKPdf 215025.8  ePKPbc
215030.4
DBIC ePKPdf 215043.7