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PubMed1994

Clothing and exercise. II. Influence of clothing during exercise/work in environmental extremes.

Thermoregulatory studies often investigate thermal responses without considering the influences of clothing. These studies have expanded our understanding of basic human responses to various environmental conditions. However, human thermoregulation is variable and modified by heat transfer interactions between skin surface area, clothing and environment. Much of the original work on the influence of clothing on work performance was the result of ergonomic concerns. Currently, the importance of clothing and the influence of new clothing technology aimed at minimising thermal stress has spawned a new interest. For hot climates, new fabrics have been developed with improved wicking properties to keep the wearer cooler and drier, and to enhance heat transfer from the body while providing greater comfort. In contrast, the challenge of cold environments requires a different approach to clothing, which tries to minimise the free movement of air and water along the skin surface of the body. The materials used should also be able to absorb radiant heat from the environment and be nonconductive. In a cold climate, the wearer needs to balance the need for a clothing barrier for warmth with the potential for accumulating too much heat as the result of metabolic heat production from exercise. To counteract this potential problem, it is suggested that cold-weather clothing be worn in layers that can be removed during exercise and replaced during less active periods. Protective clothing for firefighters, hazardous waste workers and astronauts, and athletic protective gear, have specialised design requirements which may be influenced by considerations, for example, of environmental conditions, garment weight, the need for durability, impact forces.

Body Temperature Regulation↗
PubMed2003

Photosynthesis of overwintering evergreen plants.

In this review we focus on photosynthetic behavior of overwintering evergreens with an emphasis on both the acclimative responses of photosynthesis to cold and the winter behavior of photosynthesis in conifers. Photosynthetic acclimation is discussed in terms of the requirement for a balance between the energy absorbed through largely temperature-insensitive photochemical processes and the energy used for temperature-sensitive biochemical processes and growth. Cold acclimation transforms the xanthophyll-mediated nonphotochemical antenna quenching of absorbed light from a short-term dynamic response to a long-term sustained quenching for the whole winter period. This acclimative response helps protect the evergreen foliage from photooxidative damage during the winter when photosynthesis is restricted or prevented by low temperatures. Although the molecular mechanisms behind the sustained winter excitation quenching are largely unknown, it does involve major alterations in the organization and composition of the photosystem II antenna. In addition, photosystem I may play an important role in overwintering evergreens not only by quenching absorbed light photochemically via its support of cyclic electron transport at low temperatures, but also by nonphotochemical quenching of absorbed light irrespective of temperature. The possible role of photosystem II reaction centers in nonphotochemical quenching of absorbed energy in overwintering evergreens is also discussed. Processes like chlororespiration and cyclic electron transport may also be important for maintaining the functional integrity of the photosynthetic apparatus of overwintering evergreens both during periods of thawing in winter and during recovery from winter stress in spring. We suggest that the photosynthetic acclimation responses of overwintering evergreens represent specific evolutionary adaptations for plant species that invest in the long-term maintenance of leaf structure in cold climatic zones as exemplified by the boreal forests of the Northern Hemisphere.

Acclimatization↗
PubMed1999

Thermophysical effects of ointments in cold: an experimental study with a skin model.

The use of emollients on the face is a traditional way to protect the skin against cold injuries in cold climate countries like Finland, but their preventive effect against frostbite has been questioned. The purpose of this investigation was to define the thermal insulation and occlusivity of ointments in cold by using a skin model with a sweating hot plate. The properties of four different emollients were studied in both dry and humid conditions simulating transepidermal water loss, sweating, and a combination of sweating and drying. The thermal insulation of ointments applied on a dry surface was minimal. Evaporation of water from an oil-in-water cream caused significant cooling for 40 min after its application. The diffusion of water through the applied emollients changed their thermal effects depending on their composition and on the amount of water. Low input of water increased and high input diminished slightly the thermal resistance of ointments. The minimal or even negative thermal insulation of emollients in varying conditions gives them at best only a negligible and at worst a disadvantageous physical effect against cold.

Cold Temperature↗
PubMed1989

An unusual case of accidental hypothermia due to cold water immersion.

Accidental deaths due to hypothermia most commonly result from exposure to low environmental temperature. Generally, a cold climatic condition is present in a severe environmental setting. A case report is presented of a 58-year-old man who died from accidental hypothermia associated with immersion in cold water while on a farm during warm weather. The importance of an adequate death scene investigation is discussed.

Cold Temperature↗
PubMed2003

Formation of recent martian gullies through melting of extensive water-rich snow deposits.

The observation of gullies on Mars indicates the presence of liquid water near the surface in recent times, which is difficult to reconcile with the current cold climate. Gullies have been proposed to form through surface runoff from subsurface aquifers or through melting of near-surface ice under warmer conditions. But these gullies are observed to occur preferentially in cold mid-latitudes, where the presence of liquid water is less likely, and on isolated surfaces where groundwater seepage would not be expected, making both potential explanations unsatisfactory. Here I show that gullies can form by the melting of water-rich snow that has been transported from the poles to mid-latitudes during periods of high obliquity within the past 10(5) to 10(6) years (refs 5, 6). Melting within this snow can generate sufficient water to erode gullies in about 5,000 years. My proposed model for gully formation is consistent with the age and location of the gullies, and it explains the occurrence of liquid water in the cold mid-latitudes as well as on isolated surfaces. Remnants of the snowpacks are still present on mid-latitude, pole-facing slopes, and the recent or current occurrence of liquid water within them provides a potential abode for life.

Journal Article↗
PubMed2002

Cryoprotectin: a plant lipid-transfer protein homologue that stabilizes membranes during freezing.

Plants from temperate and cold climates are able to increase their freezing tolerance during exposure to low non-freezing temperatures. It has been shown that several genes are induced in a coordinated manner during this process of cold acclimation. The functional role of most of the corresponding cold-regulated proteins is not yet known. We summarize our knowledge of those cold-regulated proteins that are able to stabilize membranes during a freeze-thaw cycle. Special emphasis is placed on cryoprotectin, a lipid-transfer protein homologue that was isolated from cold-acclimated cabbage leaves and that protects isolated chloroplast thylakoid membranes from freeze-thaw damage.

Acclimatization↗
PubMed1998

Climate change, thermal stress and mortality changes.

One of the potential effects of an anthropogenically induced climate change is a change in mortality related to thermal stress. In this paper, existing literature on the relationship between average temperatures and mortality is evaluated. By means of a simple meta-analysis an aggregated effect of a change in temperature on mortality is estimated for total, cardiovascular and respiratory mortality. These effect estimates are combined with projections of changes in baseline climate conditions of 20 cities, according to climate change scenarios of three General Circulation Models (GCMs). The results indicate that for most of the cities included, global climate change is likely to lead to a reduction in mortality rates due to decreasing winter mortality. This effect is most pronounced for cardiovascular mortality in elderly people in cities which experience temperate or cold climates at present. The sensitivity of the results to physiological and socio-economical adaptation is examined. However, more research is necessary to extend this work by inclusion of data from a wider range of populations.

Acclimatization↗
PubMed2006

Beta-2-microglobulin gene expression is maintained in rainbow trout and Atlantic salmon kept at low temperatures.

Finfish in the wild are regularly subjected to low temperatures, which have been shown to cause a loss of Major Histocompatibility receptor expression in common carp kept at 6 degrees C. This is similar to what was seen in a mammalian cell line cultured at 26 degrees C. Loss of expression of this critical viral recognition protein may provide one mechanism for the increased frequency of fish diseases at low temperatures. This report demonstrates that unlike carp and mammals, beta(2)m transcript levels in both rainbow trout and Atlantic salmon do not decrease after 10 days at temperatures as low as 2 degrees C. Reverse transcriptase (RT)-PCR indicated that transcript steady-state levels of trout beta(2)m were maintained in both tissues and peripheral blood leucocytes, whether freshly isolated or in primary culture. Polyclonal antibodies raised against a recombinant form of trout beta(2)m, demonstrated cross-reactivity to both rainbow trout and Atlantic salmon protein lysates. Use of these antibodies in western blot analyses indicated that cellular protein levels are also maintained at low temperatures in both species while qualitative epifluorescence analysis of freshly isolated peripheral blood leucocytes indicated persistent cell surface expression of trout beta(2)m even after 10 days at 2 degrees C. Rainbow trout and Atlantic salmon may therefore utilise an alternative mode of immune gene regulation than the common carp and mammals allowing them to maintain viral recognition machinery at low temperatures, possibly due to selection for survival in cold climates.

Animals↗
PubMed2001

Effects of climatic warming on cold hardiness of some northern woody plants assessed from simulation experiments.

Effects of climatic warming on cold hardiness were investigated for some northern woody plants. In the first experiment, seedlings of Norway spruce (Picea abies [L.] Karst.), Scots pine (Pinus sylvestris L.) and lodgepole pine (Pinus contorta Dougl. var. latifolia Engelm.) were exposed to naturally fluctuating temperatures averaging -6 degrees C (ambient) and 0 degrees C (elevated) for 16 weeks in midwinter before they were thawed and re-saturated with water. In lodgepole pine, needle sugar concentrations had decreased by 15%, and the temperature needed to induce 10% injury to needles in terms of electrolyte leakage had increased by 6 degrees C following treatment to elevated as compared with control temperatures. In contrast, Norway spruce and Scots pine showed no effects. The lack of an effect for Scots pine was ascribed to seedlings containing unusually large energy reserves that buffered respiratory expenditure of sugars. A strong, linear relationship between levels of cold hardiness, assessed by the electrolyte leakage method, and sugars was found when combining data from this and previous, similar experiments. In the second experiment, the evergreen dwarf shrub Empetrum hermaphroditum Hagerup was analysed for leaf cold hardiness, using the electrolyte leakage method, and sugar concentrations in late spring and late autumn during the third year of a warming experiment in a subarctic dwarf shrub community. The objective was to test the hypothesis that warming in the growing season alters hardening/dehardening cycles by increasing soil nitrogen mineralization and plant growth. Data found, however, suggested that cold hardening/dehardening cycles were unaffected by warming.

Journal Article↗
PubMed2000

Combining a beta2-agonist with a face mask to prevent exercise-induced bronchoconstriction.

BACKGROUND: In this study, we aimed to test the effect of combining a P2-agonist with a heat- and moisture-exchanging cellulose face mask in patients with bronchoconstriction induced by exercise in cold air. METHODS: Nine allergic, asthmatic patients with a history of adverse reaction to exercise were tested on an ergometric bicycle at a temperature of approximately -10 degrees C. They were in turn given no treatment, given premedication with a beta2-agonist, allowed to breathe through a heat- and moisture-exchanging cellulose face mask, and given both premedication and the face mask. After each treatment regimen, they were subjected to provocation with exercise and cold air. RESULTS: The decrease in FEV, was greatest with no therapy (mean maximal change: 27%), and this diminished when the face mask was used (mean maximal change: 12%,) or premedication with a 32-agonist was given (mean maximal change: 7%); no decrease in FEV1 occurred with the combination of agonist and face mask. CONCLUSIONS: The results suggest that different mechanisms are involved in the pathophysiology of exercise-induced bronchoconstriction (EIB). This finding may be of importance for asthmatic athletes who train and compete in a cold climate and are affected by small changes in their lung function.

Adrenergic beta-2 Receptor Agonists↗
PubMed1981

Human nasal protrusion, latitude, and climate.

Relationships between morphological features of human skeletal nasal protrusion, latitude, and climate were investigated. Craniofacial dimensions and indices determined by Woo and Morant (1934) on a world sample of 55 skeletal populations were used as dependent variables. Sample sizes were as low as 39 in some calculations because either skeletal or geographic data were missing. Thirteen climatically related averaged variables, for each population's provenience, were the independent variables. Multivariate techniques of bivariate correlation, multiple regression, and partial correlation were applied. A strong, Statistically significant cline of increasing nose protrusion, with decreasing absolute humidity and with increasing latitude, was found. Cold climatic variables appeared to be of greater importance than warm measures. Similarly, absolute humidity was found to be a much better predictor of nose protrusion than was relative humidity.

Adult↗
PubMed1989

What did our ancestors eat?

Over the millennia various hominoids and hominids have subsisted on very different dietaries, depending on climate, hunting proficiency, food-processing technology, and available foods. The Australopithecines were not browsers and fruit-eaters with very high intakes of vitamin C; rather they were scavengers of kills made by other animals. The hominids who followed did include some cold-climate hunters of large game, but the amount of animal protein decreased with the advent of grain-gathering and decreased further with the introduction of cereal agriculture, with a concomitant decrease in body size. From what we know about food adequacy, preparation, and storage, the notion that the postulated "primitive" diet was generally adequate, safe, and prudent can be rejected. Over evolutionary time, many of our ancestors ate poorly, especially during climate extremes, and they were often at risk for vitamin deficiencies, food-borne diseases, and neurotoxins. Until the advent of modern processing technologies, dirt, grit, and fiber constituted a large part of most early diets.

Animals↗
PubMed2005

Glacial-interglacial changes in the occurrence of Pb, Cd, Cu and Zn in Vostok Antarctic ice from 240 000 to 410 000 years BP.

Lead (Pb), cadmium (Cd), copper (Cu) and zinc (Zn) have been measured by electrothermal atomic absorption spectrometry in various sections of the 3623 m deep ice core drilled at Vostok, in central East Antarctica. The sections were dated from 240 to 410 kyear BP (Marine Isotopic Stages (MIS) 7.5 to 11.3), which corresponds to the 3rd and 4th glacial-interglacial cycles before present. Concentrations are found to have varied greatly during this 170 kyear time period, with high concentration values during the coldest climatic stages such as MIS 8.4 and 10.2 and much lower concentration values during warmer periods, such as the interglacials MIS 7.5, 9.3 and 11.3. Rock and soil dust were the dominant sources for Pb, whatever the period, and for Zn and Cu and possibly Cd during cold climatic stages. The contribution from volcanic emissions was important for Cd during all periods and might have been significant for Cu and Zn during warm periods.

Antarctic Regions↗
PubMed1999

Carbon monoxide fatalities in medicolegal autopsies.

All post-mortem medicolegal reports issued by Jordan University Hospital (JUH) during the period 1978-96 were reviewed. Carbon monoxide (CO) as a silent killer was responsible for 31.5% (n = 110) of poisoning fatalities. These were due to unintentional exposure to CO sources in confined spaces (bedrooms (24.6%), worker lodgings (23.6%) and bathrooms (16.4%), and without the victims being aware of CO hazards. Sixty-five per cent of CO fatalities occurred during December to February and 30% of the cases involved the age group 20-29 years, followed by the age group 30-39 years (20%). Non-Jordanians constituted 50% of CO fatalities and Egyptian workers accounted for 78%. Being unaccustomed to cold climates, and on low incomes, they had been using simple and unsafe heating devices. Many of these deaths could have been prevented. Safety educational campaigns to increase awareness of the general population of CO sources, their hazards and how to avoid them should be held continuously during the cold months of the year. All health and safety sectors are advised to be involved.

Adolescent↗
PubMed2004

Hospital admissions for heart disease: the effects of temperature and humidity.

BACKGROUND: We estimated the effects of temperature and humidity on hospital admissions for heart disease (International Classification of Diseases, 9th revision [ICD-9] codes 390-429) and myocardial infarction (ICD-9 code 410) of persons age 65 and older in 12 U.S. cities with a wide range of climates. To account for possible delayed effects and harvesting, we examined the impact of weather up to 20 days before each admission. METHODS: Poisson regression models were fitted in each city, with regression splines used to control for season and barometric pressure. We also controlled day of the week. We estimated the effect and the lag structure of both temperature and humidity based on a distributed lag model. FINDINGS: For cities in both hot and cold climates, we found that hospital admissions for all heart disease increased monotonically with average temperature on the same day as and the day before admission. The effect of very high temperatures had a temporal pattern consistent with harvesting: several days after an episode of high temperature, there were fewer admissions. In contrast, a protective effect of cold temperature persisted without rebound. The effects of either hot or cold temperature disappeared within 10 days of exposure. There was no evidence for a humidity effect. Similar but smaller effects of temperature were seen for admissions for myocardial infarction specifically. CONCLUSIONS: The effects of temperature on hospital admissions predominantly occur within a few days after exposure, and much of the effect of hot temperatures is short-term displacement of events.

Algorithms↗
PubMed1983

Winter blahs and spring irritability: the chronic but subtle behavioral operations.

Operation analyses, for which behavioral and environmental events are translated into reinforcement schedules, indicate that winter depression and spring irritability reported by people living in northern climates are dominated by four paradigms. They are (1) a shift in the ratio of negative to positive stimuli, (2) stimulus redundancy and satiation, (3) coerced hypoactivity or attenuation of free operant behavior, and (4) conditioned suppression or anxiety due to the progressive escalation of negative stimulus presentations. The chronic effects of these schedules on the behaviors of people living in cold climate during the winter season are discussed.

Anxiety↗
PubMed1993

Responses of Arctic and tropical men to a standard cold test and peripheral vascular responses to local cold stress in the Arctic.

Thermoregulatory, metabolic and peripheral vascular responses to cold were studied in two groups (six each) of healthy men during exposure to the natural cold environment of the Arctic. Group A comprised of two arctic natives and four temporary residents who had migrated from the temperature zone of Russia. Group B consisted of six soldiers from a tropical region (India). Group B was airlifted to the arctic (70 degrees N, 38 degrees E). Both groups stayed in a field camp. The experiments were conducted during the 7th week of the stay. The volunteers were subjected to a standard cold test at 10 degrees C for 2 h wearing only shorts. Their heart rate, blood pressure, ventilation, oxygen consumption, oral temperature, mean skin and extremity temperatures were recorded initially and at 30 min intervals during standard cold test. The cold-induced vasodilatation response in both groups was also studied separately. The tropical natives (Group B) were flown back to Delhi and retested after 6 weeks. The physiological responses to general cold exposure as well as peripheral vascular response to local arctic cold stress were similar in both groups. The observation suggested that cold acclimatization in tropical men is similar to that of the people of Russian origin from a temperature zone.

Acclimatization↗
PubMed2004

Natural and anthropogenic enrichments of molybdenum, thorium, and uranium in a complete peat bog profile, Jura Mountains, Switzerland.

A core from an ombrotrophic Swiss bog representing 12 370 (14)C years of peat accumulation was evaluated as a possible archive of atmospheric deposition of Mo, Th and U. Calcium, Sr, and Ba were also determined to quantify weathering inputs, Mn to follow possible redox transformations, and Rb to identify plant uptake. Each of these elements was determined using ICP-MS, following digestion in a microwave heated autoclave using 3 ml HNO(3) and 0.1 ml HBF(4). Calcium and Sr clearly identify the thickness of the ombrotrophic zone because they are enriched in the minerogenic zone relative to the concentration of mineral matter. The concentration of Ba, however, is proportional to the concentration of mineral matter in all samples, and is not added to peat column by weathering reactions at the peat-sediment interface. The lowest element concentrations are found during the Holocene climate optimum (5320 to 8030 (14)C year BP) with the following natural background values (n= 18): Mo 0.08 +/- 0.02 microg g(-1), U 0.029 +/- 0.008 microg g(-1), Ba 5.2 +/- 2.6 microg g(-1), Th 0.070 +/- 0.022 microg g(-1) and Rb 0.63 +/- 0.09 microg g(-1). By far the highest concentrations of Ba, Mn, Rb and Th were found during the Younger Dryas cold climate event (10 590 (14)C year BP) when the flux of atmospheric soil dust was at its post-glacial maximum. Molybdenum and U are elevated in concentration throughout the minerogenic zone because of sediment weathering and this masks the atmospheric signal in samples older than ca. 8000 (14)C year BP (ca. 9000 calendar years). Enrichment factors (EF) calculated using Sc as a conservative, lithogenic element shows that minerogenic peats are enriched in Mo up to 18x and U 26x, relative to the natural "background" values. During the two millennia prior to industrialisation, the accumulation rate of atmospheric Mo averaged 0.23 +/- 0.13 microg m(-2) year(-1). With the onset of the Industrial Revolution, Mo accumulation rates rapidly and continuously increased to approximately 10 microg m(-2) year(-1) in the late 1980s. These data suggest that Mo in atmospheric aerosols today is derived predominately from anthropogenic emissions. Uranium does not show the same enrichment pattern which suggests that steel-making rather than coal combustion is the primary source of atmospheric Mo contamination at this site.

Calcium↗