Name: Sea surface temperature
Display Field:
Type: Raster Layer
Geometry Type: null
Description: <DIV STYLE="text-align:Left;font-size:12pt"><DIV><DIV><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>Changes in Sea Surface Temperature (SST) can affect primary production rates, species composition and the spread of invasive species and disease as well as exacerbate sea level rise through thermal expansion. This map uses The New Zealand Earth System Model (NZESM) to compare the historical reference (2002-2019) and future (2040-2059 and 2080–2099) predictions of SST in degrees C. The future predictions show the difference between the future layer and the present layer to indicate areas with the most change in SST. Each cell of the present layer is subtracted from the corresponding cell in the future layer to show projected future change.</SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>The recently developed New Zealand Earth System Model (NZESM) incorporates component models of ocean biogeochemistry and other aspects of biology and chemistry that provide a highly complex model of the climate system (Behrens et al. 2020, Williams et al. 2016). The NZESM model differs from the UK Earth System Model (UKESM) in that it includes a high-resolution regional ocean model for the seas around New Zealand, and it includes a representation of the variability of solar radiation in atmospheric chemistry, as solar input is an important driver of climate variability at southern high latitudes. In the NZESM the nested high-resolution ocean model domain spans from 132.7°E to 143.7°W and 60.17°S to 10.75°S with a nominal resolution of 1/5°, which translates into grid sizes of 12 to 20 km. The horizontal grid has 75 vertical levels with a thickness of 1 m at surface and increasing with depth to about 250 m. Environmental parameters were obtained from the NZESM for the midpoint of every 1x1 km cell within the New Zealand region. The interpolation of all 2-D fields for each grid point of the 1 km target grid was done through bilinear interpolation of all surrounding model grid cells, after extrapolating ocean values onto land. For the interpolation of 3-D seafloor variables, a similar approach was applied, but with consideration of vertical model grid and model bathymetry. </SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>This NZESM can produce projections out to 200 years into the future (Williams et al. 2016). Here, we extracted predicted environmental conditions for an historical reference period (2002-2019) to represent present conditions, and two future reference periods (2040-2059, 2080–2099) to represent future conditions at different points in the current century. The predicted future conditions were based on the SSP3 (7.0 W/m2) pathway (RCP 7.0), which describes a medium-high reference scenario within the “regional rivalry” socio-economic family (O’Neill et al. 2017). Models were trained on current conditions, then fitted to these and future conditions under the future emissions pathways (SSP3-7.0). Each cell of the historical reference layer is subtracted from the corresponding cell in the future layer to create the layers shown indicating where the projected changes are greatest.</SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN>Source: National Institute of Water and Atmospheric Research Limited. (NIWA)</SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>Behrens, E., J. Williams, O. Morgenstern, P. Sutton, G. Rickard, and M. J. M. Williams. 2020. Local Grid Refinement in New Zealand's Earth System Model: Tasman Sea Ocean Circulation Improvements and Super-Gyre Circulation Implications. Journal of Advances in Modeling Earth Systems 12:e2019MS001996. https://doi.org/10.1029/2019MS001996 </SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>Williams, J., Morgenstern, O., Varma, V., Behrens, E., Hayek, W., Oliver, H., Dean, S., Mullan, B., Frame, D. (2016) Development of the New Zealand Earth System Model: NZESM. Weather and Climate, 36: 25-44. https://doi.org/10.2307/26779386</SPAN></SPAN></P><P STYLE="margin:0 0 11 0;"><SPAN><SPAN>O’Neill, B. C., E. Kriegler, K. L. Ebi, E. Kemp-Benedict, K. Riahi, D. S. Rothman, B. J. van Ruijven, D. P. van Vuuren, J. Birkmann, K. Kok, M. Levy, and W. Solecki. 2017. The roads ahead: Narratives for shared socioeconomic pathways describing world futures in the 21st century. Global Environmental Change 42:169-180. https://doi.org/10.1016/j.gloenvcha.2015.01.004</SPAN></SPAN></P></DIV></DIV></DIV>
Service Item Id: 6fcbce991df24254b470e4c7af03b010
Copyright Text: NIWA
Default Visibility: true
MaxRecordCount: 0
Supported Query Formats: JSON, geoJSON, PBF
Min Scale: 0
Max Scale: 0
Supports Advanced Queries: false
Supports Statistics: false
Has Labels: false
Can Modify Layer: false
Can Scale Symbols: false
Use Standardized Queries: true
Supports Datum Transformation: true
Extent:
XMin: 715115.8279954058
YMin: 3727333.0868047345
XMax: 2894115.8279954055
YMax: 7142333.086804735
Spatial Reference: 2193
(2193)
Drawing Info:
Advanced Query Capabilities:
Supports Statistics: false
Supports OrderBy: false
Supports Distinct: false
Supports Pagination: false
Supports TrueCurve: true
Supports Returning Query Extent: true
Supports Query With Distance: true
Supports Sql Expression: false
Supports Query With ResultType: false
Supports Returning Geometry Centroid: false
Supports Binning LOD: false
Supports Query With LOD Spatial Reference: false
HasZ: false
HasM: false
Has Attachments: false
HTML Popup Type: esriServerHTMLPopupTypeNone
Type ID Field: null
Fields:
None
Supported Operations:
Query
Query Attachments
Query Analytic
Generate Renderer
Return Updates
Iteminfo
Thumbnail
Metadata