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Sea_surface_temperature (MapServer)

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Service Description: <DIV STYLE="text-align:Left;font-size:12pt"><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>Sea surface temperatures (SST) varies with location (generally warmer in the north and cooler in the south of New Zealand) and changes seasonally (warmer in summer and cooler in winter). Changes in sea surface temperatures are driven by wind causing major current and gyre formations as well as upwelling of deep water in addition to the influx of freshwater. Factors such as wind and wave mixing can bring colder water up, inflow of river water tends to be cooler than the sea in winter and warmer in summer, and coastal currents can bring warmer or colder water near to the coast. Sea surface temperatures influence both climate and weather in largescale events such as El Niño or smaller scale development of tropical cyclones as well as the health and distribution of marine life. Sea surface temperatures in NZ tend to range from ~8-23C. This layer uses long-term (2002–2017) average values at 250 m resolution blended from OI-SST (Reynolds et al., 2002) ocean product and MODIS-Aqua SST coastal product Pinkerton et al. (2018). To view a dynamic model of the change in SST along part of the South Island coast over 1 year see: </SPAN></SPAN><A href="https://vimeo.com/48991074" STYLE="text-decoration:underline;"><SPAN STYLE="text-decoration:underline;"><SPAN>https://vimeo.com/48991074</SPAN></SPAN></A></P><P STYLE="margin:0 0 11 0;"><SPAN STYLE="font-weight:bold;">Reference:</SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>Pinkerton, M.H. (2018). Ocean colour satellite observations of phytoplankton in the New Zealand EEZ, 1997–2018. NIWA report MFE18301-2018180WN, Prepared for Ministry</SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>Reynolds, RW, Rayner, NA, Smith, TM, Stokes, DC, &amp; Wang, W (2002). An improved in situ and satellite SST analysis for climate. Journal of Climate, 15: 1609-1625.</SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN /></P></DIV>

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Layers: Description: <DIV STYLE="text-align:Left;font-size:12pt"><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>Sea surface temperatures (SST) varies with location (generally warmer in the north and cooler in the south of New Zealand) and changes seasonally (warmer in summer and cooler in winter). Changes in sea surface temperatures are driven by wind causing major current and gyre formations as well as upwelling of deep water in addition to the influx of freshwater. Factors such as wind and wave mixing can bring colder water up, inflow of river water tends to be cooler than the sea in winter and warmer in summer, and coastal currents can bring warmer or colder water near to the coast. Sea surface temperatures influence both climate and weather in largescale events such as El Niño or smaller scale development of tropical cyclones as well as the health and distribution of marine life. Sea surface temperatures in NZ tend to range from ~8-23C. This layer uses long-term (2002–2017) average values at 250 m resolution blended from OI-SST (Reynolds et al., 2002) ocean product and MODIS-Aqua SST coastal product Pinkerton et al. (2018). To view a dynamic model of the change in SST along part of the South Island coast over 1 year see: </SPAN></SPAN><A href="https://vimeo.com/48991074" STYLE="text-decoration:underline;"><SPAN STYLE="text-decoration:underline;"><SPAN>https://vimeo.com/48991074</SPAN></SPAN></A></P><P STYLE="margin:0 0 11 0;"><SPAN STYLE="font-weight:bold;">Reference:</SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>Pinkerton, M.H. (2018). Ocean colour satellite observations of phytoplankton in the New Zealand EEZ, 1997–2018. NIWA report MFE18301-2018180WN, Prepared for Ministry</SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>Reynolds, RW, Rayner, NA, Smith, TM, Stokes, DC, &amp; Wang, W (2002). An improved in situ and satellite SST analysis for climate. Journal of Climate, 15: 1609-1625.</SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN /></P></DIV>

Service Item Id: c39d274aeb7f42cf90d522c69a59a346

Copyright Text: National Institute of Water and Atmospheric Research Ltd. (NIWA)

Spatial Reference: 2193  (2193)  LatestVCSWkid(0)


Single Fused Map Cache: false

Initial Extent: Full Extent: Units: esriMeters

Supported Image Format Types: PNG32,PNG24,PNG,JPG,DIB,TIFF,EMF,PS,PDF,GIF,SVG,SVGZ,BMP

Document Info: Supports Dynamic Layers: true

MaxRecordCount: 2000

MaxImageHeight: 4096

MaxImageWidth: 4096

Supported Query Formats: JSON, geoJSON, PBF

Supports Query Data Elements: true

Min Scale: 0

Max Scale: 0

Supports Datum Transformation: true



Child Resources:   Info   Dynamic Layer

Supported Operations:   Export Map   Identify   QueryLegends   QueryDomains   Find   Return Updates