Chironomids, temperature and numerical models: a reply to Seppala

We reply to comments by Seppala (2001) concerning the suitability of the surface-water temperature measurements and mean July air temperature estimates used by Olander et al. (1999) to derive quantitative chironomid-temperature transfer functions. We use new data for water temperatures based on two-...

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Bibliographic Details
Main Authors: Korhola, A, Birks, HJB, Olander, H, Blom, T
Format: Article in Journal/Newspaper
Language:unknown
Published: ARNOLD, HODDER HEADLINE PLC 2001
Subjects:
Online Access:http://discovery.ucl.ac.uk/156719/
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author Korhola, A
Birks, HJB
Olander, H
Blom, T
author_facet Korhola, A
Birks, HJB
Olander, H
Blom, T
author_sort Korhola, A
collection University College London: UCL Discovery
description We reply to comments by Seppala (2001) concerning the suitability of the surface-water temperature measurements and mean July air temperature estimates used by Olander et al. (1999) to derive quantitative chironomid-temperature transfer functions. We use new data for water temperatures based on two-hourly recordings from thermistors installed in 32 lakes and air-temperature data from an automatic weather station at one lake to refute Seppalas accusations that our field data are unsatisfactory. We also respond to Seppala's suggestions about factors influencing chironomid distribution and abundance and suggest that there is a serious confusion of temporal and spatial scales between Seppala's ideas and the Olander et al. study. We attempt to explain the underlying logic behind empirical transfer functions that form a major part of Holocene quantitative environmental reconstructions and the major assumptions behind such transfer functions as Seppala appears not to understand the basis or the assumptions of such widely used numerical models in palaeolimnology. We respond to Seppala's comments that lakewater pH and distance beyond tree-line have been inadequately measured and answer his erroneous understanding that a helicopter was used to facilitate lake sampling. We briefly consider Seppala's suggestion that a helicopter can totally mix the surface water of a lake for many hours.
format Article in Journal/Newspaper
genre Arctic
Climate change
Fennoscandia
Fennoscandian
genre_facet Arctic
Climate change
Fennoscandia
Fennoscandian
geographic Arctic
Norway
geographic_facet Arctic
Norway
id ftucl:oai:eprints.ucl.ac.uk.OAI2:156719
institution Open Polar
language unknown
op_collection_id ftucl
op_source HOLOCENE , 11 (5) 615 - 622. (2001)
publishDate 2001
publisher ARNOLD, HODDER HEADLINE PLC
record_format openpolar
spelling ftucl:oai:eprints.ucl.ac.uk.OAI2:156719 2025-01-16T20:41:43+00:00 Chironomids, temperature and numerical models: a reply to Seppala Korhola, A Birks, HJB Olander, H Blom, T 2001 http://discovery.ucl.ac.uk/156719/ unknown ARNOLD, HODDER HEADLINE PLC HOLOCENE , 11 (5) 615 - 622. (2001) Chironomidae calibration modelling transfer functions summer temperature palaeotemperatures field measurements northern Fennoscandia ARCTIC FENNOSCANDIAN LAKES GAUSSIAN RESPONSE MODEL WATER TEMPERATURE AQUATIC INVERTEBRATES AIR TEMPERATURES QUANTITATIVE INDICATORS WESTERN NORWAY CLIMATE-CHANGE EARLY-HOLOCENE Article 2001 ftucl 2016-01-21T23:13:18Z We reply to comments by Seppala (2001) concerning the suitability of the surface-water temperature measurements and mean July air temperature estimates used by Olander et al. (1999) to derive quantitative chironomid-temperature transfer functions. We use new data for water temperatures based on two-hourly recordings from thermistors installed in 32 lakes and air-temperature data from an automatic weather station at one lake to refute Seppalas accusations that our field data are unsatisfactory. We also respond to Seppala's suggestions about factors influencing chironomid distribution and abundance and suggest that there is a serious confusion of temporal and spatial scales between Seppala's ideas and the Olander et al. study. We attempt to explain the underlying logic behind empirical transfer functions that form a major part of Holocene quantitative environmental reconstructions and the major assumptions behind such transfer functions as Seppala appears not to understand the basis or the assumptions of such widely used numerical models in palaeolimnology. We respond to Seppala's comments that lakewater pH and distance beyond tree-line have been inadequately measured and answer his erroneous understanding that a helicopter was used to facilitate lake sampling. We briefly consider Seppala's suggestion that a helicopter can totally mix the surface water of a lake for many hours. Article in Journal/Newspaper Arctic Climate change Fennoscandia Fennoscandian University College London: UCL Discovery Arctic Norway
spellingShingle Chironomidae
calibration modelling
transfer functions
summer temperature
palaeotemperatures
field measurements
northern Fennoscandia
ARCTIC FENNOSCANDIAN LAKES
GAUSSIAN RESPONSE MODEL
WATER TEMPERATURE
AQUATIC INVERTEBRATES
AIR TEMPERATURES
QUANTITATIVE INDICATORS
WESTERN NORWAY
CLIMATE-CHANGE
EARLY-HOLOCENE
Korhola, A
Birks, HJB
Olander, H
Blom, T
Chironomids, temperature and numerical models: a reply to Seppala
title Chironomids, temperature and numerical models: a reply to Seppala
title_full Chironomids, temperature and numerical models: a reply to Seppala
title_fullStr Chironomids, temperature and numerical models: a reply to Seppala
title_full_unstemmed Chironomids, temperature and numerical models: a reply to Seppala
title_short Chironomids, temperature and numerical models: a reply to Seppala
title_sort chironomids, temperature and numerical models: a reply to seppala
topic Chironomidae
calibration modelling
transfer functions
summer temperature
palaeotemperatures
field measurements
northern Fennoscandia
ARCTIC FENNOSCANDIAN LAKES
GAUSSIAN RESPONSE MODEL
WATER TEMPERATURE
AQUATIC INVERTEBRATES
AIR TEMPERATURES
QUANTITATIVE INDICATORS
WESTERN NORWAY
CLIMATE-CHANGE
EARLY-HOLOCENE
topic_facet Chironomidae
calibration modelling
transfer functions
summer temperature
palaeotemperatures
field measurements
northern Fennoscandia
ARCTIC FENNOSCANDIAN LAKES
GAUSSIAN RESPONSE MODEL
WATER TEMPERATURE
AQUATIC INVERTEBRATES
AIR TEMPERATURES
QUANTITATIVE INDICATORS
WESTERN NORWAY
CLIMATE-CHANGE
EARLY-HOLOCENE
url http://discovery.ucl.ac.uk/156719/