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The tenth IMSC, Beijing, China, 2007 - International Meetings on ...

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Richard E. Chandler<br />

University College L<strong>on</strong>d<strong>on</strong><br />

Valerie Isham<br />

University College L<strong>on</strong>d<strong>on</strong><br />

Howard Wheater<br />

Imperial College L<strong>on</strong>d<strong>on</strong><br />

<str<strong>on</strong>g>The</str<strong>on</strong>g>re is increasing recogniti<strong>on</strong> that, in hydrological problems such as flood risk<br />

assessment and management, it is desirable to simulate catchment processes over extended<br />

time periods. Such ’c<strong>on</strong>tinuous simulati<strong>on</strong>’ requires the ability to generate l<strong>on</strong>g sequences of<br />

rainfall data, at an appropriate spatial and temporal scale, for input to hydrological models of<br />

catchment resp<strong>on</strong>se. Moreover, for medium and l<strong>on</strong>g term planning it is necessary to account<br />

for climate change. This talk will describe research at UCL and at Imperial College L<strong>on</strong>d<strong>on</strong>,<br />

which aims to provide the UK with a nati<strong>on</strong>al capability for the generati<strong>on</strong> of future rainfall<br />

sequences at daily and subdaily time scales. <str<strong>on</strong>g>The</str<strong>on</strong>g> methodology exploits informati<strong>on</strong> from<br />

numerical climate models, while recognising that there are questi<strong>on</strong>s regarding the ability of<br />

these models to represent rainfall at scales of hydrological relevance. <str<strong>on</strong>g>The</str<strong>on</strong>g> work falls into two<br />

parts. First, generalized linear models (GLMs) are used to parameterise relati<strong>on</strong>ships between<br />

observed daily raingauge data and large-scale atmospheric variables that are represented<br />

reas<strong>on</strong>ably well by the climate models. It is shown that GLM simulati<strong>on</strong>s are able to reproduce<br />

closely the properties of historical rainfall sequences, including measures of interannual<br />

variability and extremes. In the sec<strong>on</strong>d stage, relati<strong>on</strong>ships are identified between rainfall<br />

properties at different temporal scales; these relati<strong>on</strong>ships appear invariant over a wide range<br />

of different climatic c<strong>on</strong>diti<strong>on</strong>s (represented by different m<strong>on</strong>ths of the year and different<br />

locati<strong>on</strong>s), and hence enable the properties of subdaily rainfall sequences to be deduced from<br />

those of daily sequences in an altered climate that is<br />

<str<strong>on</strong>g>The</str<strong>on</strong>g> seas<strong>on</strong>al characteristic of ChangSha's climate warming<br />

Liao Chunhua<br />

Weather service of Hunan Province<br />

liaochunhua_chat@126.com<br />

Liu Tiantian<br />

Weather service of Hunan Province<br />

This article statistics the air temperature data of ChangSha m<strong>on</strong>thly,the results are<br />

found:1.<str<strong>on</strong>g>The</str<strong>on</strong>g> air temperature of ChangSha has been rising in more than half century.2.<str<strong>on</strong>g>The</str<strong>on</strong>g><br />

characteristic of elevated temperature exist a notable seas<strong>on</strong>al difference in ChangSha,which<br />

is distinct in spring,but is unclear in summer.3.<str<strong>on</strong>g>The</str<strong>on</strong>g> climate warming of ChangSha is stand out<br />

in the recent 10 years.<br />

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