Search results for "TLA"
showing 10 items of 1764 documents
"Table 4" of "Search for Higgs boson decays into a $Z$ boson and a light hadronically decaying resonance using 13 TeV $pp$ collision data from the AT…
2020
Expected and observed 95% CL upper limits on $\sigma(pp\to H)B(H\to Z(\eta_c~\text{or}~J/\psi))/$pb. The smaller (larger) quoted ranges around the expected limits represent $\pm 1\sigma$ ($\pm 2\sigma$) fluctuations.
"Table 4" of "Search for low-mass dijet resonances using trigger-level jets with the ATLAS detector in $pp$ collisions at sqrt(s)=13 TeV"
2018
Expected 95% CL limit on cross section times acceptance times branching ratio for each width and mass of Gaussian signal shape tested, in the region defined by |y*|<0.3.
"Table 6" of "Search for low-mass dijet resonances using trigger-level jets with the ATLAS detector in $pp$ collisions at sqrt(s)=13 TeV"
2018
Expected 95% CL limit on cross section times acceptance times branching ratio for each width and mass of Gaussian signal shape tested, in the region defined by |y*|<0.6.
"Table 3" of "Search for low-mass dijet resonances using trigger-level jets with the ATLAS detector in $pp$ collisions at sqrt(s)=13 TeV"
2018
Observed 95% CL limit on cross section times acceptance times branching ratio for each width and mass of Gaussian signal shape tested, in the region defined by |y*|<0.3.
"Table 2" of "Search for low-mass dijet resonances using trigger-level jets with the ATLAS detector in $pp$ collisions at sqrt(s)=13 TeV"
2018
Data, estimated background and uncertainties, in the region defined by |y*|<0.6.
"Table 5" of "Search for low-mass dijet resonances using trigger-level jets with the ATLAS detector in $pp$ collisions at sqrt(s)=13 TeV"
2018
Observed 95% CL limit on cross section times acceptance times branching ratio for each width and mass of Gaussian signal shape tested, in the region defined by |y*|<0.6.
"Table 1" of "Search for low-mass dijet resonances using trigger-level jets with the ATLAS detector in $pp$ collisions at sqrt(s)=13 TeV"
2018
Data, estimated background and uncertainties, in the region defined by |y*|<0.3.
Arvovallan ja vakauden puolesta : Jugoslavian hajoaminen Ranskan parlametin keskusteluissa vuosina 1991-1995
2013
Tässä tutkimuksessa perehdytään niihin tulkintoihin, joita Ranskan parlamentissa esitettiin vuosina 1991–1995 Jugoslavian hajoamista seuranneeseen konfliktiin liittyen sekä siihen, miten tulkinnoista muodostui Ranskan sisäpoliittinen kysymys. Hallitukselle esitetyistä kysymyksistä on muodostunut tärkeä parlamentaarinen instrumentti, jonka avulla parlamentaarikoiden on mahdollista pakottaa haluamansa aiheet osaksi valtiopäivätyöskentelyä. Ensisijaisen tutkimusaineiston muodostavatkin Ranskan parlamentin istuntopöytäkirjoista löytyvät hallitukselle esitetyt kysymykset, joita täydentävät (entistä) Jugoslaviaa koskevat hallituksen tiedonannot. Aineistoa lähestytään noudattamalla Quentin Skinner…
Accounting More Precisely for Peat and Other Soil Carbon Resources
2012
In the context of “recarbonization”, it is important to know where the soil C stocks are located and how much of these are prone to emission to the atmosphere. While it may appear to be a trivial question considering available global estimates and maps, yet there is a strong need to emphasize that erroneous estimates are made in assessing the global soil C stocks. Without doubt, peatlands hold the single most important soil C stock at the global scale, and these soils are mostly located in the northern latitudes between 50°N and 70°N. However, there are additional wetlands or other ecosystems which also hold potentially relevant amounts of soil C stocks. From the soil science perspective, i…
Parasite fauna and community structure of bathydemersal fishes: Notacanthus bonaparte (Osteichthyes), Etmopterus spinax and Deania profundorum (Chond…
2017
Resumen El mar profundo es el mayor bioma de la tierra y el menos estudiado (Ramirez-Llodra et al. 2010). Si bien inicialmente el mar profundo se consideró como un ambiente muy estable con variaciones muy leves por debajo de la termoclina permanente, los estudios realizados en las últimas décadas indican que el mar profundo es un ambiente más dinámico de lo que se pensaba (Gage 2003, Ramirez-Llodra et al. 2010). La variabilidad natural de los procesos que tiene lugar en los hábitats del mar profundo tiene su origen en diferentes factores entre los que se encuentran las corrientes horizontales de masas de agua de grandes dimensiones dirigidas por las corrientes circunglobales, las cuales pue…