River and stream water quality and ecology - Greater Wellington ...
River and stream water quality and ecology - Greater Wellington ...
River and stream water quality and ecology - Greater Wellington ...
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<strong>River</strong> <strong>and</strong> <strong>stream</strong> <strong>water</strong> <strong>quality</strong> <strong>and</strong> <strong>ecology</strong> in the <strong>Wellington</strong> region: State <strong>and</strong> trends<br />
8.5 Monitoring limitations <strong>and</strong> knowledge gaps<br />
<strong>Greater</strong> <strong>Wellington</strong>’s RSoE monitoring programme has provided a significant<br />
amount of knowledge about the health of rivers <strong>and</strong> <strong>stream</strong>s in the <strong>Wellington</strong><br />
region. However, there are some limitations associated with the monitoring to<br />
date, as well as some more general knowledge gaps. The main limitations <strong>and</strong><br />
knowledge gaps are outlined below.<br />
While the RSoE programme has remained relatively stable in terms of<br />
monitoring sites <strong>and</strong> variables in recent years, there have been several<br />
changes in analytical laboratory over the last ten years, the most recent<br />
change being in July 2006 (for both <strong>water</strong> <strong>quality</strong> analyses <strong>and</strong> periphyton<br />
<strong>and</strong> macroinvertebrate identification). There have also been some changes<br />
in sampling personnel, most notably the use of external contractors<br />
between July 2006 <strong>and</strong> December 2007. Despite a number of checks<br />
being put in place to maintain consistency in sampling <strong>and</strong> analytical<br />
methods, a review of the RSoE data collected during the preparation of<br />
this report does indicate that there have been some effects on data <strong>quality</strong>,<br />
particularly for some <strong>water</strong> <strong>quality</strong> variables. For this reason the length of<br />
the temporal trend assessment period was restricted to the five most recent<br />
years. While a five-year period is considered appropriate for analysing<br />
recent trends in <strong>water</strong> <strong>quality</strong> data collected at monthly intervals<br />
(eg, Ballantine et al. 2010), assessment over a longer period would also<br />
have been desirable. Potentially the five-year period assessed here<br />
prevented the detection of some significant changes in <strong>water</strong> <strong>quality</strong><br />
(Ballantine et al. 2010).<br />
In addition to the change from external to in-house <strong>water</strong> <strong>quality</strong> sampling<br />
personnel during the five-year trend period, changes in some of the RSoE<br />
sampling runs meant that sampling times at some RSoE sites varied across<br />
the reporting period. As noted in Section 4.2, these changes impeded<br />
robust trend analysis for field measurements, particularly <strong>water</strong><br />
temperature, dissolved oxygen <strong>and</strong> pH which all exhibit diurnal variation.<br />
The need for st<strong>and</strong>ardisation of field data collection, ideally to within +/- 1<br />
hour, has been emphasised by Davies-Colley et al. (2011) in a recent<br />
report setting out recommended variables <strong>and</strong> protocols to support the<br />
establishment of a national river <strong>water</strong> <strong>quality</strong> monitoring programme.<br />
This same report also recommended continuous monitoring of diurnally<br />
fluctuating variables where possible.<br />
While flow-adjusted trend analyses were possible for <strong>water</strong> <strong>quality</strong> data<br />
from a much greater number of monitoring sites than in the last assessment<br />
of trends in river <strong>and</strong> <strong>stream</strong> <strong>water</strong> <strong>quality</strong> (Milne & Perrie 2005), there are<br />
still 11 sites where it has not yet been possible to derive an estimate of<br />
flow robust enough to enable flow-adjusted trend analysis. This is a<br />
significant limitation given that flow is known to influence some aspects<br />
of <strong>water</strong> <strong>quality</strong>, particularly optical properties <strong>and</strong> total phosphorus <strong>and</strong> E.<br />
coli concentrations (eg, three RSoE sites exhibited declining trends in<br />
visual clarity based on ‘raw’ measurements but the lack of flow data<br />
means that it is not known whether the trends are simply a result of<br />
changes in flow). Further efforts are required to obtain robust flow<br />
estimates for the affected sites; this may require manual flow gaugings at<br />
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