Schemes of multi-parameter stations in the Bering and Chukchi Seas and North Pacific made in research cruises of TINRO (1986–2019)

Spatial distribution of stations made in research expeditions conducted by Pacific Res. Inst. of Fisheries and Oceanography (TINRO) in the Bering and Chukchi Seas and in the North Pacific in 1986–2019 is discussed. Schemes of the stations for every cruise are presented and sorted by decades, years, seasons, and months. The data sufficiency is estimated at regional and temporal levels by calculation of the stations number in the daytime and nighttime, per years, per seasons, and per biostatistical areas.

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Spatial distribution analysis of the North Pacific spiny dogfish,Squalus suckleyi, in the North Pacific using generalized additive models

Fisheries Oceanography ◽

10.1111/fog.12225 ◽

2017 ◽

Vol 26 (6) ◽

pp. 668-679 ◽

Cited By ~ 6

Author(s):

Toshikazu Yano ◽

Seiji Ohshimo ◽

Minoru Kanaiwa ◽

Tsutomu Hattori ◽

Masa-aki Fukuwaka ◽

...

Keyword(s):

Spatial Distribution ◽

North Pacific ◽

Generalized Additive Models ◽

Additive Models ◽

Spiny Dogfish ◽

Distribution Analysis ◽

The North ◽

The North Pacific

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Trends and Variability of North Pacific Polar Lows

Advances in Meteorology ◽

10.1155/2013/170387 ◽

2013 ◽

Vol 2013 ◽

pp. 1-11 ◽

Cited By ~ 8

Author(s):

Fei Chen ◽

Hans von Storch

Keyword(s):

Spatial Distribution ◽

North Pacific ◽

Canonical Correlation ◽

Decadal Variability ◽

Observational Evidence ◽

Positive Trend ◽

Mean Flow ◽

Polar Lows ◽

The North ◽

The North Pacific

The 6-hourly 1948–2010 NCEP 1 reanalyses have been dynamically downscaled for the region of the North Pacific. With a detecting-and-tracking algorithm, the climatology of North Pacific Polar Lows has been constructed. This derived climatology is consistent with the limited observational evidence in terms of frequency and spatial distribution. The climatology exhibits strong year-to-year variability but weak decadal variability and a small positive trend. A canonical correlation analysis describes the conditioning of the formation of Polar Lows by characteristic seasonal mean flow regimes, which favor, or limit, cold air outbreaks and upper air troughs.

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Spatial distribution, size composition, feeding habits, and dynamics of abundance of Alaska skate Bathyraja parmifera in the North Pacific

Journal of Ichthyology ◽

10.1134/s0032945215050069 ◽

2015 ◽

Vol 55 (5) ◽

pp. 644-663 ◽

Cited By ~ 3

Author(s):

I. V. Grigorov ◽

A. M. Orlov ◽

A. A. Baitalyuk

Keyword(s):

Spatial Distribution ◽

North Pacific ◽

Feeding Habits ◽

Size Composition ◽

Dynamics Of Abundance ◽

The North ◽

Alaska Skate ◽

Bathyraja Parmifera ◽

The North Pacific

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A Case Study of Downstream Baroclinic Development over the North Pacific Ocean. Part II: Diagnoses of Eddy Energy and Wave Activity

Monthly Weather Review ◽

10.1175/mwr3173.1 ◽

2006 ◽

Vol 134 (5) ◽

pp. 1549-1567 ◽

Cited By ~ 23

Author(s):

Richard E. Danielson ◽

John R. Gyakum ◽

David N. Straub

Keyword(s):

Group Velocity ◽

North Pacific ◽

North Pacific Ocean ◽

Wave Activity ◽

The North ◽

Initial Evolution ◽

Activity Center ◽

The North Pacific ◽

Made In

Abstract The sequential development of a western, and then an eastern, North Pacific cyclone is examined in terms of eddy energy and a phase-independent wave activity. Based on the propagation of both a contiguous wave activity center and eddy energy, the development of the western cyclone appears to influence its downstream neighbor. A quantitative comparison of these two diagnoses is made in terms of group velocity, and only minor differences are found during much of the initial evolution. It is only once the tropopause undulations lose their wavelike appearance (at which point, application of the group-velocity concept itself becomes quite tenuous) that the downstream propagation of eddy energy seems faster than that of wave activity. Conventional methods of tracking this wave packet are also briefly discussed.

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