Vladimir Krivtsov

Dr. Vladimir Krivtsov

orcid

Research Focus & Metrics

Academic Career Length

29Years (1998-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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27 September 2007 in Limnology and Oceanography
Verified
Journal Article
Closed access
JSJonathan Sharples
Jonathan Sharples
JTJacqueline F. Tweddle
Jacqueline F. Tweddle
JGJ. A. Mattias Green
J. A. Mattias Green
MPMatthew R. Palmer
Matthew R. Palmer
YKYoung-Nam Kim
Young-Nam Kim
VKVladimir Krivtsov
Vladimir Krivtsov

30 August 2012 in Marine Ecology Progress Series
Verified
Journal Article
Closed access
AHAe Hickman
Ae Hickman
CMCm Moore
Cm Moore
JSJ Sharples
J Sharples
MLMi Lucas
Mi Lucas
GTGh Tilstone
Gh Tilstone
PHPm Holligan
Pm Holligan
Photosynthesis versus irradiance relationships were used to estimate primary production (PP) at a number of locations across the seasonally stratified Celtic Sea during summer in 2003 and 2005. A subsurface chlorophyll maximum (SCM) was ubiquitously located at the base of the seasonal thermocline on the nitracline. Average PP for the stratified waters was 170 to 390 mg C m−2 d−1, of which 40 to 50% occurred within the thermocline, the range reflecting cloudy or sunny conditions. Phytoplankton photosynthesis was light-limited at the SCM, resulting in PP in the thermocline being more sensitive to surface irradiance conditions than that in the surface mixed layer. During the stratified period, production fuelled by nitrate from below the thermocline was estimated to be ~10 to 19 g C m−2, around half that determined for the spring bloom. Comparison of carbon (14C) fixation and nitrate (15NO3–) uptake versus irradiance experiments revealed that the proportion of 15NO3– uptake compared to 14C fixed was higher at the SCM than in the upper part of the thermocline where nitrate was depleted. The proportion also decreased with increasing irradiance. Estimates of 15NO3– and 14C uptake, dissolved oxygen production and the potential vertical diffusive nitrate flux from below suggested that ‘excess’ nitrate is assimilated relative to photosynthetic carbon fixation in the thermocline, particularly under cloudy conditions

12 March 2009 in Limnology and Oceanography
Verified
Journal Article
Closed access
PDF file
AHAnna Hickman
Anna Hickman
PHPatrick M. Holligan
Patrick M. Holligan
CMC. Mark Moore
C. Mark Moore
JSJonathan Sharples
Jonathan Sharples
VKVladimir Krivtsov
Vladimir Krivtsov
MPMatthew R. Palmer
Matthew R. Palmer


24 May 2019 in Water
Verified
Journal Article
Open access
PDF file
Richard FennerRichard Fenner
Richard Fenner
Emily O'DonnellEmily O'Donnell
Emily O'Donnell
Sangaralingam AhilanSangaralingam Ahilan
Sangaralingam Ahilan
DDDavid Dawson
David Dawson
LKLEON KAPETAS
LEON KAPETAS
VKVercruysse Kim
Vercruysse Kim
Preliminary results of the UK Urban Flood Resilience research consortium are presented and discussed, with the work being conducted against a background of future uncertainties with respect to changing climate and increasing urbanization. Adopting a whole systems approach, key themes include developing adaptive approaches for flexible engineering design of coupled grey and blue-green flood management assets; exploiting the resource potential of urban stormwater through rainwater harvesting, urban metabolism modelling and interoperability; and investigating the interactions between planners, developers, engineers and communities at multiple scales in managing flood risk. The work is producing new modelling tools and an extensive evidence base to support the case for multifunctional infrastructure that delivers multiple, environmental, societal and economic benefits, while enhancing urban flood resilience by bringing stormwater management and green infrastructure together.

13 February 2008 in Limnology and Oceanography: Methods
Verified
Journal Article
Closed access
OMOle A. Mikkelsen
Ole A. Mikkelsen
TMTimothy G. Milligan
Timothy G. Milligan
PHPaul S. Hill
Paul S. Hill
RCRobert J. Chant
Robert J. Chant
CJColin F. Jago
Colin F. Jago
GMGay Mitchelson‐Jacob
Gay Mitchelson‐Jacob