A<sc>bstract</sc> The production cross sections of$$ {\textrm{B}}_{\textrm{s}}^0 $$ and B+mesons are reported in proton-proton (pp) collisions recorded by the CMS experiment at the CERN LHC with a center-of-mass energy of 5.02 TeV. The data sample corresponds to an integrated luminosity of 302 pb−1. The cross sections are based on measurements of the$$ {\textrm{B}}_{\textrm{s}}^0 $$ →J/ψ(μ+μ−)ϕ(1020)(K+K−) and B+→J/ψ(μ+μ−)K+decay channels. Results are presented in the transverse momentum (pT) range 7–50 GeV/cand the rapidity interval |y|<2.4 for the B mesons. The measuredpT-differential cross sections of B+and$$ {\textrm{B}}_{\textrm{s}}^0 $$ in pp collisions are well described by fixed-order plus next-to-leading logarithm perturbative quantum chromodynamics calculations. Using previous PbPb collision measurements at the same nucleon-nucleon center-of-mass energy, the nuclear modification factors,RAA, of the B mesons are determined. ForpT>10 GeV/c, both mesons are found to be suppressed in PbPb collisions (withRAAvalues significantly below unity), with less suppression observed for the$$ {\textrm{B}}_{\textrm{s}}^0 $$ mesons. In thispTrange, theRAAvalues for the B+mesons are consistent with those for inclusive charged hadrons and D0mesons. Below 10 GeV/c, both B+and$$ {\textrm{B}}_{\textrm{s}}^0 $$ are found to be less suppressed than either inclusive charged hadrons or D0mesons, with the$$ {\textrm{B}}_{\textrm{s}}^0 $$ RAAvalue consistent with unity. TheRAAvalues found for the B+and$$ {\textrm{B}}_{\textrm{s}}^0 $$ are compared to theoretical calculations, providing constraints on the mechanism of bottom quark energy loss and hadronization in the quark-gluon plasma, the hot and dense matter created in ultrarelativistic heavy ion collisions.
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High Salinity Shelf Water production rates in Terra Nova Bay, Ross Sea from high-resolution salinity observations
Abstract High Salinity Shelf Water (HSSW) formed in the Ross Sea of Antarctica is a precursor to Antarctic Bottom Water (AABW), a water mass that constitutes the bottom limb of the global overturning circulation. HSSW production rates are poorly constrained, as in-situ observations are scarce. Here, we present high-vertical-and-temporal-resolution salinity time series collected in austral winter 2017 from a mooring in Terra Nova Bay (TNB), one of two major sites of HSSW production in the Ross Sea. We calculate an annual-average HSSW production rate of ~0.4Sv(106m3s−1), which we use to ground truth additional estimates across 2012–2021 made from parametrized net surface heat fluxes. We find sub-seasonal and interannual variability on the order of$$0.1$$ $${Sv}$$ , with a strong dependence on variability in open-water area that suggests a sensitivity of TNB HSSW production rates to changes in the local wind regime and offshore sea ice pack.
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- PAR ID:
- 10559749
- Publisher / Repository:
- Nature
- Date Published:
- Journal Name:
- Nature Communications
- Volume:
- 15
- Issue:
- 1
- ISSN:
- 2041-1723
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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