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Looking for things to do in Hamburg? Whether you're a local, new in town or just
cruising through we've got loads of great tips and events. In diesem Jahr gibt
es das Oktoberfest Paket mit eigenem. Providence Bank Park. Arkansas Calendar of
Events. Upcoming local events, concerts, festivals, kids events, pet events, and
more in Hamburg metro area.

Blockchance Conference Hamburg Arkansas is home to amazing events year-round.
Date: Thursday, September 10, Unfortunately, in the current situation the HOW
conference team has concluded that it is not possible or reasonable to have a
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events that take place in and around the Village of Hamburg, please check out
the links to the left or below.

Public event.

Find tickets to all live music, concerts, tour dates and festivals in and around
Hamburg in and Be a part of the journey of aviation and innovation. Click this
link to learn about the Hamburg Middle School's summer reading requirements for
all incoming students in grades The wine and tourism event taking place in
Hamburg invites you to explore the 13 German wine regions. MIPIM is a 4-day real
estate exhibition, conference and networking event gathering 26, international
property professionals, in Cannes.

HansePferd Hamburg is going to open on Friday. Website Windenergy Hamburg. Watch
the keynote, learn from technical talks, and meet fellow local developers
online. Shenandoah Garden City Farmers. Die Brandursache ist noch ungeklärt.
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Movie Meets Media Hamburg Travel Guides. The coming EuroShop edition will be one
of the most exciting ever. Cancellation and Refund. Southern Manufacturing and
Electronics is the most comprehensive annual industrial exhibition in the UK and
a major pan-European showcase for new technology in machinery, production
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While countries such as Mexico, Argentina , and Brazil built railways and
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In , although the country had a land mass of 1,, square kilometers, there were
only 3, kilometers of railways. There were a total , kilometers of roadways;
however, only 13, kilometers of which were paved Williams and Guerrieri; Central
Intelligence Agency. Columbia is a country of contrasts. There are large cities
facing the common problems of industrialization such as air pollution from
vehicle emissions. There are rural sections where underdevelopment is a problem.
Only about 4 percent of the land is arable, and about 48 percent of it remains
forests and woodlands. Despite these large natural areas in Colombia,
deforestation and soil abuse persist as serious problems.

The population suffers from extreme income inequality.


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In , An unemployment rate of 20 percent intensified the economic problems
Central Intelligence Agency. Before the arrival of the Spanish, several Native
American groups occupied the region. However, none of these people had developed
the ability to write. Some groups, such as the Taironas constructed impressive
roads, bridges, systems of platforms for large buildings, and mountainside
terraces for agriculture.

The Taironas also produced stone statuary, gold objects, and fine ceramics. The
largest group was the Muisca, who lived in the intermountain basins of the
Cordillera Oriental. Depending mostly on agriculture for survival, the Muisca
made cotton textiles, worked gold, and made some stone sculptures. Although
there is reason to believe the Muisca were unifying their society when the
Spanish arrived, the group never demonstrated the engineering abilities of the
Taironas.


COVID-19 PANDEMIC IN COLOMBIA

Within years after the first Spanish settlement, nearly 95 percent of all Native
Americans in Colombia had died. Many were killed during armed conflicts with
European settlers, but the majority of deaths were caused by diseases such as
smallpox and measles, which were imported by Spanish settlers Bushnell. The era
of Spanish colonization began in with the founding of San Sebastian near Panama.
In , settlers founded Santa Marta, the oldest Spanish city still in existence in
Colombia.

For most of the colonial period, New Granada, which included the areas that
became Columbia, Panama, Venezuela, and Ecuador, fell within the Viceroyalty of
Peru as part of the Spanish empire. In , New Granada retained independent status
as a Viceroyalty separate from Peru. Administrative divisions such as these
influenced the boundaries of the countries when they sought independence
Bushnell. Although many Spaniards began their explorations searching for gold,
other colonists took advantage of the sedentary lifestyle of Native American
groups such as the Muisca. The Spanish established themselves as the leaders and
ruled through the existing native social organizations.

The Spanish crown outlawed this system of exploiting Native American labor,
called encomienda. However, the practice did continue for some time because it
served as a type of educational institution through which the European leaders
were able to teach the Native Americans the Christian faith and the ways of
civilization. Most Spanish colonists avoided the tropical grasslands of the
interior.

Jesuit priests went into those regions and established missions that gathered
together the communities of semi-settled Native American groups who lived there.
Depending on Native American labor, these missionaries created cattle ranches
and plantations that passed into the hands of other religious orders in when the
Jesuits were expelled from the Spanish empire. Through these mission
communities, Catholic priests served as mediators between the settled Native
Americans and the Spanish state, and they provided education for the Native
Americans that otherwise was unavailable.

However, critics complain that the education Native Americans received in the
missions actually was nothing more than an indoctrination into the Christian
faith and instruction in Spanish. The earliest missionary schools date to the
mid-sixteenth century. Although the seminary closed in due to student
dissatisfaction, it later reopened. Their goal was to record all of the
botanical species found in South America. Nonetheless, the educational efforts
in New Grenada were extensive.

By the end of the colonial period in , the number of Catholic clerics — whose
calling essentially required spiritual and educational endeavors — rose to
nearly 1, With a population of 1. The clerics could not provide education for
children from rural areas or from lower classes, despite the large number of
priests in colonial New Grenada. The members of the congress had not come
together to improve education.

Having broken with Spain , they sought to define the country's political
organization. Although these actions were driven more by anticlerical feelings
than by educational concerns, Santander did open several new secondary schools.
Despite opposition from the Catholic Church , Santander urged that works by
unorthodox authors, such as Jeremy Bentham , be included in the school's
curriculums.

According to the congressional delegates in , Spanish indifference had caused
widespread illiteracy, a condition they pledged to correct. Thus, in the
constitution of , the delegates chose as the date by which all voters would have
to pass a literacy test. Unfortunately, for the next 10 years, educational
reform moved slowly.

In , delegates met in a national convention to draft a new constitution.
However, acknowledging that literacy had not spread throughout the new republic,
the delegates postponed the date for voter literacy tests until Bushnell. A
civil war called the War of the Supremes interrupted educational reform. For
example, they removed the controversial authors from the secondary curriculum,
reduced the extent of theoretical studies, and increased studies that had more
practical applications, such as natural science.

In , fulfilling the Liberals' desire to reverse many of the Conservative
policies, the Congress enacted various policies that were intended to increase
the freedom of education. The Congress disbanded all universities, placing those
programs of higher education into colegios secondary schools , and ended all
academic requirements for people to practice any profession, with the exception
of pharmacy. The citizens had the freedom to decide what training they needed,
or if they needed any education at all, before entering a profession. He argued
that the sanction of , which originally expelled the Jesuits from the Spanish
empire, was still valid in New Granada.

To consolidate their victories, the liberals adopted a new constitution in They
offered universal male suffrage, removed the electoral college system, and
increased the number of officials who were elected rather than appointed. In
addition, the new constitution guaranteed freedom of worship for all citizens
and introduced civil marriage and divorce.

In , the liberals framed another constitution that changed the name of the state
to Estados Unidos de Colombia United States of Colombia and advanced the
regionalism of the country. The new constitution gave extensive authority to the
then nine states, allowing them to determine their own suffrage laws and
maintain their own services, such as postal delivery.

To further limit the authority of the federal government , the constitution of
reduced the president's term to two years and prohibited anyone from serving
consecutive terms Bushnell. By the liberal government had started to undo the
educational reforms of Emphasizing the traditional disciplines of law, medicine,
and philosophy, the university offered technical studies to help Colombia enter
the mechanical age. Three years later, the Congress made primary education in
Colombia free and compulsory and established several teacher training
institutions — called normal schools — to meet the sudden need for teachers.

To assist in the process, German experts were brought in to serve as instructors
at the normal schools.

Fearing this represented the beginning of a godless education, church leaders
called on parents to ignore the public schools. Some Catholics complained that
the German educators imported to staff in the schools belonged to the Protestant
faith.

To alleviate the controversy, the government allowed church representatives to
offer religious instruction in the public primary schools during specific hours
to pupils whose parents requested it. Some states required religious teaching in
the primary schools. Adopted in , this constitution, which remained in effect
until , offered free elementary education to any child who wanted it.

However, the constitution reversed the law that made such elementary education
compulsory. At the same time, the constitution declared Colombia a republic and
recognized the Catholic Church as the national church. The following year, the
government entered the Concordat of , requiring that all public education be
done in accordance with the Roman Catholic religion. As result, clergy could
approve school texts, determine the curriculum, and appoint teachers Bushnell,
Hanson. In , the central government took responsibility for establishing a
national system of education with the passage of the Organic Law of Public
Education, which made education free but not compulsory.

Together with its regulating decree of , the Organic Law set up a system of
national inspection, divided schools into elementary and secondary levels, and
established professional, industrial, and artistic branches. Although the law of
placed education under the control of the states, it gave the power to set
policy for all public, private, state, and national schools to the Ministry of
Education.

Other levels of government took different responsibilities. For example, states
had to pay teacher salaries while municipalities had to construct and furnish
the schools. Unfortunately, the law perpetuated discrepancies between urban and
rural education by ordering cities to provide six years of schooling and
requiring rural areas to provide only three Hanson.

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In , the Conservative government of Colombia made education compulsory, but did
not provide funds to make this possible.


DATING REGION IN BELEM BRAZIL

Contents:

Oct 23, 2020 Cheap Flight Deals from Belem (BEL) | LATAM Airlines Coronavirus:
Brazil headed for catastrophe Current Local Time in Belém, Pará, Brazil



Lavinas, ed. Publipur, Rio de Janeiro. Schmink, M. Schneider, R. World Bank,
Washington, DC. Silva, J. Skole, D. Smith, N. University of California Press,
Berkeley. Stedile, J. Toni, F. Turner, F. Holt Press, New York. Veiga, J. Velho,
O. Zahar, Rio de Janeiro. Walker, R. Deforestation and economic development.
Canadian Journal of Regional Science 16 3 , — Ecological Economics 18 ,67— World
Development 28 4 , — International Regional Science Review. Welch, C. Wood, C.
Moran, ed. Download references. Reprints and Permissions. Simmons, C. The
changing dynamics of land conflict in the Brazilian Amazon: The rural-urban
complex and its environmental implications.

Urban Ecosystems 6, 99— Download citation. Issue Date : March Search
SpringerLink Search. Abstract The Brazilian Amazon is an area of both serious
environmental degradation and social instability. Immediate online access to all
issues from Subscription will auto renew annually. References Almeida, A.
Simmons View author publications.

View author publications. At 7 o'clock, the archbishop conducts the image to the
carriage as bells toll and fireworks explode. The main procession then goes
through the streets of the city to the Architectonic Centre of Nazareth, known
for its Sanctuary Square.


OCT 23, 2020

Built in a 23,square-metre area, the Hangar Convention and Fair Center of the
Amazon has 12 rooms, ticket offices, baggage keeping, press room, and a food
court , distributed in two big buildings with a parking lot for vehicles.
Genuine Amazonian trees will soon be planted in the outdoor area. National
conventions had not been held in the Northern region previously. Hangar, whose
auditorium has room for 2, participants, has some of the best technologies
available in the world and is the most modern and functional space for events in
the country. These activities bring together approximately 28 million
participants.

Neoclassical architecture is also present in buildings such as the Theatro da
Paz , built in Many of the buildings at the end of the nineteenth century and
early twentieth century also echo French architecture. The local Amerindian
culture makes use of local elements to create the colors and flavors of its
cuisine. Its pulp is also extracted to make juices, candies, jellies, liquors,
and ice cream. Long prized by the local population, it recently it has also
reached the national menu. Freshwater crab , a traditional local delicacy, is
popular.

Found only in swamps, its well-tempered meat can be served in different forms:
as a shell, the so-called unha the claws or toc-toc. Its preparation is
time-consuming and its final appearance is quite surprising for those who have
never tried it, due to the dark look of the cooked maniva ground manioc leaves.
But this first impression ends quickly, after you taste the dish with its
seemingly awkward ingredients. The latter stadium is currently the home of Clube
Municipal Ananindeua who represent the very large suburb of Ananindeua. The
Ver-o-Peso Portuguese: "see the weight" market in the old port centre is a major
tourist attraction.

There are eight trails, all providing direct contact with various species of
flora and fauna. The most popular is the monkey trail, which takes about 40
minutes and goes from Bolonha lake to the visitor center, where other activities
are available. Located less than 15 kilometres 9. Summary of the Amazon
landscape with lush flora and fauna, the zoo has about 14 miles 23 kilometres of
trails in an area composed of four interconnected ecosystems.

A large attractive Bioparque is the Museum of Paleontology and Malacology where
visitors can watch a collection of three thousand pieces of exposed shells and
mollusks collected from all continents. On site, you will also see paintings
with motifs of cabloco Amazon. Comprising 16 hectares , in the ample Avenida
Almirante Barroso , one of the city's busiest thoroughfares, having 2, native
species, an orchidary, lakes, caverns, waterfalls and even a replica of a
mountain. The U- Pb spike is used for U -Pb analysis of whole rock and sulfide
samples and any quantity of mineral fractions higher than 2 mg.

The U- Pb spike is useful for small fractions 0. Finally, calibration of spikes
were verified and adjusted by analyses of the international standard zircon. For
calibration of the ion counter efficiency in relation to that of Faraday cup, ng
of NBS is used in every magazine. The isotope ratios for standards during period
were:. Thallium interference was controlled on Tl peak by periodic scanning of
mass spectrum in mass range.

In some special cases, zircon grains can be step-wise leached Krogh and Davis a,
Mattinson , , Corfu , Davis and Krogh The Mattison technique is preferred for
complex and metamictic grains. When the U- Pb tracer is used, we add it after
zircon dissolution and aliquoting. The complete dissolution of the zircon grains
is checked under a stereomicroscope and the sample solutions evaporated to
dryness.

There are 5 main ways to separate U and Pb from zircon solution:. Description of
modified method of Parrish et al. For this procedure hand-made shrinkable Teflon
micro-columns with internal diameter of 1. The resin usually is not disposable
because of long period of pre-washing and it can be used up to 20 times, if the
lead blank does not increase.


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The sequence of elements separation with consists of:. Total blanks for this
zircon procedure are pg of Pb and 0. Description of Paquette and Pin modified
method. The columns are washed in the same way as for the procedure described
above.


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The resin mixture consists of 0. The resin mixture serves only for one
separation procedure. The sequence of elements separation is the following:.
Resin washing: 2 ml of 6N HCl; Resin media equilibration: 2x2 drops of 2. Total
blanks for this zircon procedure are 4 pg of Pb and 0. This procedure also can
be applied for analysis of other accessory minerals titanite, rutile, apatite ,
but separation of Ca and Fe from the sample is not ideal.

Depending on the characteristics of accessory mineral, we different procedures
of washing are applied. Rutile, titanite, garnet, other oxides and silicates are
washed with methanol, 0. The mineral fractions may be previously polished by air
abrasion mill without pyrite powder. For bigger samples the U- Pb tracer is
utilized. In case of using U- Pb spike, aliquoting is made and spike is added
after dissolution. The micro-column is used for 0. Small amounts of titanite,
apatite and monazite are processed in micro-columns using the same technique
used for zircon with HCl and H 2 O.

The oxides and silicate mineral solutions are separated with HBr using a
modified technique of Tera and Wasserburg The Pb separation sequence is the
following:. Resin media equilibration: 2x3 drops of 0. Uranium can be separated
by the same method as mentioned for zircon separation with HCl and H 2 O or by
the following HNO 3 technique:. The current blanks for total procedure
digestion, separation with HBr-HNO 3 technique and deposition for accessory
mineral are 60 pg of Pb and 0. Ordinary digestion in oven normally takes days
and, in some cases, even more.

The microwave digestion conditions are: 36 min at W; 3 min cooling, 15 min at W;
3 min cooling.


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Nanyang Technological University, Singapore Video. Round Trip. The resin mixture
serves only for one separation procedure. These zircons are characterized by
high uranium ppm and lead ppm concentrations Table IV. Not only is LATAM a
leader in sustainability and service technology, but it is also the largest
airline in the region. Best fares on flights from Belem. Women are
over-represented in informal employment, where they do not have social security
coverage. History at your fingertips. Rb-Sr age dating of tin-bearing granites
from the Central Sikhote-Alin. For other chemical operation lower temperature
dissolution, collection of U, Pb during ion exchange separation. Some
improvements of dating region in Belem Brazil procedures aiming blank reduction
are in course. The smaller Brig. Isotopic compositions of Pb and U are measured
on a Finnigan MAT variable multicollector mass spectrometer equipped with 7
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the pregnant women in the Control group will be guided about normal labor and it
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After digestion first steps, the sample is evaporated, and the procedure is
repeated. The concentration aliquot is spiked with U- Pb tracer ''A''. Both
aliquots are evaporated, 0. Then, 1.

The U separation procedure using the same columns is following:. The blanks for
total whole rock procedure are 0. Isotopic compositions of Pb and U are measured
on a Finnigan MAT variable multicollector mass spectrometer equipped with 7
Faraday cups and 1 ion counter. The numbers of Faraday cups are 2, 3, 4, 5, 6, 7
and 8, the ion counter position corresponding to the cup 5. The lead-uranium
fraction mixed with the silica gel-phosphoric acid solution is loaded under HEPA
laminar flow on a single outgassed rhenium filament.

The filament is heated slowly from 0.

Different configurations of Faraday cups and ion counter are utilized for the
lead analysis with different spikes and different signal levels. Transportation
within the state and externally is almost entirely by water, road, or air. Area
, square miles 1,, square km. Print Cite.


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Contents:

NAOE MIAMI | CHEF KEVIN CORY | BIOGRAPHY Access Denied The pandemic pipeline A
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The interdecadal NAO variability also exhibits a marked linkage with the
underlying ocean Rodwell et al.

More specifically, the warm phase of the Atlantic multidecadal oscillation AMO ,
characterized by broad warming over the North Atlantic Deser et al. Given this
potential influence of interdecadal SST variability on the atmospheric
circulation and its modulating effect on the meridional excursions of the jet
stream and occurrence of blocking events Woollings et al.

While they argue that it is the change in the blocking frequency that may partly
drive multidecadal SST anomalies over the North Atlantic, multidecadal oceanic
variability may, in turn, have the potential to modulate blocking frequency as
suggested by recent modeling studies Davini et al. Despite the recent efforts
made to deepen our understanding of the processes regulating interdecadal
variability over the North Atlantic sector and its influence on subseasonal
variability, large uncertainties remain concerning the driving factors of
interdecadal atmospheric variability and the dynamical processes by which it
modulates variability on shorter time scales.

The present work thus explores, with the use of multidecadal atmospheric
reanalysis data, the relationship between the interdecadal variability in the
state of atmospheric circulation and subseasonal variability over the North
Atlantic sector and seeks a dynamical explanation for the relationship. We first
identify the dominant mode of covariability between interdecadal fluctuations of
the midtropospheric background state and modulated subseasonal variability
through a maximum covariance analysis see section 2c for details.

In the following, fluctuations on time scales between 10 days and a season, from
which subweekly variations associated with cyclones and anticyclones migrating
along the storm tracks are excluded, are referred to as subseasonal variability.
Our focus on this time scale of atmospheric variability is motivated by the need
for a deeper understanding of the dynamics of persistent weather anomalies,
including blocking events. We also focus on the winter season, when the
variability of the North Atlantic atmospheric circulation is largest both on
decadal Simpson et al.

Considering its direct socioeconomic impacts, we focus on subseasonal
variability of SAT rather than the variance of the midtropospheric circulation
as in many other studies e. Our maximum covariance analysis reveals that
interdecadal NAO variability can substantially modulate subseasonal variability.
We will then show that interdecadal changes in subseasonal SAT variability are a
consequence of amplitude modulations of quasi-stationary eddies.

We will also show that the interdecadal NAO circulation anomalies are embedded
in a basin-scale wave train originating from the subtropical North Atlantic that
appears to be forced in part by precipitation anomalies that are sustained by
enhanced turbulent heat fluxes near the Gulf Stream.

This study primarily uses data from the atmospheric reanalysis of the twentieth
century ERAC; Poli et al. Unlike conventional reanalyses, ERAC only assimilates
surface pressure and marine winds. Only the ensemble mean of 20CRv2c is used for
the comparison. The ability of these two surface-input reanalyses to capture
interdecadal changes in subseasonal surface variability is also briefly
evaluated by comparing them to conventional reanalyses: NCEP—NCAR Kalnay et al.

A thorough description of these datasets is provided in Fujiwara et al. Surface
data from ERAC are analyzed on a 1. The subseasonal SAT variability is evaluated
by applying a 10—day Butterworth bandpass filter locally for each winter season
from November to March, after which only the months of December—February DJF are
retained to eliminate artifacts arising from the filter edges. Whereas the day
lower bound is often used to separate subseasonal variability from
high-frequency variability Kushnir and Esbensen ; Blackmon et al.

Here we use an upper limit of 60 days, similar to Kushnir and Wallace , to
ensure a clear separation from seasonal-scale variability, which is important
for investigating interactions between the wintertime basic-state circulation
and subseasonal variability. The separation of the subseasonal eddies from the
high-frequency eddies is justified by the differences in wave—mean flow
interactions between the two time scales Hoskins et al. Similar results are
obtained when using a 10—day filter not shown. To characterize how subseasonal
SAT variability is modulated from one year to another, we locally define a
measure of subseasonal variability SSV as the standard deviation of the
subseasonal SAT component for every winter season.

The resultant index is hereafter referred to as interdecadal modulations of
subseasonal variability SSV ID. The locations that tend to be affected strongly
by interdecadal changes of SSVID around the North Atlantic sector section 3b are
chosen. SSV varies substantially from one year to another and, at some
locations, almost doubles between its maximum and minimum.

The interdecadal variability isolated with SSV ID is not as large as the full
interannual variability but nonetheless shows impressive extents in some
locations such as over Quebec and Denmark. This suggests that subseasonal
variability and its year-to-year modulations are reasonably well constrained by
the assimilation of surface data alone. This appears to be largely due to a
time-mean bias since the two reanalyses overall exhibit similar interdecadal
variability.

We have repeated the same analysis of SSV ID with 20CRv2c and obtained similar
results not shown , indicating that this bias does not adversely affect our
analysis of interdecadal variability. We select ERAC for our main analysis
primarily because it has a better representation of the dynamical variability in
the upper troposphere Gerber and Martineau , which is necessary for evaluating
the energetics of atmospheric eddies.

The evolution of the subseasonal variability SSV of SAT is shown for several
reference locations rows and various reanalysis datasets color-coded according
to the legend. The reference coordinates are indicated in the upper-left corner
of each panel.

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All values have units of K. Leading modes of interdecadal covariability between
the winter-mean atmospheric circulation and SSV are identified with maximum
covariance analysis Bjornsson and Venegas ; Bretherton et al. The results are
insensitive to the choice of the domain. In fact, the dominant SVD mode over the
North Atlantic can be retrieved from a similar SVD analysis carried out for the
whole Northern Hemisphere, although the fraction of the total squared covariance
explained is reduced substantially.

The SVD analysis applied to the correlation matrix in place of the covariance
matrix yields essentially the same results. The use of Z to characterize the
basic-state circulation is motivated by the fact that subseasonal variability is
produced by eddies that have deep vertical structures Blackmon et al. A similar
SVD analysis with sea level pressure in place of Z yields consistent results not
shown.

Interdecadal changes in the energy of subseasonal eddy anomalies can be
quantified by evaluating the atmospheric energy budget. It was introduced by
Lorenz with a decomposition of the atmospheric circulation into its zonal mean
and deviations from it and was later reformulated by Oort with a partitioning of
energy associated with the time-mean flow and anomalies. Our study uses the
latter to investigate sources of eddy energy over the subseasonal frequency
band.

We define the subseasonal component of variability, denoted here with primes, in
the same manner as we defined the SSV index 10—day bandpass filter.


NAOE MIAMI | CHEF KEVIN CORY | BIOGRAPHY

The slowly evolving basic state, denoted with overbars, is defined as the DJF
mean in each year. For the purpose of this study, which focuses on interdecadal
variability, a yr low-pass filter is further applied on the winter-mean fields.
The barotropic conversion of kinetic energy CK from the background state to
subseasonal eddies is expressed as. The eddy available potential energy EAPE
associated with subseasonal thermal anomalies is defined as.

The conversion of available potential energy CP from the background flow to
subseasonal eddies may be expressed Kosaka and Nakamura ; Tanaka et al.
Feedbacks from high-frequency eddies, which are extracted with a day high-pass
Butterworth filter and denoted with double primes, are also evaluated with the
method of Tanaka et al. In practice, all the conversion terms in 2 , 5 , 7 , and
8 were evaluated with the formulas for spherical coordinates and subjected to a
yr low-pass filter. Attempting to explain changes in eddy energy with the use of
energy conversion terms can lead to some ambiguity since both the energy terms
EKE and EAPE and conversion terms CP and CK depend on the squared magnitude of
eddy quantities.

The inverse of the efficiency thus offers a measure of the time scale needed to
fully replenish the energy of subseasonal eddies Kosaka and Nakamura Statistical
significance for all regressions is evaluated with a t test for the population
correlation coefficient r. Here we estimate the effective number of degrees of
freedom taking into account serial correlation as.

For our investigation, the AMO index is obtained through the same method as
described in detail by Ting et al. Since the AMO index does show some
sensitivity to the season used to compute it Yamamoto and Palter , we focus on
the winter index to more accurately capture interactions with the winter-mean
atmospheric circulation.

This is also motivated by the fact that the connection between SST variability
and atmospheric circulation variability over the North Atlantic sector is
seasonally dependent, with a maximum in late winter Simpson et al.


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Nevertheless, interdecadal modulations of subseasonal variability are found to
maximize in midwinter not shown , and thus we focus on DJF for our analysis. A
low-pass filter with a yr cutoff is subsequently applied and followed by
normalization. The interdecadal variability of the lower-tropospheric hPa
circulation and activity of subseasonal eddies, with periods ranging from 10 to
60 days, is overviewed as wintertime statistics for DJF Fig. The climatology and
interdecadal variability of EKE are both maximized over the North Atlantic
sector, where the exit region of the eddy-driven jet is located, in agreement
with classical analyses of subseasonal variability Blackmon et al.

Meanwhile, the EAPE of subseasonal eddies is the largest over high-latitude
landmasses but weaker over the ocean, which is indicative of damping of
lower-tropospheric thermal variability at the ocean—atmosphere interface. The
interdecadal variability of EAPE is also largest over the same regions. Decadal
standard deviation shadings and climatology contours of DJF mean statistics.
Contours of standard deviation and climatology are in steps of 0.

By generating 10 synthetic Gaussian white noise time series with the same
variance as the original time series, we have verified that interdecadal
variations in U, EKE, EAPE, and SATVAR are unlikely to be explained by white
noise over some regions of the North Atlantic sector and surrounding landmasses.
This result indicates that their variability is unlikely to be purely internally
driven and likely to be under an external influence such as ocean variability
Simpson et al. Similar results are obtained when assuming a red noise process
instead of white noise since 1-yr lag autocorrelation of each of those
atmospheric variables investigated is typically quite small not shown.

The fraction of the variance of the original fields explained by SVD1 i. The
dipolar Z ID anomalies shown in Fig. Typical time scales of the SVD1 variability
are examined by evaluating its power spectral characteristics. As shown in Fig.
These significant spectral peaks suggest that an external forcing may influence
SVD1 on decadal to multidecadal time scales.

They are shown together with the expansion coefficients thick lines shown
previously in Fig. The power spectrum of the AMO is also shown for reference.
Among the external forcings that are known to influence North Atlantic
atmospheric variability, the AMO is one of the main contenders Deser et al.

In Africa, demand remained strong centering on mining equipment. However, the
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In response to the booming market for solar cells, Komatsu NTC boosted its sales
of wire saws. Segment profit increased Segment profit ratio was 8. Japan
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